Journal articles: 'Geology New South Wales Bermagui'

1

Bryant, E. A., and R. W. Young. "Bedrock-Sculpturing by Tsunami, South Coast New South Wales, Australia." Journal of Geology 104, no. 5 (September 1996): 565–82. http://dx.doi.org/10.1086/629852.

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Carr, Paul, Malcolm Southwood, and Jeff Chen. "Fluorapatite from Broken Hill, New South Wales, Australia." Rocks & Minerals 97, no. 1 (December 20, 2021): 16–27. http://dx.doi.org/10.1080/00357529.2022.1989948.

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McIntyre, J. I. "Northwestern New South Wales regional magnetics and gravity." Exploration Geophysics 22, no. 2 (June 1991): 261–64. http://dx.doi.org/10.1071/eg991261.

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4

Greenhalgh, S. A., and D. W. Emerson. "Elastic Properties of Coal Measure Rocks New South Wales." Exploration Geophysics 17, no. 3 (September 1986): 157–63. http://dx.doi.org/10.1071/eg986157.

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Birch, William D. "Broken Hill New South Wales, Australia: Its Contribution to Mineralogy." Rocks & Minerals 82, no. 1 (January 2007): 40–49. http://dx.doi.org/10.3200/rmin.82.1.40-49.

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Smith, John V. "Textures recording transient porosity in synkinematic quartz veins, South Coast, New South Wales, Australia." Journal of Structural Geology 27, no. 2 (February 2005): 357–70. http://dx.doi.org/10.1016/j.jsg.2004.09.003.

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Spencer, Ross, and Robert J. Musgrave. "Isostatic and Decompensative Correction of Gravity Data From New South Wales." Exploration Geophysics 37, no. 3 (September 2006): 210–14. http://dx.doi.org/10.1071/eg06210.

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Thomas, Barry A., and Christopher J. Cleal. "A new early Westphalian D flora from Aberdulais Falls, South Wales." Proceedings of the Geologists' Association 112, no. 4 (January 2001): 373–77. http://dx.doi.org/10.1016/s0016-7878(01)80016-x.

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Rickards, R. B., and A. J. Wright. "Graptolites of the Barnby Hills Shale (Silurian, Ludlow), New South Wales, Australia." Proceedings of the Yorkshire Geological Society 51, no. 3 (May 1997): 209–27. http://dx.doi.org/10.1144/pygs.51.3.209.

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10

Howells, Cindy, and Thomas Kammer. "A new crinoid from the Mississippian (Early Carboniferous) of South Pembrokeshire, Wales." Geological Journal 49, no. 2 (May 21, 2013): 207–12. http://dx.doi.org/10.1002/gj.2514.

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Rickards, Barrie, Lawrence Sherwin, and Penelope Williamson. "Gisbornian (Caradoc) graptolites from New South Wales, Australia: systematics, biostratigraphy and evolution." Geological Journal 36, no. 1 (January 2001): 59–86. http://dx.doi.org/10.1002/gj.876.

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Graham, Lan T., and Ross E. Pogson. "The Albert Chapman Mineral Collection: Australian Museum, Sydney, New South Wales, Australia." Rocks & Minerals 82, no. 1 (January 2007): 29–39. http://dx.doi.org/10.3200/rmin.82.1.29-39.

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Le Gleuher, M. "Olivine wathering in basalts near Cooma, New-South-Wales, Australia." Chemical Geology 84, no. 1-4 (July 1990): 96–97. http://dx.doi.org/10.1016/0009-2541(90)90174-6.

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Holford, I. C. R., C. Hird, and R. Lawrie. "Effects of animal effluents on the phosphorus sorption characteristics of soils." Soil Research 35, no. 2 (1997): 365. http://dx.doi.org/10.1071/s96048.

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Two groups of soils were examined to determine the effects of dairy, pig, or sewage effluent and other materials containing phosphorus (P) on their P sorption characteristics, using the Langmuir equation to estimate values of both sorption capacity and sorption strength. There were 19 soils (0-15 cm) from 6 sites in the Williams River catchment and 3 soils (0-100 cm) from Bermagui, all from coastal New South Wales. Effluent usually decreased P sorption capacities of the Williams River soils, and in 3 soils the capacities were reduced to zero. Sorption strength was reduced substantially by effluent treatment in all soils except one, which had received effluent for only 3 years. Sorption strength, but not necessarily capacity, was also lower after treatment with poultry manure or chicken litter than after treatment with superphosphate only. Where effluent did not decrease sorption capacity there was a substantial increase in total carbon and iron, both of which could increase sorption capacities. After 3 years of effluent treatment of the Bermagui soil, sorption capacities had been reduced in the top 70 cm depth, the extent of the reduction varying from 17% at 0-7 · 5 cm depth to 38% at 40-70 cm depth. Sorption strength was reduced in the top 40 cm depth only. After 12 years of effluent treatment, sorption capacities and strength had also decreased at the deeper sampling depths (to 100 cm), and the average reduction in capacity was about 40%. These results suggest that P leaching will begin well before the total sorption capacity has been saturated. There was a direct and significant correlation between the sorption strength of the untreated soil and the percentage saturation reached before leaching began. Further saturation of the sorption complex appears to be slow after this degree of saturation has been reached, and it seems that P leaching exceeds adsorption during this phase. There was also a negative correlation between sorption strength and KCl-soluble P in all soils, suggesting that soil P solubility and potential saturation are both controlled by this characteristic.

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15

Hendrickx, Marc. "Fibrous Tremolite in Central New South Wales, Australia." Environmental and Engineering Geoscience 26, no. 1 (February 20, 2020): 73–77. http://dx.doi.org/10.2113/eeg-2273.

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ABSTRACT Tremolite schists in Ordovician meta-volcanic units in central New South Wales (NSW) consist of fine fibrous tremolite-actinolite. They host tremolite asbestos occurrences, and small quantities of asbestos were mined from narrow vein deposits in central NSW during the last century. When pulverized, the tremolite schist releases mineral fragments that fall into the classification range for countable mineral fibers and may be classed as asbestos despite not having an asbestiform habit. The ambiguity in classification of this type of natural material raises significant health and safety, legal, and environmental issues that require clarification. While the health effects of amphibole asbestos fibers are well known, the consequences of exposure to non-asbestiform, fibrous varieties is not well studied. This group of elongated mineral particles deserves more attention due to their widespread occurrence in metamorphic rocks in Australia. Toxicological studies are needed to assess the health risks associated with disturbance of these minerals during mining, civil construction, forestry, and farming practices.

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16

Bowyer, J. K. "Basin changes in Jervis Bay, New South Wales: 1894–1988." Marine Geology 105, no. 1-4 (March 1992): 211–24. http://dx.doi.org/10.1016/0025-3227(92)90189-o.

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17

Leslie, Christopher, Leonie Jones, Éva Papp, Kevin Wake-Dyster, Tara J. Deen, and Karsten Gohl. "High-resolution seismic imagery of palaeochannels near West Wyalong, New South Wales." Exploration Geophysics 31, no. 1-2 (March 2000): 383–88. http://dx.doi.org/10.1071/eg00383.

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18

Parr, Joanna M., Brian P. J. Stevens, Graham R. Carr, and Rodney W. Page. "Subseafloor origin for Broken Hill Pb-Zn-Ag mineralization, New South Wales, Australia." Geology 32, no. 7 (2004): 589. http://dx.doi.org/10.1130/g20358.1.

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19

Fortey, Richard A. "A new deep-water Upper Ordovician (Caradocian) trilobite fauna from south-west Wales." Geological Journal 41, no. 2 (2006): 243–53. http://dx.doi.org/10.1002/gj.1042.

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20

Rheinberger, Mark, and Ernst Holland. "Australian Fossil & Mineral Museum: Home of the Somerville CollectionBathurst, New South Wales." Rocks & Minerals 83, no. 6 (November 2008): 528–33. http://dx.doi.org/10.3200/rmin.83.6.528-533.

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21

Sherwin, L., and B. Rickards. "Rogercooperia, a new genus of Ordovician glossograptid graptolite from southern Scotland and New South Wales, Australia." Scottish Journal of Geology 36, no. 2 (November 2000): 159–64. http://dx.doi.org/10.1144/sjg36020159.

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22

Gray, Nigel, Alex Mandyczewsky, and Richard Hine. "Geology of the zoned gold skarn system at Junction Reefs, New South Wales." Economic Geology 90, no. 6 (October 1, 1995): 1533–52. http://dx.doi.org/10.2113/gsecongeo.90.6.1533.

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23

Young, Robert, and Ian McDougall. "Long-Term Landscape Evolution: Early Miocene and Modern Rivers in Southern New South Wales, Australia." Journal of Geology 101, no. 1 (January 1993): 35–49. http://dx.doi.org/10.1086/648195.

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24

Mayer, W. "The quest for limestone in colonial New South Wales, 1788–1825." Geological Society, London, Special Publications 287, no. 1 (2007): 325–42. http://dx.doi.org/10.1144/sp287.25.

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25

Nimbs, Matt J., and Stephen D. A. Smith. "An illustrated inventory of the sea slugs of New South Wales, Australia (Gastropoda: Heterobranchia)." Proceedings of the Royal Society of Victoria 128, no. 2 (2016): 44. http://dx.doi.org/10.1071/rs16011.

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Although the Indo-Pacific is the global centre of diversity for the heterobranch sea slugs, their distribution remains, in many places, largely unknown. On the Australian east coast, their diversity decreases from approximately 1000 species in the northern Great Barrier Reef to fewer than 400 in Bass Strait. While occurrence records for some of the more populated sections of the coast are well known, data are patchy for more remote areas. Many species have very short lifecycles, so they can respond rapidly to changes in environmental conditions. The New South Wales coast is a recognised climate change hot-spot and southward shifts in distribution have already been documented for several species. However, thorough documentation of present distributions is an essential prerequisite for identifying further range extensions. While distribution data are available in the public realm, much is also held privately as photographic collections, diaries and logs. This paper consolidates the current occurrence data from both private and public sources as part of a broader study of sea slug distribution in south-eastern Australia and provides an inventory by region. A total of 382 species, 155 genera and 54 families is reported from the mainland coast of New South Wales.

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26

Webster, S. S., and K. Tenison Woods. "Field Trials of Non-Seismic Geophysical Techniques for Petroleum Exploration in New South Wales." Exploration Geophysics 19, no. 1-2 (March 1988): 193–98. http://dx.doi.org/10.1071/eg988193.

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27

Robson, D. F., and R. Spencer. "The New South Wales Government’S Discovery 2000 – Geophysical Surveys and Their Effect on Exploration." Exploration Geophysics 28, no. 1-2 (March 1997): 296–98. http://dx.doi.org/10.1071/eg997296.

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28

Degeling, P. R., L. B. Gilligan, E. Scheibner, and D. W. Suppel. "Metallogeny and tectonic development of the Tasman Fold Belt System in New South Wales." Ore Geology Reviews 1, no. 2-4 (November 1986): 259–313. http://dx.doi.org/10.1016/0169-1368(86)90011-9.

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29

Ishak, A. K., and A. C. Dunlop. "Drainage sampling for uranium in the Torrington district, New South Wales, Australia." Journal of Geochemical Exploration 24, no. 1 (September 1985): 103–19. http://dx.doi.org/10.1016/0375-6742(85)90006-8.

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30

Nutley, David M., Cosmos Coroneos, and James Wheeler. "Potential submerged Aboriginal archaeological sites in South West Arm, Port Hacking, New South Wales, Australia." Geological Society, London, Special Publications 411, no. 1 (September 11, 2014): 265–85. http://dx.doi.org/10.1144/sp411.3.

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31

STEVENS, B., R. BARNES, R. BROWN, W. STROUD, and I. WILLIS. "The Willyama Supergroup in the Broken Hill and Euriowie Blocks, New South Wales." Precambrian Research 40-41 (October 1988): 297–327. http://dx.doi.org/10.1016/0301-9268(88)90073-3.

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32

Cope, J. C. W., and A. W. A. Rushton. "Cambrian and early Tremadoc rocks of the Llangynog Inlier, Dyfed, South Wales." Geological Magazine 129, no. 5 (September 1992): 543–52. http://dx.doi.org/10.1017/s0016756800021701.

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AbstractUntil recently no Cambrian rocks were known in the Llangynog area. Detailed mapping has now revealed a succession of ?Lower and Upper Cambrian rocks overlain by Tremadoc rocks. The Allt y Shed Sandstones (new) rest unconformably on the Precambrian, but have yielded no diagnostic fossils and are tentatively assigned to the Comley Series. Succeeding with faulted or unconformable contact is an Upper Cambrian Merioneth Series succession which includes in ascending order: conglomerates, sandstones and siltstones with olenid trilobites and resembling the Treffgarne Bridge Beds of the Haverfordwest area; micaceous shales and siltstones referred to the Ffestiniog Flags Formation; and black mudstones with calcareous concretions and a rich olenid fauna referred to the Dolgellau Formation. Succeeding the latter with possible disconformity is a succession belonging to the lower part of the Tremadoc Series and earlier than any rocks of that series hitherto recorded from the area.

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33

PHILLIPS, EMRYS. "Progressive deformation of the South Stack and New Harbour Groups, Holy Island, western Anglesey, North Wales." Journal of the Geological Society 148, no. 6 (November 1991): 1091–100. http://dx.doi.org/10.1144/gsjgs.148.6.1091.

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34

Munday, Tim J., Nerida S. Reilly, Mark Glover, Kenneth C. Lawrie, Tenille Scott, Colin J. Chartres, and W. R. (Ray) Evans. "Petrophysical characterisation of parna using ground and downhole geophysics at Marinna, central New South Wales." Exploration Geophysics 31, no. 1-2 (March 2000): 260–66. http://dx.doi.org/10.1071/eg00260.

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35

Spadari, M., M. Kardani, R. De Carteret, A. Giacomini, O. Buzzi, S. Fityus, and S. W. Sloan. "Statistical evaluation of rockfall energy ranges for different geological settings of New South Wales, Australia." Engineering Geology 158 (May 2013): 57–65. http://dx.doi.org/10.1016/j.enggeo.2013.03.007.

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36

Ward, Colin R., D. A. Spears, Carol A. Booth, Ian Staton, and Lila W. Gurba. "Mineral matter and trace elements in coals of the Gunnedah Basin, New South Wales, Australia." International Journal of Coal Geology 40, no. 4 (July 1999): 281–308. http://dx.doi.org/10.1016/s0166-5162(99)00006-3.

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37

Cohen, D. R., C. M. Silva-Santisteban, N. F. Rutherford, D. L. Garnett, and H. M. Waldron. "Comparison of vegetation and stream sediment geochemical patterns in northeastern New South Wales." Journal of Geochemical Exploration 66, no. 3 (September 1999): 469–89. http://dx.doi.org/10.1016/s0375-6742(99)00042-4.

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38

McPhie, J. "Evolution of a non-resurgent cauldron: the Late Permian Coombadjha Volcanic Complex, northeastern New South Wales, Australia." Geological Magazine 123, no. 3 (May 1986): 257–77. http://dx.doi.org/10.1017/s0016756800034749.

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AbstractThe Coombadjha Volcanic Complex is the remnant of a Late Permian cauldron. It is part of an extensive sequence of silicic calc-alkaline volcanics that covers the southeastern portion of the New England Orogen in NSW. The Complex is elliptical, measuring 15 × 24 km, and is outlined by a ring pluton and an arcuate fault. Bedding in the volcanic units of the Complex defines a structural basin, with steep inward dips at the monoclinal rim and gentle to horizontal orientations near the centre. An older group of outflow ignimbrites, lavas, breccias and volcaniclastic rocks at least 1500 m thick, is conformably overlain by more than 500 m of texturally homogeneous, crystal-rich, dacitic ignimbrite. Ignimbrites of the older group are the products of several discrete eruptions from separate vents, all of which were situated outside the Coombadjha area. Silicic lava domes with volcaniclastic aprons, and a tuff ring, mark the positions of local vents active on a small scale during intervals between the emplacement of the outflow ignimbrites. No significant subsidence occurred, nor did a caldera exist at this stage. Cauldron subsidence occurred in response to the large magnitude eruption that produced the crystal-rich ignimbrite. The central cauldron block was lowered at least 2000 m by downwarping and fault displacement, and remained largely intact. There is no evidence for resurgent doming of the cauldron after subsidence, although igneous activity continued with intrusion of an adamellite ring pluton along much of the cauldron margin. The crystal-rich ignimbrite and the ring pluton are similar in composition and may have been successive products of a common magma source that sustained this simple, single cauldron cycle.

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39

Hill, Michael, and Michael Armstrong. "COAL SEAM METHANE: THE FUTURE OF OPERATIONS IN NEW SOUTH WALES." APPEA Journal 31, no. 1 (1991): 367. http://dx.doi.org/10.1071/aj90029.

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The coal seams of the coal basins in New South Wales contain vast resources of methane. The gas has been of interest in the past, principally because the inflow of significant quantities into coal mine workings is a danger to mine safety and reduces production. Drainage techniques have been introduced into deeper collieries but they have not proved to be totally effective.Surface pre-drainage operations using hydraulic fracturing to stimulate gas production have been successful in the United States over recent years. The technique has yet to be successfully tested in New South Wales but if effective it will enable future mining areas to be drained prior to commencement of mining. The technique will also enable commercial production of large quantities of methane from both within and outside the coal mining areas.Seven organisations have commenced or will soon commence the exploration and development of the State's coal seam methane resources. Total planned expenditure over the next two years is over $4 000 000. Other Australian and overseas organisations are actively reviewing investment opportunities.Detailed exploration programs will be required prior to the commencement of operations because of the relative lack of data on the geology and gas resources of the basins. Differences exist between Australian and American coals and comparative reservoir and pilot studies will be required to determine the most effective pre-drainage methods. Potential markets exist in the State for methane and changes have been made to relevant legislation and administrative procedures to create incentives for exploration and production. Careful land-use planning will be required to ensure that the gas resource is not sterilised.

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40

Mackey, Timothy, Kenneth Lawrie, Paul Wilkes, Tim Munday, Nadir de Souza Kovacs, Roslyn Chan, Dave Gibson, Colin Chartres, and Ray Evans. "Palaeochannels near West Wyalong, New South Wales: A case study in delineation and modelling using aeromagnetics." Exploration Geophysics 31, no. 1-2 (March 2000): 1–7. http://dx.doi.org/10.1071/eg00001.

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41

Deen, Tara J., Karsten Gohl, Christopher Leslie, Eva Papp, and Kevin Wake-Dyster. "Seismic refraction inversion of a palaeochannel system in the Lachlan Fold Belt, Central New South Wales." Exploration Geophysics 31, no. 1-2 (March 2000): 389–93. http://dx.doi.org/10.1071/eg00389.

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42

ALAM, M. MUSTAFA, KEITH A. W. CROOK, and GRAHAM TAYLOR. "Fluvial herring-bone cross-stratification in a modern tributary mouth bar, Coonamble, New South Wales, Australia." Sedimentology 32, no. 2 (April 1985): 235–44. http://dx.doi.org/10.1111/j.1365-3091.1985.tb00506.x.

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43

NICHOL, SCOTT L., BRIAN A. ZAITLIN, and BRUCE G. THOM. "The upper Hawkesbury River, New South Wales, Australia: a Holocene example of an estuarine bayhead delta." Sedimentology 44, no. 2 (April 1997): 263–86. http://dx.doi.org/10.1111/j.1365-3091.1997.tb01524.x.

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44

Barron, L. M., B. J. Barron, T. P. Mernagh, and W. D. Birch. "Ultrahigh pressure macro diamonds from Copeton (New South Wales, Australia), based on Raman spectroscopy of inclusions." Ore Geology Reviews 34, no. 1-2 (September 2008): 76–86. http://dx.doi.org/10.1016/j.oregeorev.2007.07.003.

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45

England, B. M., and J. Ostwald. "Framboid-derived structures in some Tasman fold belt base-metal sulphide deposits, New South Wales, Australia." Ore Geology Reviews 7, no. 5 (January 1993): 381–412. http://dx.doi.org/10.1016/0169-1368(93)90002-g.

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46

Pohler, Susanne M. L. "Devonian carbonate buildup facies in an intra-oceanic island arc (Tamworth Belt, New South-Wales, Australia)." Facies 39, no. 1 (December 1998): 1–34. http://dx.doi.org/10.1007/bf02537009.

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47

Slansky, J. M. "Geochemistry of high-temperature coal ashes and the sedimentary environment of the New South Wales coals, Australia." International Journal of Coal Geology 5, no. 4 (December 1985): 339–76. http://dx.doi.org/10.1016/0166-5162(85)90002-3.

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48

Bryant, E. A., R. W. Young, D. M. Price, and S. A. Short. "Late Pleistocene dune chronology: Near-coastal New South Wales and eastern Australia." Quaternary Science Reviews 13, no. 3 (January 1994): 209–23. http://dx.doi.org/10.1016/0277-3791(94)90026-4.

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49

Hegarty, Rosemary. "Interpretation of aeromagnetic and gravity data from western New South Wales – identifying basin and basement geology." ASEG Extended Abstracts 2012, no. 1 (December 2012): 1–4. http://dx.doi.org/10.1071/aseg2012ab281.

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50

McNally, G. H. "Geology and mining practice in relation to shallow subsidence in the Northern Coalfield, New South Wales." Australian Journal of Earth Sciences 47, no. 1 (February 2000): 21–34. http://dx.doi.org/10.1046/j.1440-0952.2000.00761.x.

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Journal articles on the topic 'Geology New South Wales Bermagui'

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