Relevant bibliographies by topics / New South Wales Branch

Academic literature on the topic 'New South Wales Branch'

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Published: 4 June 2021
Last updated: 20 February 2023

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Journal articles on the topic "New South Wales Branch"

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Ferguson, Lorraine. "New South Wales branch." Confederation of Australian Critical Care Nurses Journal 4, no. 4 (December 1991): 12. http://dx.doi.org/10.1016/s1033-3355(11)80033-0.

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Ferguson, Lorraine. "New South Wales branch." Australian Critical Care 5, no. 1 (March 1992): 6. http://dx.doi.org/10.1016/s1036-7314(92)70003-4.

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3

Martin, A. P. "NEW SOUTH WALES BRANCH NEWS." Australian Endodontic Newsletter 8, no. 2 (February 11, 2010): 20. http://dx.doi.org/10.1111/j.1747-4477.1982.tb00817.x.

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Entwisle, Timothy J., and Helen J. Foard. "Batrachospermum (Batrachospermales, Rhodophyta) in Australia and New Zealand: New taxa and records in sections Contorta and Hybrida." Australian Systematic Botany 12, no. 4 (1999): 615. http://dx.doi.org/10.1071/sb98023.

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Six species of Batrachospermum from Australia and New Zealand have a twisted to coiled carpogonial branch and determinate gonimoblast filaments, and are therefore referable to section Contorta or Hybrida. Batrachospermum australicum KÜtz. ex sp. nov. from large rivers in tropical Northern Territory has a tightly 3-coiled carpogonial branch; B. vittatum sp. nov. from tropical Northern Territory has a characteristic longitudinal mid-whorl band of spermatangia; and B. deminutum sp. nov. from a single locality in eastern-central New South Wales has reduced whorls and long carpogonial branches. The other three species are cosmopolitan in distribution: B. virgatodecaisneanum Sirodot is widespread but uncommon in temperate regions of both countries; B. ambiguum Montagne is widespread and common in tropical Australia; and B. globosporum Israelson is restricted in Australia to near Brisbane in subtropical southern Queensland.
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PERKINS, PHILIP D. "A revision of the Australian humicolous and hygropetric water beetle genus Tympanogaster Perkins, and comparative morphology of the Meropathina (Coleoptera: Hydraenidae)." Zootaxa 1346, no. 1 (October 30, 2006): 1. http://dx.doi.org/10.11646/zootaxa.1346.1.1.

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The Australian endemic humicolous and hygropetric water beetle genus Tympanogaster Perkins, 1979, is revised, based on the study of 7,280 specimens. The genus is redescribed, and redescriptions are provided for T. cornuta (Janssens), T. costata (Deane), T. deanei Perkins, T. macrognatha (Lea), T. novicia (Blackburn), T. obcordata (Deane), T. schizolabra (Deane), and T. subcostata (Deane). Lectotypes are designated for Ochthebius labratus Deane, 1933, and Ochthebius macrognathus Lea, 1926. Ochthebius labratus Deane, 1933, is synonymized with Ochthebius novicius Blackburn, 1896. Three new subgenera are described: Hygrotympanogaster new subgenus (type species Tympanogaster (Hygrotympanogaster) maureenae new species; Topotympanogaster new subgenus (type species Tympanogaster (Topotympanogaster) crista new species; and Plesiotympanogaster new genus (type species Tympanogaster (Plesiotympanogaster) thayerae new species. Seventy-six new species are described, and keys to the subgenera, species groups, and species are given. High resolution digital images of all primary types are presented (online version in color), and geographic distributions are mapped. Male genitalia, representative spermathecae and representative mouthparts are illustrated. Scanning electron micrographs of external morphological characters of adults and larvae are presented. Selected morphological features of the other members of the subtribe Meropathina, Meropathus Enderlein and Tympallopatrum Perkins, are illustrated and compared with those of Tympanogaster. Species of Tympanogaster are typically found in the relict rainforest patches in eastern Australia. Most species have very limited distributions, and relict rainforest patches often have more than one endemic species. The only species currently known from the arid center of Australia, T. novicia, has the widest distribution pattern, ranging into eastern rainforest patches. There is a fairly close correspondence between subgenera and microhabitat preferences. Members of Tympanogaster (s. str.) live in the splash zone, usually on stream boulders, or on bedrock stream margins. The majority of T. (Hygrotympanogaster) species live in the hygropetric zone at the margins of waterfalls, or on steep rockfaces where water is continually trickling; a few rare species have been collected from moss in Nothofagus rainforests. Species of T. (Plesiotympanogaster) have been found in both hygropetric microhabitats and in streamside moss. The exact microhabitats of T. (Topotympanogaster) are unknown, but the morphology of most species suggests non-aquatic habits; most specimens have been collected in humicolous microhabitats, by sifting rainforest debris, or were taken in flight intercept traps. Larvae of hygropetric species are often collected with adults. These larvae have tube-like, dorsally positioned, mesothoracic spiracles that allow the larvae to breathe while under a thin film of water. The key morphological differences between larvae of Tympanogaster (s. str.) and those of Tympanogaster (Hygrotympanogaster) are illustrated. New species of Tympanogaster are: T. (s. str.) aldinga (New South Wales, Dorrigo National Park, Rosewood Creek), T. (s. str.) amaroo (New South Wales, Back Creek, downstream of Moffatt Falls), T. (s. str.) ambigua (Queensland, Cairns), T. (Hygrotympanogaster) arcuata (New South Wales, Kara Creek, 13 km NEbyE of Jindabyne), T. (Hygrotympanogaster) atroargenta (Victoria, Possum Hollow falls, West branch Tarwin River, 5.6 km SSW Allambee), T. (Hygrotympanogaster) barronensis (Queensland, Barron Falls, Kuranda), T. (s. str.) bluensis (New South Wales, Blue Mountains), T. (Hygrotympanogaster) bondi (New South Wales, Bondi Heights), T. (Hygrotympanogaster) bryosa (New South Wales, New England National Park), T. (Hygrotympanogaster) buffalo (Victoria, Mount Buffalo National Park), T. (Hygrotympanogaster) canobolas (New South Wales, Mount Canobolas Park), T. (s. str.) cardwellensis (Queensland, Cardwell Range, Goddard Creek), T. (Hygrotympanogaster) cascadensis (New South Wales, Cascades Campsite, on Tuross River), T. (Hygrotympanogaster) clandestina (Victoria, Grampians National Park, Golton Gorge, 7.0 km W Dadswells Bridge), T. (Hygrotympanogaster) clypeata (Victoria, Grampians National Park, Golton Gorge, 7.0 km W Dadswells Bridge), T. (s. str.) cooloogatta (New South Wales, New England National Park, Five Day Creek), T. (Hygrotympanogaster) coopacambra (Victoria, Beehive Falls, ~2 km E of Cann Valley Highway on 'WB Line'), T. (Topotympanogaster) crista (Queensland, Mount Cleveland summit), T. (Hygrotympanogaster) cudgee (New South Wales, New England National Park, 0.8 km S of Pk. Gate), T. (s. str.) cunninghamensis (Queensland, Main Range National Park, Cunningham's Gap, Gap Creek), T. (s. str.) darlingtoni (New South Wales, Barrington Tops), T. (Hygrotympanogaster) decepta (Victoria, Mount Buffalo National Park), T. (s. str.) dingabledinga (New South Wales, Dorrigo National Park, Rosewood Creek, upstream from Coachwood Falls), T. (s. str.) dorrigoensis (New South Wales, Dorrigo National Park, Rosewood Creek, upstream from Coachwood Falls), T. (Topotympanogaster) dorsa (Queensland, Windin Falls, NW Mount Bartle-Frere), T. (Hygrotympanogaster) duobifida (Victoria, 0.25 km E Binns, Hill Junction, adjacent to Jeeralang West Road, 4.0 km S Jeerelang), T. (s. str.) eungella (Queensland, Finch Hatton Gorge), T. (Topotympanogaster) finniganensis (Queensland, Mount Finnigan summit), T. (s. str.) foveova (New South Wales, Border Ranges National Park, Brindle Creek), T. (Hygrotympanogaster) grampians (Victoria, Grampians National Park, Epacris Falls, 2.5 km WNW Halls Gap), T. (Hygrotympanogaster) gushi (New South Wales, Mount Canobolas Park), T. (s. str.) hypipamee (Queensland, Mount Hypipamee National Park, Barron River headwaters below Dinner Falls), T. (s. str.) illawarra (New South Wales, Macquarie Rivulet Falls, near Wollongong), T. (Topotympanogaster) intricata (Queensland, Mossman Bluff Track, 5–10 km W Mossman), T. (s. str.) jaechi (Queensland, Running Creek, along road between Mount Chinghee National Park and Border Ranges National Park), T. (Topotympanogaster) juga (Queensland, Mount Lewis summit), T. kuranda (Queensland, Barron Falls, Kuranda), T. (s. str.) lamingtonensis (Queensland, Lamington National Park, Lightening Creek), T. (s. str.) magarra (New South Wales, Border Ranges National Park, Brindle Creek), T. (Hygrotympanogaster) maureenae (New South Wales, Back Creek, Moffatt Falls, ca. 5 km W New England National Park boundary), T. (Hygrotympanogaster) megamorpha (Victoria, Possum Hollow falls, W br. Tarwin River, 5.6 km SSW Allambee), T. (Hygrotympanogaster) merrijig (Victoria, Merrijig), T. (s. str.) millaamillaa (Queensland, Millaa Millaa), T. modulatrix (Victoria, Talbot Creek at Thomson Valley Road, 4.25 km WSW Beardmore), T. (Topotympanogaster) monteithi (Queensland, Mount Bartle Frere), T. moondarra (New South Wales, Border Ranges National Park, Brindle Creek), T. (s. str.) mysteriosa (Queensland), T. (Hygrotympanogaster) nargun (Victoria, Deadcock Den, on Den of Nargun Creek, Mitchell River National Park), T. (Hygrotympanogaster) newtoni (Victoria, Mount Buffalo National Park), T. (s. str.) ovipennis (New South Wales, Dorrigo National Park, Rosewood Creek, upstream from Coachwood Falls), T. (s. str.) pagetae (New South Wales, Back Creek, downstream of Moffatt Falls), T. (Topotympanogaster) parallela (Queensland, Mossman Bluff Track, 5–10 km W Mossman), T. (s. str.) perpendicula (Queensland, Mossman Bluff Track, 5–10 km W Mossman), T. plana (Queensland, Cape Tribulation), T. (Hygrotympanogaster) porchi (Victoria, Tarra-Bulga National Park, Tarra Valley Road, 1.5 km SE Tarra Falls), T. (s. str.) precariosa (New South Wales, Leycester Creek, 4 km. S of Border Ranges National Park), T. (s. str.) protecta (New South Wales, Leycester Creek, 4 km. S of Border Ranges National Park), T. (Hygrotympanogaster) punctata (Victoria, Mount Buffalo National Park, Eurobin Creek), T. (s. str.) ravenshoensis (Queensland, Ravenshoe State Forest, Charmillan Creek, 12 km SE Ravenshoe), T. (s. str.) robinae (New South Wales, Back Creek, downstream of Moffatt Falls), T. (s. str.) serrata (Queensland, Natural Bridge National Park, Cave Creek), T. (Hygrotympanogaster) spicerensis (Queensland, Spicer’s Peak summit), T. (Hygrotympanogaster) storeyi (Queensland, Windsor Tableland), T. (Topotympanogaster) summa (Queensland, Mount Elliott summit), T. (Hygrotympanogaster) tabula (New South Wales, Mount Canobolas Park), T. (Hygrotympanogaster) tallawarra (New South Wales, Dorrigo National Park, Rosewood Creek, Cedar Falls), T. (s. str.) tenax (New South Wales, Salisbury), T. (Plesiotympanogaster) thayerae (Tasmania, Liffey Forest Reserve at Liffey River), T. (s. str.) tora (Queensland, Palmerston National Park), T. trilineata (New South Wales, Sydney), T. (Hygrotympanogaster) truncata (Queensland, Tambourine Mountain), T. (s. str.) volata (Queensland, Palmerston National Park, Learmouth Creek, ca. 14 km SE Millaa Millaa), T. (Hygrotympanogaster) wahroonga (New South Wales, Wahroonga), T. (s. str.) wattsi (New South Wales, Blicks River near Dundurrabin), T. (s. str.) weiri (New South Wales, Allyn River, Chichester State Forest), T. (s. str.) wooloomgabba (New South Wales, New England National Park, Five Day Creek).
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6

Bułat-Silva, Zuzanna. "Śpiące języki, czyli słów kilka o sytuacji językowej rdzennych mieszkańców Australii na przykładzie języka gamilaraay z Nowej Południowej Walii." Język a Kultura 26 (February 22, 2017): 337–46. http://dx.doi.org/10.19195/1232-9657.26.27.

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Sleeping languages, afew remarks on the linguistic situation of Aboriginal people in Australia through the specific case of Gamilaraay, an Aboriginal language of New South WalesThe main aim of this article is to investigate revival linguistics, anew branch of linguistics as yet little known in Poland, through the specific case of the recent revival of Gamilaraay, an Aboriginal language of New South Wales, Australia. After discussing the classification of the world’s languages according to their vitality, the author presents the language situation in Australia and offers adefinition of revival linguistics, justifying its relevance to the revitalization of Aboriginal languages, including some that have been extinct for up to two hundred years.
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Clews, Lukas L. "Observations on roost use by the yellow-bellied sheathtail-bat (Saccolaimus flaviventris) in northern New South Wales, Australia." Australian Mammalogy 39, no. 1 (2017): 95. http://dx.doi.org/10.1071/am15048.

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Hollow-bearing trees are recognised as essential habitat features for insectivorous bats and provide sites for mating, the rearing of young, hibernation, protection from predators, and social interaction. The characteristics of hollow-bearing trees used as roosts by insectivorous bats in Australia are poorly known. To help fill this gap, this note presents data on tree roost characteristics for the yellow-bellied sheathtail-bat (Saccolaimus flaviventris) obtained from northern New South Wales, Australia. Of the 19 roost trees observed, most were live Eucalyptus albens trees with an incomplete crown with substantial numbers of dead limbs. Roosts selected were, on average, 9.3 m high with an entrance diameter of 12.7 cm in trees with a mean diameter at breast height of 49.5 cm. All entrance hollows were located at the end of a rotten spout formed when a branch had broken off the tree. These observations are some of the first to document the characteristics of roost trees for this species in New South Wales and this information can be used by land managers to identify and retain suitable roosting habitat for S. flaviventris in the landscape.
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Argent, N. M., and F. Rolley. "Financial Exclusion in Rural and Remote New South Wales, Australia: a Geography of Bank Branch Rationalisation, 1981-98." Australian Geographical Studies 38, no. 2 (July 2000): 182–203. http://dx.doi.org/10.1111/1467-8470.00110.

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O'Brien, John. "Book Reviews : Cause for Power: the Official Hispory of the New South Wales Branch of the Australian Labor Party." Journal of Industrial Relations 34, no. 4 (December 1992): 610–11. http://dx.doi.org/10.1177/002218569203400411.

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Waterson, D. B. "Book Reviews : TRADITIONS FOR REFORM IN NEW SOUTH WALES: LABOUR HISTORY ESSAYS Pluto Press in association with the New South Wales Branch of the Australian Labor Party, Sydney, 1987, xiv + 188 pp., $14.95 (paperback)." Journal of Industrial Relations 30, no. 4 (December 1988): 583–84. http://dx.doi.org/10.1177/002218568803000406.

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More sources

Dissertations / Theses on the topic "New South Wales Branch"

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Zhao, Lihua Built Environment Faculty of Built Environment UNSW. "The integration of geographical information systems and multicriteria decision making models for the analysis of branch bank closures." Awarded by:University of New South Wales. School of Built Environment, 2002. http://handle.unsw.edu.au/1959.4/33239.

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The research presented in this Thesis is primarily concerned with the field of Geographical Information Systems (GIS) - specifically, the business applications of the technology. The empirical problem addressed is the selection of branch banks as candidates for closure using the network of branch banks of the Commonwealth Bank of Australia in the Sydney metropolitan region as the case study. Decisions to close branches are made by the Bank on the basis of performance indicators that are essentially financial. In this research, however, an alternative approach is adopted: the problem is addressed using a set of spatial criteria. Following the deregulation of the finance industry in the 1980's and the rapid introduction of new electronic channels for delivering financial services, the major banking institutions have been engaged in a process of reorganising their networks of branch banks. The most visible manifestation of this has been the ongoing and widespread closure of branches. Selecting branch banks for closure is a typical example of a complex semi-structured multi-dimensional, multi-criteria, decision-making problem. It has been well documented in previous research that Multi-Criteria Decision-Making (MCDM) models are the most appropriate ones for solving problems in this particular domain. The identification of branches for closure is also characterised by a significant spatial dimension. Decisions are based on a consideration of a number of geographical criteria and various forms of spatial analysis may be involved. An appropriate technology to assist with solving decision-making problems with a significant spatial dimension is a Spatial Decision Support System (SDSS). Most SDSS have been based on the integration of Geographical Information Systems (GIS) technology with analytical models that are proven to be best suited to specific decision-making problems and this is the approach adopted in this research. The prototype MCBC-SDSS (Multi-Criteria Branch Closure SDSS) developed here is based on the integration through the loose coupling of the ArcView GIS software with the Criterium DecisionPlus (CDP) software, which contains the suite of non-spatial analytical models that provide the analytical capability for solving multi-criteria problems. ArcView GIS is used as the engine that drives the system and to provide the analytical and display facilities to support the spatial data involved. Two MCDM models from the CDP software are used to support the decision-making analysis - the Analytical Hierarchy Process (AHP) and Simple Multi-Attribute Rating Technique (SMART). The integration of GIS with the MCDM models is based on a considerable amount of software enhancement, interface development, and computer programming. The development of the integrated system is designed to create an intelligent and user-friendly SDSS, the application of which, from the user's perspective, is a seamless operation. The success of the MCBC-SDSS is demonstrated by its application to identify candidates for closure among the 197 branches of the CBA in the Sydney metropolitan area in 2000 - the year when the building of the database for the research had been completed. The analysis is based purely on spatial considerations that have been gleaned from a major review of the literature that previous researchers have identified as affecting branch viability and performance. A set of 17 spatial variables was used as the criteria in the MCDM models. The criteria are organised in two blocks: the first includes 9 criteria relating to the characteristics of demand for branch service in the branch trade areas ('catchment area' specific criteria) while the second includes 8 criteria relating to aspects of supply provided by the existing branches in their location ('location specific' criteria). Using the developed approach, the MCBC-SDSS has been used directly to compare alternatives against criteria, not only spatial based but also financial ones, thus providing a basis for identifying the best choices regarding branch closure. The steps in the preparation of the data and the iterative procedure for implementing the MCDM models are explained and illustrated. This involves building the initial evaluation matrix, normalising the raw criteria scores, assigning weights to the criteria, and calculating priorities. Based on these, the AHP and SMART models then calculate a decision score for each branch that is used as the basis for creating the preference ranking of the branches. In this, branches with a high rank score based on the combined weighted contribution of the 17 criteria are considered to be operationally viable. On the other hand, branches with the lowest rank scores are considered as potential candidates for closure. The preference rankings generated by the models have been tested to examine their robustness in terms of the validity of criteria and their weights used in the decision analysis. Sensitivity analysis has been conducted, the results of which show that the preference rankings are stable. Different approaches have been used to validate the initial criteria, and analyse their contribution to the ranking of branch banks for closure. These help identify critical spatial variables among the 17 initial criteria selected, and suggest that some of the criteria initially selected could be deleted from the criteria list used to generate the preference rankings without substantially affecting the results. The reasonableness of the resulting preference ranking has been further demonstrated from analyses based on changing criteria weights and alternatives. The research successfully demonstrates one of the ways of enhancing the functionality of a GIS through its integration with non-spatial analytical models to develop a SDSS to aid solving decision-making problems in the selected domain. Given that to date there has been relatively few applications of SDSS similar to that developed in this research to real world decision-making problems, the procedure adopted makes it suitable for decision-making in a range of other service business applications characterised by a significant spatial dimension and multiple outlets including shopping centres, motor car dealerships, restaurant and supermarket chains. Instead of just providing solutions, however, the SDSS-based analysis in this research can better be thought of as adding value to spatial data that forms an important source of information required by decision-makers, providing insight about the situation, uncertainty, objectives, and trade-offs involved in reaching decisions, and being capable of generating alternative scenarios based on different inputs to the models that may be used to identify recommended courses of action. It can lead to better and more effective decision-making in institutions involving multi-outlet retail and service businesses and hence enables both integrated data analysis and modelling while taking multiple criteria and decision-makers' preferences into consideration.
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Elder, John Richard. "THE AUSTRALIAN BUILDING CONSTRUCTION EMPLOYEES & BUILDERS LABOURERS FEDERATION AND THE NEW SOUTH WALES BUILDING INDUSTRY." Thesis, The University of Sydney, 1994. http://hdl.handle.net/2123/2155.

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Australia, during the twenty five years that followed the end of the Second World War, experienced increased prosperity and a stable industrial relations system in which the Commonwealth Conciliation and Arbitration Commission (the federal commission) played a dominant and authoritative role. The NSW building boom which began in the latter part of the 1950s introduced new technology, concentrated building workers in the central business district of Sydney, and broadened the range of skills required of builders' labourers. The major NSW building tradesmen's union, the Building Workers' Industrial Union (NSW/BWIU), had a communist leadership. The national body of that union lost its federal industrial registration in 1948, and the NSW/BWIU moderated its behaviour after it nearly lost its own, NSW state, registration in 1957. The Australian Building Construction Employees and Builders' Labourers Federation (ABLF) had a federal award under which most of the members of its NSW branch (NSW/BLF) were employed. The leadership of both the ABLF and of the NSW/BLF were communist. The Communist Party of Australia (CPA) suffered a defection by the ABLF leadership in the early 1960s to a communist party which endorsed Marxist- Leninist policies. The BWIU leadership also left the CPA (and formed the Socialist Party of Australia) following an announced shift in policy direction by the CPA in 1969. That shift in policy abandoned the `united front' concept and adopted ultra-left policies which advocated vanguard action by small groups. The announcement by the CPA of its new policies occurred after the gaoling of a Victorian union leader which signalled the virtual collapse of the previously authoritative, and punitive, role of the federal commission. The structure and politics of society underwent enormous change during the 1960s and early 1970s which was an era of protest during which various social movements were formed. The NSW/BLF became a major participant in those protests and movements, and conducted various industrial and social campaigns during the first half of the 1970s. Those campaigns were conducted in line with the ultra-left policies of the CPA, and this isolated the NSW/BLF from its federal body and from the trade union movement generally. This thesis analyses some of the campaigns conducted by the NSW/BLF during the period 1970-1974 and the various responses by the Master Builders Association of NSW (MBA/NSW) to those campaigns. The MBA/NSW broadened its membership base during the 1950s, and the effect that its new membership structure had on its decision-making processes is also considered.
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Elder, John Richard. "THE AUSTRALIAN BUILDING CONSTRUCTION EMPLOYEES & BUILDERS LABOURERS FEDERATION AND THE NEW SOUTH WALES BUILDING INDUSTRY." University of Sydney, 1994. http://hdl.handle.net/2123/2155.

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Master of Industrial Relations
Australia, during the twenty five years that followed the end of the Second World War, experienced increased prosperity and a stable industrial relations system in which the Commonwealth Conciliation and Arbitration Commission (the federal commission) played a dominant and authoritative role. The NSW building boom which began in the latter part of the 1950s introduced new technology, concentrated building workers in the central business district of Sydney, and broadened the range of skills required of builders' labourers. The major NSW building tradesmen's union, the Building Workers' Industrial Union (NSW/BWIU), had a communist leadership. The national body of that union lost its federal industrial registration in 1948, and the NSW/BWIU moderated its behaviour after it nearly lost its own, NSW state, registration in 1957. The Australian Building Construction Employees and Builders' Labourers Federation (ABLF) had a federal award under which most of the members of its NSW branch (NSW/BLF) were employed. The leadership of both the ABLF and of the NSW/BLF were communist. The Communist Party of Australia (CPA) suffered a defection by the ABLF leadership in the early 1960s to a communist party which endorsed Marxist- Leninist policies. The BWIU leadership also left the CPA (and formed the Socialist Party of Australia) following an announced shift in policy direction by the CPA in 1969. That shift in policy abandoned the `united front' concept and adopted ultra-left policies which advocated vanguard action by small groups. The announcement by the CPA of its new policies occurred after the gaoling of a Victorian union leader which signalled the virtual collapse of the previously authoritative, and punitive, role of the federal commission. The structure and politics of society underwent enormous change during the 1960s and early 1970s which was an era of protest during which various social movements were formed. The NSW/BLF became a major participant in those protests and movements, and conducted various industrial and social campaigns during the first half of the 1970s. Those campaigns were conducted in line with the ultra-left policies of the CPA, and this isolated the NSW/BLF from its federal body and from the trade union movement generally. This thesis analyses some of the campaigns conducted by the NSW/BLF during the period 1970-1974 and the various responses by the Master Builders Association of NSW (MBA/NSW) to those campaigns. The MBA/NSW broadened its membership base during the 1950s, and the effect that its new membership structure had on its decision-making processes is also considered.
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Rowling, Jill. "Cave Aragonites of New South Wales." Thesis, The University of Sydney, 2004. http://hdl.handle.net/2123/694.

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Abstract Aragonite is a minor secondary mineral in many limestone caves throughout the world. It has been claimed that it is the second-most common cave mineral after calcite (Hill & Forti 1997). Aragonite occurs as a secondary mineral in the vadose zone of some caves in New South Wales. Aragonite is unstable in fresh water and usually reverts to calcite, but it is actively depositing in some NSW caves. A review of current literature on the cave aragonite problem showed that chemical inhibitors to calcite deposition assist in the precipitation of calcium carbonate as aragonite instead of calcite. Chemical inhibitors work by physically blocking the positions on the calcite crystal lattice which would have otherwise allowed calcite to develop into a larger crystal. Often an inhibitor for calcite has no effect on the aragonite crystal lattice, thus aragonite may deposit where calcite deposition is inhibited. Another association with aragonite in some NSW caves appears to be high evaporation rates allowing calcite, aragonite and vaterite to deposit. Vaterite is another unstable polymorph of calcium carbonate, which reverts to aragonite and calcite over time. Vaterite, aragonite and calcite were found together in cave sediments in areas with low humidity in Wollondilly Cave, Wombeyan. Several factors were found to be associated with the deposition of aragonite instead of calcite speleothems in NSW caves. They included the presence of ferroan dolomite, calcite-inhibitors (in particular ions of magnesium, manganese, phosphate, sulfate and heavy metals), and both air movement and humidity. Aragonite deposits in several NSW caves were examined to determine whether the material is or is not aragonite. Substrates to the aragonite were examined, as was the nature of the bedrock. The work concentrated on Contact Cave and Wiburds Lake Cave at Jenolan, Sigma Cave, Wollondilly Cave and Cow Pit at Wombeyan and Piano Cave and Deep Hole (Cave) at Walli. Comparisons are made with other caves. The study sites are all located in Palaeozoic rocks within the Lachlan Fold Belt tectonic region. Two of the sites, Jenolan and Wombeyan, are close to the western edge of the Sydney Basin. The third site, Walli, is close to a warm spring. The physical, climatic, chemical and mineralogical influences on calcium carbonate deposition in the caves were investigated. Where cave maps were unavailable, they were prepared on site as part of the study. %At Jenolan Caves, Contact Cave and Wiburds Lake Cave were examined in detail, %and other sites were compared with these. Contact Cave is located near the eastern boundary of the Late Silurian Jenolan Caves Limestone, in an area of steeply bedded and partially dolomitised limestone very close to its eastern boundary with the Jenolan volcanics. Aragonite in Contact Cave is precipitated on the ceiling as anthodites, helictites and coatings. The substrate for the aragonite is porous, altered, dolomitised limestone which is wedged apart by aragonite crystals. Aragonite deposition in Contact Cave is associated with a concentration of calcite-inhibiting ions, mainly minerals containing ions of magnesium, manganese and to a lesser extent, phosphates. Aragonite, dolomite and rhodochrosite are being actively deposited where these minerals are present. Calcite is being deposited where minerals containing magnesium ions are not present. The inhibitors appear to be mobilised by fresh water entering the cave as seepage along the steep bedding and jointing. During winter, cold dry air pooling in the lower part of the cave may concentrate minerals by evaporation and is most likely associated with the ``popcorn line'' seen in the cave. Wiburds Lake Cave is located near the western boundary of the Jenolan Caves Limestone, very close to its faulted western boundary with Ordovician cherts. Aragonite at Wiburds Lake Cave is associated with weathered pyritic dolomitised limestone, an altered, dolomitised mafic dyke in a fault shear zone, and also with bat guano minerals. Aragonite speleothems include a spathite, cavity fills, vughs, surface coatings and anthodites. Calcite occurs in small quantities at the aragonite sites. Calcite-inhibitors associated with aragonite include ions of magnesium, manganese and sulfate. Phosphate is significant in some areas. Low humidity is significant in two areas. Other sites briefly examined at Jenolan include Glass Cave, Mammoth Cave, Spider Cave and the show caves. Aragonite in Glass Cave may be associated with both weathering of dolomitised limestone (resulting in anthodites) and with bat guano (resulting in small cryptic forms). Aragonite in the show caves, and possibly in Mammoth and Spider Cave is associated with weathering of pyritic dolomitised limestone. Wombeyan Caves are developed in saccharoidal marble, metamorphosed Silurian Wombeyan Caves Limestone. Three sites were examined in detail at Wombeyan Caves: Sigma Cave, Wollondilly Cave and Cow Pit (a steep sided doline with a dark zone). Sigma Cave is close to the south east boundary of the Wombeyan marble, close to its unconformable boundary with effusive hypersthene porphyry and intrusive gabbro, and contains some unmarmorised limestone. Aragonite occurs mainly in a canyon at the southern extremity of the cave and in some other sites. In Sigma Cave, aragonite deposition is mainly associated with minerals containing calcite-inhibitors, as well as some air movement in the cave. Calcite-inhibitors at Sigma Cave include ions of magnesium, manganese, sulfate and phosphate (possibly bat origin), partly from bedrock veins and partly from breakdown of minerals in sediments sourced from mafic igneous rocks. Substrates to aragonite speleothems include corroded speleothem, bedrock, ochres, mud and clastics. There is air movement at times in the canyon, it has higher levels of CO2 than other parts of the cave and humidity is high. Air movement may assist in the rapid exchange of CO2 at speleothem surfaces. Wollondilly Cave is located in the eastern part of the Wombeyan marble. At Wollondilly Cave, anthodites and helictites were seen in an inaccessible area of the cave. Paramorphs of calcite after aragonite were found at Jacobs Ladder and the Pantheon. Aragonite at Star Chamber is associated with huntite and hydromagnesite. In The Loft, speleothem corrosion is characteristic of bat guano deposits. Aragonite, vaterite and calcite were detected in surface coatings in this area. Air movement between the two entrances of this cave has a drying effect which may serve to concentrate minerals by evaporation in some parts of the cave. The presence of vaterite and aragonite in fluffy coatings infers that vaterite may be inverting to aragonite. Calcite-inhibitors in the sediments include ions of phosphate, sulphate, magnesium and manganese. Cave sediment includes material sourced from detrital mafic rocks. Cow Pit is located near Wollondilly Cave, and cave W43 is located near the northern boundary of the Wombeyan marble. At Cow Pit, paramorphs of calcite after aragonite occur in the walls as spheroids with minor huntite. Aragonite is a minor mineral in white wall coatings and red phosphatic sediments with minor hydromagnesite and huntite. At cave W43, aragonite was detected in the base of a coralloid speleothem. Paramorphs of calcite after aragonite were observed in the same speleothem. Dolomite in the bedrock may be a source of magnesium-rich minerals at cave W43. Walli Caves are developed in the massive Belubula Limestone of the Ordovician Cliefden Caves Limestone Subgroup (Barrajin Group). At the caves, the limestone is steeply bedded and contains chert nodules with dolomite inclusions. Gypsum and barite occur in veins in the limestone. At Walli Caves, Piano Cave and Deep Hole (Deep Cave) were examined for aragonite. Gypsum occurs both as a surface coating and as fine selenite needles on chert nodules in areas with low humidity in the caves. Aragonite at Walli caves was associated with vein minerals and coatings containing calcite-inhibitors and, in some areas, low humidity. Calcite-inhibitors include sulfate (mostly as gypsum), magnesium, manganese and barium. Other caves which contain aragonite are mentioned. Although these were not major study sites, sufficient information is available on them to make a preliminary assessment as to why they may contain aragonite. These other caves include Flying Fortress Cave and the B4-5 Extension at Bungonia near Goulburn, and Wyanbene Cave south of Braidwood. Aragonite deposition at Bungonia has some similarities with that at Jenolan in that dolomitisation of the bedrock has occurred, and the bedding or jointing is steep allowing seepage of water into the cave, with possible oxidation of pyrite. Aragonite is also associated with a mafic dyke. Wyanbene cave features some bedrock dolomitisation, and also features low grade ore bodies which include several known calcite-inhibitors. Aragonite appears to be associated with both features. Finally, brief notes are made of aragonite-like speleothems at Colong Caves (between Jenolan and Wombeyan), a cave at Jaunter (west of Jenolan) and Wellington (240\,km NW of Sydney).
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Rowling, Jill. "Cave Aragonites of New South Wales." University of Sydney. Geosciences, 2004. http://hdl.handle.net/2123/694.

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Abstract Aragonite is a minor secondary mineral in many limestone caves throughout the world. It has been claimed that it is the second-most common cave mineral after calcite (Hill & Forti 1997). Aragonite occurs as a secondary mineral in the vadose zone of some caves in New South Wales. Aragonite is unstable in fresh water and usually reverts to calcite, but it is actively depositing in some NSW caves. A review of current literature on the cave aragonite problem showed that chemical inhibitors to calcite deposition assist in the precipitation of calcium carbonate as aragonite instead of calcite. Chemical inhibitors work by physically blocking the positions on the calcite crystal lattice which would have otherwise allowed calcite to develop into a larger crystal. Often an inhibitor for calcite has no effect on the aragonite crystal lattice, thus aragonite may deposit where calcite deposition is inhibited. Another association with aragonite in some NSW caves appears to be high evaporation rates allowing calcite, aragonite and vaterite to deposit. Vaterite is another unstable polymorph of calcium carbonate, which reverts to aragonite and calcite over time. Vaterite, aragonite and calcite were found together in cave sediments in areas with low humidity in Wollondilly Cave, Wombeyan. Several factors were found to be associated with the deposition of aragonite instead of calcite speleothems in NSW caves. They included the presence of ferroan dolomite, calcite-inhibitors (in particular ions of magnesium, manganese, phosphate, sulfate and heavy metals), and both air movement and humidity. Aragonite deposits in several NSW caves were examined to determine whether the material is or is not aragonite. Substrates to the aragonite were examined, as was the nature of the bedrock. The work concentrated on Contact Cave and Wiburds Lake Cave at Jenolan, Sigma Cave, Wollondilly Cave and Cow Pit at Wombeyan and Piano Cave and Deep Hole (Cave) at Walli. Comparisons are made with other caves. The study sites are all located in Palaeozoic rocks within the Lachlan Fold Belt tectonic region. Two of the sites, Jenolan and Wombeyan, are close to the western edge of the Sydney Basin. The third site, Walli, is close to a warm spring. The physical, climatic, chemical and mineralogical influences on calcium carbonate deposition in the caves were investigated. Where cave maps were unavailable, they were prepared on site as part of the study. %At Jenolan Caves, Contact Cave and Wiburds Lake Cave were examined in detail, %and other sites were compared with these. Contact Cave is located near the eastern boundary of the Late Silurian Jenolan Caves Limestone, in an area of steeply bedded and partially dolomitised limestone very close to its eastern boundary with the Jenolan volcanics. Aragonite in Contact Cave is precipitated on the ceiling as anthodites, helictites and coatings. The substrate for the aragonite is porous, altered, dolomitised limestone which is wedged apart by aragonite crystals. Aragonite deposition in Contact Cave is associated with a concentration of calcite-inhibiting ions, mainly minerals containing ions of magnesium, manganese and to a lesser extent, phosphates. Aragonite, dolomite and rhodochrosite are being actively deposited where these minerals are present. Calcite is being deposited where minerals containing magnesium ions are not present. The inhibitors appear to be mobilised by fresh water entering the cave as seepage along the steep bedding and jointing. During winter, cold dry air pooling in the lower part of the cave may concentrate minerals by evaporation and is most likely associated with the ``popcorn line'' seen in the cave. Wiburds Lake Cave is located near the western boundary of the Jenolan Caves Limestone, very close to its faulted western boundary with Ordovician cherts. Aragonite at Wiburds Lake Cave is associated with weathered pyritic dolomitised limestone, an altered, dolomitised mafic dyke in a fault shear zone, and also with bat guano minerals. Aragonite speleothems include a spathite, cavity fills, vughs, surface coatings and anthodites. Calcite occurs in small quantities at the aragonite sites. Calcite-inhibitors associated with aragonite include ions of magnesium, manganese and sulfate. Phosphate is significant in some areas. Low humidity is significant in two areas. Other sites briefly examined at Jenolan include Glass Cave, Mammoth Cave, Spider Cave and the show caves. Aragonite in Glass Cave may be associated with both weathering of dolomitised limestone (resulting in anthodites) and with bat guano (resulting in small cryptic forms). Aragonite in the show caves, and possibly in Mammoth and Spider Cave is associated with weathering of pyritic dolomitised limestone. Wombeyan Caves are developed in saccharoidal marble, metamorphosed Silurian Wombeyan Caves Limestone. Three sites were examined in detail at Wombeyan Caves: Sigma Cave, Wollondilly Cave and Cow Pit (a steep sided doline with a dark zone). Sigma Cave is close to the south east boundary of the Wombeyan marble, close to its unconformable boundary with effusive hypersthene porphyry and intrusive gabbro, and contains some unmarmorised limestone. Aragonite occurs mainly in a canyon at the southern extremity of the cave and in some other sites. In Sigma Cave, aragonite deposition is mainly associated with minerals containing calcite-inhibitors, as well as some air movement in the cave. Calcite-inhibitors at Sigma Cave include ions of magnesium, manganese, sulfate and phosphate (possibly bat origin), partly from bedrock veins and partly from breakdown of minerals in sediments sourced from mafic igneous rocks. Substrates to aragonite speleothems include corroded speleothem, bedrock, ochres, mud and clastics. There is air movement at times in the canyon, it has higher levels of CO2 than other parts of the cave and humidity is high. Air movement may assist in the rapid exchange of CO2 at speleothem surfaces. Wollondilly Cave is located in the eastern part of the Wombeyan marble. At Wollondilly Cave, anthodites and helictites were seen in an inaccessible area of the cave. Paramorphs of calcite after aragonite were found at Jacobs Ladder and the Pantheon. Aragonite at Star Chamber is associated with huntite and hydromagnesite. In The Loft, speleothem corrosion is characteristic of bat guano deposits. Aragonite, vaterite and calcite were detected in surface coatings in this area. Air movement between the two entrances of this cave has a drying effect which may serve to concentrate minerals by evaporation in some parts of the cave. The presence of vaterite and aragonite in fluffy coatings infers that vaterite may be inverting to aragonite. Calcite-inhibitors in the sediments include ions of phosphate, sulphate, magnesium and manganese. Cave sediment includes material sourced from detrital mafic rocks. Cow Pit is located near Wollondilly Cave, and cave W43 is located near the northern boundary of the Wombeyan marble. At Cow Pit, paramorphs of calcite after aragonite occur in the walls as spheroids with minor huntite. Aragonite is a minor mineral in white wall coatings and red phosphatic sediments with minor hydromagnesite and huntite. At cave W43, aragonite was detected in the base of a coralloid speleothem. Paramorphs of calcite after aragonite were observed in the same speleothem. Dolomite in the bedrock may be a source of magnesium-rich minerals at cave W43. Walli Caves are developed in the massive Belubula Limestone of the Ordovician Cliefden Caves Limestone Subgroup (Barrajin Group). At the caves, the limestone is steeply bedded and contains chert nodules with dolomite inclusions. Gypsum and barite occur in veins in the limestone. At Walli Caves, Piano Cave and Deep Hole (Deep Cave) were examined for aragonite. Gypsum occurs both as a surface coating and as fine selenite needles on chert nodules in areas with low humidity in the caves. Aragonite at Walli caves was associated with vein minerals and coatings containing calcite-inhibitors and, in some areas, low humidity. Calcite-inhibitors include sulfate (mostly as gypsum), magnesium, manganese and barium. Other caves which contain aragonite are mentioned. Although these were not major study sites, sufficient information is available on them to make a preliminary assessment as to why they may contain aragonite. These other caves include Flying Fortress Cave and the B4-5 Extension at Bungonia near Goulburn, and Wyanbene Cave south of Braidwood. Aragonite deposition at Bungonia has some similarities with that at Jenolan in that dolomitisation of the bedrock has occurred, and the bedding or jointing is steep allowing seepage of water into the cave, with possible oxidation of pyrite. Aragonite is also associated with a mafic dyke. Wyanbene cave features some bedrock dolomitisation, and also features low grade ore bodies which include several known calcite-inhibitors. Aragonite appears to be associated with both features. Finally, brief notes are made of aragonite-like speleothems at Colong Caves (between Jenolan and Wombeyan), a cave at Jaunter (west of Jenolan) and Wellington (240\,km NW of Sydney).
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Keogh, Andrew James, of Western Sydney Hawkesbury University, Faculty of Science and Technology, and School of Applied and Environmental Sciences. "Systems management of Glenbrook Lagoon, New South Wales." THESIS_FST_AES_Keogh_A.xml, 1996. http://handle.uws.edu.au:8081/1959.7/423.

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Glenbrook Lagoon, an 8 hectare lake receiving rainfall runoff from a residential catchment, is experiencing nutrient enrichment problems expressed as excessive aquatic plant presence. This study aims to assess the relative nutrient contribution of the total system compartments, including catchment loading, water column, aquatic plants and surface sediment. This information is utilised in the formulation of management strategies which may produce a sustainable nutrient reduction and general improvement in the system. The total nutrient content of the aquatic system was determined to be high in comparison with the present nutrient loading from the catchment. The ideal management case considers nutrient reduction of the surface sediment compartment firstly, followed by the aquatic plant community, with the water column and catchment influence as relatively low priority compartments. Various strategies for managing these are proposed. The total system benefits of the ideal management case are reductions in nutrients, aquatic plant biovolume and suspended solid loading. Unavoidable constraints placed upon the ideal management case include the excessive aquatic plant presence restricting accessability to the surface sediment for dredging. The resulting best management case requires aquatic plant eradication prior to sediment management, with the total system benefits associated with the ideal management case being retained.
Master of Science (Hons)
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Elliott, Malcolm Gordon, of Western Sydney Hawkesbury University, and Faculty of Environmental Management and Agriculture. "Grass tetany of cattle in New South Wales." THESIS_FEMA_xxx_Elliott_M.xml, 2000. http://handle.uws.edu.au:8081/1959.7/7.

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Over the last 60 years, grass tetany has been recognised as a significant lethal condition in sheep and cattle.Outcomes from this study include documentation of the likely precursors to grass tetany, ways to recognise these precursors, and long term practices that will enable producers to minimise livestock deaths. The benefit of this research to beef producers is that the environmental circumstances thought to be associated with outbreaks of grass tetany have been identified, along with remedial action that can be taken to prevent deaths occurring.Recommendations to industry on best practice to be adopted by leading producers to minimise outbreaks of grass tetany are made.This study provides an alternate strategy for the management of grass tetany in beef cattle, to the more clinical approaches previously recommended. It is suggested that losses from this economically important metabolic disease can be minimised if management practices of beef cattle producers in eastern Australia can incorporate a more holistic approach to farm management, which takes account of the soil/plant/animal/climate inter-relationships.
Master of Science (Hons)
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8

Wood, Susan, and s2000093@student rmit edu au. "Creative embroidery in New South Wales, 1960 - 1975." RMIT University. Architecture and Design, 2006. http://adt.lib.rmit.edu.au/adt/public/adt-VIT20070206.160246.

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In the years between 1960 and 1975 in NSW there emerged a loosely connected network of women interested in modern or creative embroidery. The Embroiderers' Guild of NSW served as a focus for many of these women, providing opportunities for them to exhibit their work, and to engage in embroidery education as teachers or as learners. Others worked independently, exhibited in commercial galleries and endeavoured to establish reputations as professional artists. Some of these women were trained artists and wanted embroidery to be seen as 'art'; others were enthusiastic amateurs, engaged in embroidery as a form of 'serious leisure'. They played a significant role in the development of creative embroidery and textile art in NSW and yet, for the most part, their story is absent from the narratives of Australian art and craft history. These women were involved in a network of interactions which displayed many of the characteristics of more organised art worlds, as posite d by sociologist Howard Becker. They produced work according to shared conventions, they established co-operative links with each other and with other organisations, they organised educational opportunities to encourage others to take up creative embroidery and they mounted exhibitions to facilitate engagement with a public audience. Although their absence from the literature suggests that they operated in isolation, my research indicates that there were many points of contact between the embroidery world, the broader craft world and the fine art community in NSW. This thesis examines the context in which creative embroiderers worked, discusses the careers of key individuals working at this time, explores the interactions between them, and evaluates the influence that they had on later practice in embroidery and textiles in NSW.
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Keogh, Andrew James. "Systems management of Glenbrook Lagoon, New South Wales /." View thesis View thesis, 1996. http://library.uws.edu.au/adt-NUWS/public/adt-NUWS20030519.153643/index.html.

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Elliott, Malcolm Gordon. "Grass tetany of cattle in New South Wales /." View thesis View thesis, 2000. http://library.uws.edu.au/adt-NUWS/public/adt-NUWS20030424.150628/index.html.

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Books on the topic "New South Wales Branch"

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Carr, Bob. Matters of principle: The Labor revival in New South Wales. Melbourne: Australian Fabian Society, 1989.

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Bray, Mark. Delivering the goods: A history of the Transport Workers' Union in New South Wales 1888-1986. Sydney: Allen & Unwin, 1987.

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Hagan, Jim. A history of the Labor Party in New South Wales, 1891-1991. Melbourne: Longman Cheshire, 1991.

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Parliament, New South Wales, and Australian Labor Party. New South Wales Branch., eds. From the hustings to harbour views: Electoral institutions in New South Wales, 1856-2006. Sydney: UNSW Press, 2006.

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Michael, Hogan, and Australian Labor Party. New South Wales Branch., eds. Labor pains: Early conference and executive reports of the Labor Party in New South Wales. Annandale, N.S.W: Federation Press, 2006.

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1953-, Griffith Gareth, and New South Wales Parliament, eds. Decision and deliberation: The parliament of New South Wales 1856-2003. Sydney: Federation Press, 2005.

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Freudenberg, Graham. Cause for power: The official history of the New South Wales Branch of the Australian Labor Party. Leichhardt, NSW: Pluto Press, 1991.

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Local labor: A history of the Labor Party in Glebe, 1891-2003. Annandale, N.S.W: Federation Press, 2004.

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Power crisis: The self-destruction of a state labor party. Cambridge: Cambridge University Press, 2010.

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Verity, Burgmann, ed. Green bans, red union: Environmental activism and the New South Wales Builders Labourers' Federation. Sydney: UNSW Press, 1998.

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Book chapters on the topic "New South Wales Branch"

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Thom, Bruce. "New South Wales." In Encyclopedia of the World's Coastal Landforms, 1229–38. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8639-7_225.

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Plowman, David, and Keri Spooner. "Unions in New South Wales." In Australian Unions, 104–21. London: Macmillan Education UK, 1989. http://dx.doi.org/10.1007/978-1-349-11088-9_5.

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Laidlaw, Ronald W. "New South Wales 1821–51." In Mastering Australian History, 96–120. London: Macmillan Education UK, 1988. http://dx.doi.org/10.1007/978-1-349-09168-3_5.

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Wallace, Valerie. "Republicanism in New South Wales." In Scottish Presbyterianism and Settler Colonial Politics, 219–44. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-70467-8_10.

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Frahm, Michael. "Australia: Ombudsman New South Wales." In Australasia and Pacific Ombudsman Institutions, 117–29. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-33896-0_8.

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Chapman, D. M. "Australia--New South Wales and Queensland." In The GeoJournal Library, 415–22. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2999-9_45.

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Bird, Eric. "Lord Howe Island – (New South Wales)." In Encyclopedia of the World's Coastal Landforms, 1239–46. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8639-7_226.

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Tyler, Michael J. "Frogs of western New South Wales." In Future of the Fauna of Western New South Wales, 155–60. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.014.

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Ryan, Roberta, and Joseph Drew. "Performance Monitoring in New South Wales Australia." In Performance-Based Budgeting in the Public Sector, 61–77. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-02077-4_3.

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Gramiccia, Gabriele. "With the alpacas to New South Wales." In The Life of Charles Ledger (1818–1905), 69–119. London: Macmillan Education UK, 1988. http://dx.doi.org/10.1007/978-1-349-09949-8_3.

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Conference papers on the topic "New South Wales Branch"

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Platt, T. J. "New South Wales Incident Management System." In Ninth International Conference on Road Transport Information and Control. IEE, 1998. http://dx.doi.org/10.1049/cp:19980182.

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Senden, David van, and Douglas Lord. "Estuary Processes Investigation; New South Wales, Australia." In 27th International Conference on Coastal Engineering (ICCE). Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40549(276)288.

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Conway, Andrew, Michelle Blom, Lee Naish, and Vanessa Teague. "An analysis of New South Wales electronic vote counting." In ACSW 2017: Australasian Computer Science Week 2017. New York, NY, USA: ACM, 2017. http://dx.doi.org/10.1145/3014812.3014837.

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Allen, Lori E., Michael C. B. Ashley, Michael G. Burton, Stuart D. Ryder, John W. V. Storey, and Yinsheng Sun. "UNSWIRF: the University of New South Wales infrared Fabry-Perot." In Astronomical Telescopes & Instrumentation, edited by Albert M. Fowler. SPIE, 1998. http://dx.doi.org/10.1117/12.317242.

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Radoll, Peter, Sebastian Fleissner, Duncan Stevenson, and Henry Gardner. "Improving ICT support for aboriginal land councils in New South Wales." In the Sixth International Conference. New York, New York, USA: ACM Press, 2013. http://dx.doi.org/10.1145/2517899.2517916.

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Zhu, Qinggaozi, Xihua Yang, and Qiang Yu. "Climate change impact on bushfire risk in New South Wales, Australia." In IGARSS 2015 - 2015 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2015. http://dx.doi.org/10.1109/igarss.2015.7326042.

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Catalan, Alex, and C. Suarez. "Geotechnical characterisation — Cadia East panel caving project, New South Wales, Australia." In Second International Symposium on Block and Sublevel Caving. Australian Centre for Geomechanics, Perth, 2010. http://dx.doi.org/10.36487/acg_rep/1002_26_catalan1.

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"Modelling hydrological changes in New South Wales under future climate change." In 21st International Congress on Modelling and Simulation (MODSIM2015). Modelling and Simulation Society of Australia and New Zealand, 2015. http://dx.doi.org/10.36334/modsim.2015.g4.young.

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Duc, Hiep Nguyen, Sean Watt, David Salter, and Toan Trieu. "Modelling October 2013 Bushfire Pollution Episode in New South Wales, Australia." In 31st International Symposium on Automation and Robotics in Construction. International Association for Automation and Robotics in Construction (IAARC), 2014. http://dx.doi.org/10.22260/isarc2014/0072.

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Fityus, Stephen, and J. Gibson. "Rock Mass Stability in the Southern New England Fold Belt, New South Wales, Australia." In First Southern Hemisphere International Rock Mechanics Symposium. Australian Centre for Geomechanics, Perth, 2008. http://dx.doi.org/10.36487/acg_repo/808_57.

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Reports on the topic "New South Wales Branch"

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Reid, Andrew. Tackling gambling harm to improve health equity in New South Wales. Centre for Health Equity Training, Research and Evaluation, 2021. http://dx.doi.org/10.53714/igoo2131.

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Kyi, D., J. Duan, A. Kirkby, and N. Stolz. Australian Lithospheric Architecture Magnetotelluric Project (AusLAMP): New South Wales: data release report. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.011.

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Chisholm, Emma-Kate, Carol Simpson, and Phillip Blevin. New SHRIMP U-Pb zircon ages from the New England Orogen, New South Wales : July 2010-June 2012. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.013.

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Chisholm, E. I., P. L. Blevin, and C. J. Simpson. New SHRIMP U–Pb zircon ages from the New England Orogen, New South Wales: July 2012–June 2014. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.052.

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Waltenberg, K., P. L. Blevin, S. Bodorkos, and D. E. Cronin. New SHRIMP U-Pb zircon ages from the New England Orogen, New South Wales: July 2014-June 2015. Geoscience Australia and Geological Survey of New South Wales, 2015. http://dx.doi.org/10.11636/record.2015.028.

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Armistead, S. E., and G. L. Fraser. New SHRIMP U-Pb zircon ages from the Cuttaburra and F1 prospects, southern Thomson Orogen, New South Wales. Geoscience Australia, 2015. http://dx.doi.org/10.11636/record.2015.020.

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Bodorkos, S., K. F. Bull, L. M. Campbell, M. A. Eastlake, P. J. Gilmore, and S. J. Triggs. New SHRIMP U-Pb ages from the central Lachlan Orogen and New England Orogen, New South Wales: July 2014-June 2015. Geoscience Australia and Geological Survey of New South Wales, 2016. http://dx.doi.org/10.11636/record.2016.021.

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Fraser, G. L., P. J. Gilmore, J. A. Fitzherbert, S. J. Trigg, L. M. Campbell, L. Deyssing, O. D. Thomas, et al. New SHRIMP U-Pb zircon ages from the Lachlan, southern Thomson and New England orogens, New South Wales: February 2011–June 2013. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.053.

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Armistead, S. E., R. G. Skirrow, G. L. Fraser, D. L. Huston, D. C. Champion, and M. D. Norman. Gold and intrusion-related Mo-W mineral systems in the southern Thomson Orogen, New South Wales. Geoscience Australia, 2017. http://dx.doi.org/10.11636/record.2017.005.

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Garthwaite, M. C., and T. Fuhrmann. Subsidence monitoring in the Sydney Basin, New South Wales: results of the Camden Environmental Monitoring Project. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.016.

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