Academic literature on the topic 'Marlborough'

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Journal articles on the topic "Marlborough"

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Astuti, Hesti Anggi, Dafid Setiana, and Denik Agustito. "EKSPLORASI ETNOMATEMATIKA PADA BENTENG MARLBOROUGH." UNION: Jurnal Ilmiah Pendidikan Matematika 9, no. 3 (November 30, 2021): 289–95. http://dx.doi.org/10.30738/union.v9i3.9306.

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Penelitian ini bertujuan untuk mengeksplorasi kandungan matematika pada benteng Marlbororugh serta menjabarkannya ke dalam matematika di sekolah. Metode dalam penelitian ini adalah metode penelitian kualitatif dengan pendekatan etnografi. Teknik pengumpulan data dilakukan dengan metode observasi, wawancara, dan dokumentasi. Hasil penelitian menunjukan kandungan matematika yang ada pada benteng Marlbororugh berupa: segitiga, trapesium, persegi panjang, persegi, dan balok. Sedangkan konsep matematika yang dapat dikembangkan adalah mencari luas, keliling serta volume bangun geometri pada benteng Marlborough.
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Ivonina, L. I. "The Trial in Parliament over the Duke of Marlborough: Verity or Falsification?" Izvestiya of Saratov University. History. International Relations 12, no. 2 (2012): 49–54. http://dx.doi.org/10.18500/1819-4907-2012-12-2-49-54.

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The article examines the judicial process in the British Parliament over John, the Duke of Marlborough, accused of embezzlement of funds and assignment of invested significant sums. The author suggests that Tory Parliament sought to justify Marlborough’s denial of all his command posts and his dismissal of high politics. In this sense, charges of the Duke were largely falsified.
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Rolls, R. "The Marlborough Doctors." BMJ 310, no. 6988 (May 6, 1995): 1208. http://dx.doi.org/10.1136/bmj.310.6988.1208.

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Spencer, Charles. "Book Review: Marlborough: John Churchill, Duke of Marlborough, Hero of Blenheim." War in History 13, no. 3 (July 2006): 394–97. http://dx.doi.org/10.1177/096834450601300313.

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Beresford, R. M., P. J. Wright, P. N. Wood, and R. H. Agnew. "Sensitivity of grapevine powdery mildew (Erysiphe necator) to demethylation inhibitor and quinone outside inhibitor fungicides in New Zealand." New Zealand Plant Protection 69 (January 8, 2016): 1–10. http://dx.doi.org/10.30843/nzpp.2016.69.5908.

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Isolates of Erysiphe necator from Hawkes Bay and Marlborough vineyards were tested for sensitivity to three demethylation inhibitor (DMI) fungicides (myclobutanil penconazole and cyproconazole) and one quinone outside inhibitor (QoI) fungicide (trifloxystrobin) Mean colony diameter was determined in a detached grape leaf assay for approximately 20 isolates per vineyard at 1 and 10 mg/litre of each fungicide Resistance to trifloxystrobin was prevalent in Hawkes Bay and Marlborough Mycobutanil resistance was found in both regions but particularly in Marlborough There was some loss of sensitivity to penconazole particularly in Marlborough Cyproconazole showed greater efficacy against E necator than the other two DMIs tested There was no explanation for the high trifloxystrobin resistance in sampled vineyards with few reports of trifloxystrobin use For DMIs there was a strong relationship between number of DMI fungicide applications over 10 years and DMI resistance across all three DMI active ingredients in both regions
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Anto, Monalisa Putri, Sofian Sofian, and Fauzan Fauzan. "THE INFLUENCE OF ONLINE ADVERTISING ON THE INCREASE OF TOURISTS VISITING THE MALBOROUGH FORT, BENGKULU CITY." Dynamic Management Journal 7, no. 3 (July 27, 2023): 369. http://dx.doi.org/10.31000/dmj.v7i3.8784.

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Penelitian bertujuan untuk mengetahui besarnya pengaruh youtube (X1) facebook (X2) serta instagram (X3) pada minat berkunjung wisatawan (Y), di Benteng Marlborough. Dengan metode menggunakan skala Likert dengan membagikan kuisioner kepada responden. penelitian menggunakan metode kuantitatif.Populasi diambil penelitian ialah wisatawan berkunjung ke objek wisata telah ditentukan yaitu Benteng Marlborough. Data diperoleh pada penelitian dibuat menggunakan software SPSS19.Analisis digunakan penelitian ini ialah analisis regresi berganda Hasil Penelitian menunjukan: (1)Youtube (X1) Mempunyai pengaruh yang signifikan terhadap wisatawan berkunjung (Y). (2) Facebook (X2) Mempunyai pengaruh yang signifikan terhadap wisatawan berkunjung (Y). (3) Instagram (X3) Mempunyai pengaruh secara simultan terhadap wisatawan berkunjung (Y)di Benteng Marlborough. (4) Youtube, facebook dan instagram berpengaruh secara simultan.
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Levillain, Charles-Édouard. "Churchill historien de Marlborough." Commentaire Numéro 139, no. 3 (2012): 781. http://dx.doi.org/10.3917/comm.139.0781.

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SOKOLOV, IGOR M. "Eight new species of the genus Nesamblyops Jeannel (Anillini: Carabidae: Coleoptera) from New Zealand with notes about dispersal of the genus to the North Island." Zootaxa 5230, no. 2 (January 20, 2023): 179–201. http://dx.doi.org/10.11646/zootaxa.5230.2.3.

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Species of flightless litter ground beetles of the tribe Anillini, genus Nesamblyops, from the North Island and from the north-eastern part of the South Island are revised. Eight new species are described and one previously known species, Nesamblyops oreobius (Broun), is re-described. Nesamblyops oreobius, the only hitherto recorded species from the North Island, is most similar to the group of two new species from the South Island, N. confusus n. sp. (type locality: New Zealand, Marlborough Sounds, Mount Stokes) and N. lescheni n. sp. (type locality: New Zealand, Marlborough Sounds, D’Urville Island), based on the structure of the male genitalia. The second species of the genus known from the North Island, N. tararua n. sp. (type locality: New Zealand, Wellington, Tararua Range) represents another lineage, based on the structure of the male genitalia, and is closely related to a group of three new species from the South Island, N. brouni n. sp. (type locality: New Zealand, Canterbury, Southern Alps, Lewis Pass), N. distinctus n. sp. (type locality: New Zealand, Marlborough, Richmond Range, Fabians Valley), and N. townsendi n. sp. (type locality: New Zealand, Marlborough Sounds, Tennyson Inlet). Nesamblyops carltoni n. sp. (type locality: New Zealand, Nelson, Richmond Range, Dun Mountain) and N. parvulus n. sp. (type locality: New Zealand, Marlborough Sounds, Mount Stokes), both from the South Island occupy an isolated position among the examined species. All species are illustrated with digital images of habitus, body parts, and drawings of genitalia. Distribution maps for all species are also provided. Geographical evidence of Nesamblyops dispersal to the North Island is discussed, based on distributional data.
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Asen, K. "The Marlborough Family Day Unit." Bulletin of the Royal College of Psychiatrists 12, no. 3 (March 1988): 88–90. http://dx.doi.org/10.1192/s014007890002126x.

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The Marlborough Family Day Unit has been in existence for 10 years. It is part of the Marlborough Family Service, a community-based psychiatric service for patients of all ages. Its location is the site of the former Marlborough Day Hospital in London NW8. The Day Unit was created in 1977 by Dr Alan Cooklin who is still the consultant in charge of the whole service. The reason for setting up such a unit was to experiment with new ways of dealing with what is now so fashionably termed ‘multi-problem families’. These are families where one or more members have been in extensive contact with psychiatric and social services. Multiple hospitalisations, removal of children into care, and general chaotic behaviour are the presenting ‘symptoms’. Such families have unrivalled skills in collecting agencies and professionals like flypaper and making it very difficult for anyone to leave the field given the enormous anxiety created all round.
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Bell, M. "Spread of Chilean needle grass (Nassella neesiana) in Marlborough New Zealand." New Zealand Plant Protection 59 (August 1, 2006): 266–70. http://dx.doi.org/10.30843/nzpp.2006.59.4417.

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Chilean needle grass (Nassella neesiana) is a containment pest in the Regional Pest Management Strategy for Marlborough It is of concern because it has sharptipped seeds that bore into the eyes and pelts of livestock Discovered in Marlborough in the 1930s it now infests 4311 ha In 1987 18 properties were infested increasing to 53 by 2000 and 96 by December 2005 In addition both the range and density of Chilean needle grass has increased significantly since 1987 and to date no infestations have been eradicated Failure to stop this spread is due to the difficulty of both identification and control Effective control and land management methods for this weed are urgently needed The probability of this weed spreading further both within and beyond Marlborough appears to be high This conclusion along with land use changes has implications for the review of the Regional Pest Management Plan
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Dissertations / Theses on the topic "Marlborough"

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Sheldon-Sayer, Lynne. "The vegetation of Maud Island, Marlborough, New Zealand." Lincoln University, 2006. http://hdl.handle.net/10182/1707.

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Maud Island (Te Hoiere - "a long paddle or mighty pull") is a moderately sized island of 309 hectares, located in the Pelorus Sound (41°, 02 'S, 173° 54 'E) Marlborough, at the north-east end of the South Island of New Zealand. It has a long history of human modification and impacts since its colonisation by Maori and early Europeans. The vegetation of Maud Island has been studied in the 1980's and again in the early 1990's. The objectives of this study were to (1) describe how the vascular plant communities vary in species composition across Maud Island, (2) determine which environmental factors are important predictors of the variation in species composition of Maud Island plant communities, and (3) describe the pattern of succession of the plant communities on Maud Island over the last twenty years. In this 2001 study, I comprehensively sampled the vegetation on Maud Island using a Reconnaissance Description Procedure in a total of 158 plots across the island and compared these results to previous descriptions. I also retook photos at permanent photo points to provide a visual comparison of vegetation change. In total, 219 plant species were identified; 177 species occurred within the plots and 42 additional species were observed while walking around the coastline and walking tracks. Six dominant plant species occurred in over 70% of the plots. They were Pteridium esculentum, Pseudopanax arboreus, Hebe stricta var. stricta, Melicytus ramiflorus, Ozothamnus leptophylla and Coprosma robusta. Two-Way Indicator Species Analysis resulted in the description of eight different plant communities on the island. Detrended correspondence analysis showed a high degree of turnover in species composition among these communities. Canonical correspondence analysis showed that slope and moisture were particularly important predictors of variation in plant species composition. The environmental factors that best predicted to variation communities were slope, moisture, and a gradient in historical disturbance. Comparisons of present and past vegetation maps and photos (ground and aerial) showed, in terms of the successional pathways of the vegetation on Maud Island, that over time, the vegetation is reverting from short stature grassland and scrub to predominantly forest scrub and young secondary forest.
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Norrie, Brendon Paul. "The development of viticulture and winemaking in Marlborough." Thesis, University of Canterbury. Geography, 1990. http://hdl.handle.net/10092/1986.

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A recent historical geography examining the development and evolution of a winegrowing region of New Zealand. The development of Marlborough as the nation's major viticultural location has been one of the most important developments of New Zealand’s continued growth as a wine producer. The major emphasis of this study is on the wine companies who got involved in Marlborough and have built wineries in the region. The scale of each operation and the many different reasons for each individual or companies involvement were examined and discussed. An important area of this study has been the principle reasons leading to Montana Wines deciding to plant vineyards in Marlborough in 1973. A major finding has been that there has been considerable over-emphasis on the physical characteristics of the Marlborough region and a neglect of the other “human factors” the major one being the availability of land and the price of land in explaining the region's development as a wine producer. The development of Marlborough has occurred over four stages. These are: a) The initial action by one company which pioneers a new landuse; b) If successful further development occurs by both small and large producers; c) International interest and participation; and d) end of first phase of development. Marlborough has yet to reach full maturity, because there is still some experimentation occurring with different vine varieties.
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Lauder, Glen A. "Coastal landforms and sediments of the Marlborough Sounds." Thesis, University of Canterbury. Geography, 1987. http://hdl.handle.net/10092/4518.

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This thesis examines coastal form and sediments of the Marlborough Sounds, New Zealand. An important aspect of coastal behaviour in this landscape stems from linkages between catchment and coast. Focus is therefore placed on the manner in which sediment delivered from catchment sources is redistributed within the shore and offshore domains. Coastal response is shown to depend on two factors: the form of the receiving sites and the mobility of sediments within them. Investigation of coastal landforms at a range of scales identifies the framework within which sedimentation takes place. Consideration of landscape sediment redistribution at Quaternary, Holocene and human timescales establishes the locations in the coastal landscape in which change has taken place. A key factor in coastal response relates to the wide size range of sediments delivered. The fractionation of sediment within the coastal domains is used as an index by which to identify the controls on coastal sedimentation. A new conceptual model of coastal behaviour, the Ordered Response Model, is developed as a framework within which to investigate coastal response. The model is operationalised in three ways. This is done first with regard to coastal sediments and their grain-size interpretation, secondly in the context of shoreline form and sediment redistribution, and thirdly in relation to form and sediment trapping within coastal embayments. The patterns of sediment redistribution are seen to reflect trapping behaviour in the coastal landscape at a range of scales. Sediments are investigated from the viewpoint of the factors which determine their retention or accumulation in or rejection from a coastal site. Shore sites are distinguished on the basis of the extent to which they trap materials delivered to them from catchment sources. Governing factors are shoreline gradient and size grade of materials. A primary fractionation of sediments takes place at the shore and the finer fractions are by-passed to the nearshore. Sediment fractions that are relatively immobile under prevailing environmental conditions develop paved lag surfaces at a range of scales. Sediments that accumulate at the shore are distinctive in their mixed sand and xv gravel composition with a dominant mode in the granule and very coarse sand grades (-291 to 091). Sediment deposited on the intertidal surfaces is found to be redistributed by a distinctive mechanism. Migratory intertidal bedforms defined here as "clastic waves" are a means by which the low energy shores disperse sediment which is delivered to them. These waves are a distinctive form of the shoreline of the Marlborough Sounds, and have attributes different from other shoreline forms identified in the literature. Clastic waves are shore-parallel, crescentic or lunate forms with longshore crest dimensions of 0.5 to 30m, length dimension perpendicular to the crest of up to 20m, and crest heights of 0.05m to 0.5m. Rates of intermittent migration vary from 1m/day to 10m/year. Key factors in their development are identified as low wave energy, tidal range, intermediate to low intertidal gradients (<1:20) and a mixed sand and fine gravel grain-size. Bathymetric form is found to reflect the varying influence of sub-bottom morphology, sediment accumulation and hydraulic reworking. Analysis of sediment thickness identifies a mean thickness over sub-bottom of 7.33m in Pelorus Sound. Spatial variations in sediment thickness identifY marginal embayments as significant sediment traps. Mean sedimentation rates calculated over a 6,000 year timespan give Pelorus Sound a spatially averaged rate of 1.22mm/yr. Sub-bottom form is shown to have a stronger role in determining bathymetric form than previously reported. Due to the constraining effect of shallow sub-bottom form on sedimentary processes sediment thicknesses in the inner Pelorus Sound are not greater than those found in channels or embayments in the middle reaches of the Sound. A mean thickness of 5.75m from sub-bottom seismic profiles in the inner Pelorus equates to a sedimentation rate of 0.96mm/year over 6,000years, at about which time the river valleys of the Marlborough Sounds were drowned by postglacial rising sea-levels. Analysis of sub-bottom form reveals evidence of previously unreported drowned terrace remnants, which are correlated to subaerial terrace remnants. On the basis of both long profile patterns along these remnant surfaces and an analysis of bathymetric form of marginal bays and channels, an interpretation is developed of the origin of form in Pelorus Channel and Tory ChanneL Sediment trapping behaviour is identified as the most distinctive attribute of this coastal landscape, and shown to operate at a range of nested scales. As a XVI consequence of trapping behaviour, the operation of any part of this coastal landscape must be considered in relation to its operation as a whole.
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Vickery, Sara. "Cenozoic deformation in a plate-boundary zone, Marlborough, New Zealand." Thesis, University of Oxford, 1994. https://ora.ox.ac.uk/objects/uuid:590f1ea6-6d9e-4ed0-93ee-9d82e52e6be9.

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The Marlborough Fault System is a zone of dextral transpression in continental crust at the southern end of the Hikurangi subduction system between the obliquely convergent Australian and Pacific plates. Detailed mapping of an area of deformed Tertiary cover sequence on the down thrown side of the Kekerengu Fault (the Kekerengu- Washdyke study area) has revealed two phases of deformation, De and Dl. In the study area De consists of nine kilometre scale thrust faults cutting sediments derived from extra- and intra-basinal uplift. The timing of this episode is constrained by the age of the first clastic deposits and by a previously unidentified unconformity in this area of Late Miocene age. A clear sequence of Dl events is recognized deforming all earlier structures including Pliocene aged sediments. Although elsewhere in Marlborough a regional post-Pliocene ca. 20° clockwise block rotation has been previously identified, in the Kekerengu-Washdyke study area one site suggested no post-Pliocene rotation and another a large ca. 100° clockwise rotation. This lack of Dl rotation was unexplained and the large rotation attributed to localized Early Miocene deformation. Palaeomagnetic work carried out in this study has identified six more sites which contain this large rotation (average ca. 118+11°). The rotation therefore appears to be a regional event, likely to be a result of the location of Marlborough in the hinge zone at the southern end of the Hikurangi Margin. One site from dykes in basement rocks does not record this large rotation, indicating that the rotation occurred in upper layers detached from unrotating rock below by an unknown structure (such as a thrust fault), or that the rotation did not occur in this area. The large rotation is believed to have been achieved by pinning of the De thrusts to the south of the Marlborough region. The data suggests that the De thrusts in Marlborough were initially NW-trending and seaward, not landward-directed as was previously supposed. Palaeomagnetic work has also added to the evidence for a lack of Dl regional rotation on the downthrown side of the Kekerengu Fault. A previously unidentified second phase of Dl folding and 'bending' within the study area appears to have accommodated the regional rotation and suggests that the Kekerengu Fault acted as the eastern boundary of the Dl rotating block.
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Morris, John C. "The stratigraphy of the Amuri limestone group, east Marlborough, New Zealand." Thesis, University of Canterbury. Geology, 1987. http://hdl.handle.net/10092/5614.

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An extensive study of the stratigraphy of the Amuri Limestone Group (Upper Cretaceous Upper Eocene) and the enclosing units in East Marlborough has been undertaken. The study includes regional correlation of detailed measured sections in conjunction with lithofacies descriptions, micropaleontological age determinations, petrographic examination, and geochemical analysis. A revised New Zealand Paleogene time scale has been compiled to take into account recent major revisions of international Cenozoic geochronology. The Amuri Limestone Group (c.660m maximum thickness) incorporates 6 formations: Mead Hill Formation (mid Haumurian - lower Waipawan); Teredo Limestone (mid Waipawan late Mangaorapan); Lower Limestone (mid Waipawan – mid Mangaorapan); Lower Marl (upper Waipawan - lower Heretaungan); Middle Limestone (lower Mangaorapan - lower Bortonian); Upper Marl (upper Porangan - upper Runangan). The Mead Hill Formation is diachronous and conformable on the Upper Iwitahi Group which includes the Woolshed Formation (lower - upper Haumurian) and the overlying Claverley Sandstone (upper Haumurian). The Mead Hill Formation contains the Flaxbourne Limestone Member (mid Haumurian) and Lower Chert Member (late Haumurian). The Lower Limestone contains the Upper Chert Member (mid Waipawan). The Fells Greensand Member (mid Bortonian) and Grass Seed Volcanics Member (upper Bortonian) are both intercalated within the Middle Limestone and Upper Marl. With the exception of post-unconformity sandy facies, the Amuri Limestone consists of dcm-bedded, light greenish grey, well indurated, foraminiferal biomicritic calcilutites and poorly indurated, smectite-rich marls. Macrofossils are extremely rare. Cretaceous sequences are characterized by a poorly developed Planolites - Teichichnus ichnoassemblage; Paleogene facies are dominated by a Zoophycos - Planolites ichnoassemblage. Pelagic limestone deposition was initiated within a central NW-trending trough and spread outwards onto the adjacent near-horizontal platform. Subsidence of the trough is inferred to have been maintained by reactivation of basement faults. Water depths on the platform are likely to have been relatively shallow (inner shelf) during the Late Cretaceous but much deeper (outer shelf - bathyal) during the Paleocene and Eocene. Basin morphology was the major control on lateral facies variations. Platform sediments are characteristically more thinly bedded, and the thickness of individual Formations is correspondingly attenuated, in comparison with trough facies. Chert and dolomite are restricted to the lower parts of the trough facies. Basin-wide unconformities are recognized in the late Haumurian, mid Waipawan (sub-Teredo Limestone unconformity), mid Bortonian, and mid Whaingaroan. Although these breaks are disconformable in platform areas, they regionally account for large amounts of differential erosion. Submarine erosion, hardground formation, development of a Thallasinoides-dominated ichnofauna, glauconitization, phosphatization, and accumulation of a thin sandy facies are typical of unconformities outside the trough. Within the trough, the Haumurian and Waipawan breaks in deposition are represented by paraconformities or coevally deposited siliceous, pyritic mudstones. The subfeldsarenitic Claverley Sandstone was intra-basinally derived from submarine erosion and reworking of the underlying Woolshed Formation. The detrital sand fraction of the Teredo Limestone was derived from reworking of the locally exhumed Claverley Sandstone, and from remobilization at depth and submarine extrusion of that unit. An extra-basinal source (possibly reworked quartzose coal measures) for the redeposited supermature quartzarenitic Fells Greensand is likely. Pulses of (compressional?) tectonic activity immediately preceded and possibly continued during unconformity development. These tectonic events may provide an independent estimate of the timing of some of the major (Late Cretaceous - Cenozoic) plate tectonic events affecting the New Zealand region. The amount of dextral movement on two of the major Marlborough Faults has been estimated from offsets in lithofacies and isopach patterns. 5-10km of transcurrent movement is recognized on the northern branch of the Hope Fault; 10-15km of right-lateral slip has occurred on the Kekerengu Fault.
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Frezzati, Marco. "Wine tanks in Marlborough, New Zealand. Observed seismic damage and design criteria." Master's thesis, Alma Mater Studiorum - Università di Bologna, 2019.

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Il settore dell’industria vinicola in Nuova Zelanda è in forte crescita con un aumento dell’export di circa il 24% ogni anno. Nella regione di Marlborough viene prodotto il 77% della produzione vinicola dell’intera nazione. Questa zona ha subito due eventi sismici, il terremoto di Lake Grassmere nel 2013 e di Kaikoura nel 2016, che hanno causato ingenti danni ai serbatoi d’acciaio utilizzati per lo stoccaggio e fermentazione delle uve. Questi danneggiamenti hanno evidenziato delle carenze nella progettazione di dettaglio. Per la progettazione sismica dei serbatoi d’acciaio esistono delle linee guida dal 1986 (aggiornate nel 2009) rilasciate dalla “New Zealand society of earthquake engineering” o NZSEE. Questa guida non offre indicazioni sul progetto dei dettagli costruttivi tipici dei serbatoi da vino o su come progettare secondo la gerarchia delle resistenze quando si ulizzano ancoraggi duttili per fissare il serbatoio alla fondazione. In questo elaborato vengono confronate le linee guida neo zelandesi con due norme internazionali sulla progettazione sismica dei serbatoi: l’Eurocodice 8 e le API650. Il confronto avvienen attravenso la progettazione di 6 serbatoi da vino tipici di Marlborogh in modo da evidenziare le differenze sugli sforzi. I risultati mostrano che gli sforzi calcolati con le diverse normative sono paragonabili. Inoltre le mancanze della linea guida neo zelandese non sono coperte neanche da EC8 o da API650. Vieni qui inoltre presentato un metodo per costruire la curva di capacità del serbatoio ancorato alla base attraverso l’uso della “Monolithic beam analiogy” o MBA. Questa permette di stimare la gerarchia delle resistenze e valori di sforzo sui vari elementi di dettaglio. Il modello viene applicato su 3 serbatoi che hanno subito danni dal terremoto di Kaikoura 2016 attraverso l’utilizzo del “Capacity spectrum method” che stima lo spostamento subito da una struttura in caso di evento sismico quando si conosce la curva di capacità della stessa.
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Jowett, T. W. D. "An investigation of the geotechnical properties of loess from Canterbury and Marlborough." Thesis, University of Canterbury. Engineering Geology, 1995. http://hdl.handle.net/10092/7580.

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Tunnel gully erosion is common in the loess deposits of the South Island of New Zealand. The loess deposits found on the Wither Hills (Marlborough) and Port Hills (Banks Peninsula) are prone to extensive tunnel gully erosion which has caused significant damage in both rural and urban areas. However, the loess deposits found on the Timaru Downs (South Canterbury) and the hills surrounding Akaroa (Banks Peninsula) are significantly less affected. Geotechnical tests including pinhole erosion, uniaxial expansion, crumb test and dispersion % were carried out to determine the erosive and dispersive characteristics of loess samples from locations in the aforementioned areas. From this data, the extent to which geotechnical properties influence the incidence of tunnel gully erosion was determined. Other geotechnical characteristics such as grain size, clay mineralogy, exchangeable sodium content and insitu dry density were also evaluated in order to determine the controlling factors on the erosive and dispersive characteristics of the different loess samples. In general, it was found that laboratory test results did not correlate fully with field erodibility. For instance, the two non tunnel gullied soils exhibited characteristics which suggested that they should be prone to tunnel gully erosion. The lack of correlation between laboratory test data and field erodibility suggests that other factors such as climate, land use and soil profile characteristics are important in determining the occurrence of sub-surface erosion. A comparison was made of the loess stabilising properties of an enzyme based product known as Endurazyme and quicklime (CaO), a commonly used loess stabiliser. Tests were carried out on samples from the Timaru Downs and the Ahuriri quarry on Banks Peninsula. It was found that Endurazyme has a negligible effect on important geotechnical properties such as erodibility, dispersivity, durability, strength and maximum dry density/optimum moisture content.
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Goodman, Jane M. "The ecology and conservation of shortjaw kokopu (Galaxias postvectis) in Nelson and Marlborough." Thesis, University of Canterbury. Department of Zoology, 2002. http://hdl.handle.net/10092/4310.

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The short jaw kokopu (Galaxias postvectis) is a threatened New Zealand freshwater fish (family Galaxiidae) that migrates between freshwater habitat and the marine environment during its life cycle. The influence of this diadromous life-cycle, as well as the potential effect of introduced predatory fish on the population dynamics and habitat occupancy of short jaw kokopu were investigated in the Nelson Marlborough Department of Conservation conservancy. The distribution and abundance of short jaw kokopu were measured using spotlighting, substantially increasing their known range in this area. Juveniles (<100 mm FL) were recorded from the same stream reaches as adults using this method. Short jaw kokopu were positively associated with native forest, however they occupied a wide range of streams and habitat variables were not accurate predictors of their presence and absence. Diadromy had a large influence on fish communities at low- to mid- elevation sites. Short jaw kokopu were associated with the presence of other diadromous species, in particular other migratory galaxiids. Juvenile galaxiids were able to migrate through modified stream reaches, but the density of juvenile galaxiids significantly decreased with increasing distance from the sea. The number of juveniles recruiting to the adult population was probably influenced by the biomass of piscivorous fish species (e.g. introduced trout) and the cumulative effects of habitat modifications downstream. Short jaw kokopu and trout co-occurred at the reach scale, however short jaw kokopu were more likely to be absent when trout abundance was high. Negative interactions between short jaw kokopu and trout may be offset by diadromy, whereby individuals eaten or displaced are constantly replaced by juveniles returning from the marine environment. Conservation effort should be aimed at mitigating the deleterious effects of habitat degradation and migration barriers on short jaw kokopu and other migratory fish popUlations. Further research is needed to properly understand the effect that introduced trout have had on native migratory fish species.
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Irvine, Janelle Rose Mae. "Sedimentology, stratigraphy and palaeogeography of Oligocene to Miocene rocks of North Canterbury-Marlborough." Thesis, University of Canterbury. Geological Sciences, 2012. http://hdl.handle.net/10092/6826.

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The Cenozoic was a time of climatic, tectonic and eustatic change in the Southern Hemisphere. Cooling at the pole, glaciation and substantial sea ice formation occurred as latitudinal temperature gradients increased and tectonics altered Southern Hemisphere circulation patterns. During this same time frame, the tectonic regime of the New Zealand continental block transitioned from a passive margin to an active plate boundary, resulting in the reversal of a long-standing transgression and an influx of terrigenous sediment to marine basins. In this transition, depositional basins in the South Island became more localized; however, the influence of oceanographic and tectonic drivers is poorly understood on a local scale. Here we apply sedimentological, biostratigraphic and geochemical analyses to revise understanding of the effects of the changing climatic regime and active tectonics on the development of Oligocene and Miocene rocks in the Northern Canterbury Basin. The Late Oligocene to Middle Miocene sedimentary rocks of the northern Canterbury Basin record oceanographic and tectonic influences on basin formation, sediment supply and deposition. The Palaeocene to Late Eocene Amuri Formation in the basin are micrites and biogenic cherts recording deepwater, terrigenous-starved environments, and do not show any influence of active tectonics. The Early Oligocene development of ice on the Antarctic continent and the associated global sea level response is reflected in this basin as the Marshall Paraconformity, an eroded, glauconitized and phosphatised firm ground and hardground atop the Amuri. Sedimentation above this unconformity resumed in the Late Oligocene-Early Miocene with cleaner, deep-water, bathyal planktic foraminifera packstones and wackestones in eastern areas and Late Oligocene inner shelf volcaniclastic packstones in parts of the western basin. Post-unconformity sedimentation resumed earlier in western areas, as the currents responsible for scouring the sea floor moved progressively to the east. The development of tectonic uplift in terrestrial settings is first seen in the northwestern basin in Lower Miocene fine quartz-rich sandstones, and by the Middle Miocene, bathyal sandstones and quartz-rich wackestones appear in the basin, replacing earlier, more pure carbonates. The uplift caused shallowing to the west, in the form of shelf progradation due to sediment influx. This shallowing is not observed to the east; instead, the palaeoenvironments show a deepening as a result of sea level rise.
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Audru, Jean-Christophe. "De la subduction d'hikurangi a la faille alpine, region de marlborough, nouvelle zelande." Nice, 1996. http://www.theses.fr/1996NICE5041.

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En nouvelle zelande, la transition structurale de la subduction d'hikurangi a la collision sur la faille alpine s'effectue par le systeme de failles de marlborough (sfm). A terre, l'analyse structurale du sfm revele qu'apres inversion tectonique, des decrochements et des failles inverses accommodent la convergence oblique. Les premiers sont associes a des structures en fleur, les secondes agissent en failles de transfert ou en relais compressifs. Le developpement de bassins sedimentaires contre les decrochements a enregistre la rapide propagation de la tectonique coulissante a tout le sfm des le miocene inferieur (24 ma). En mer, des structures transpressives actives sont reconnues dans la plate-forme continentale de marlborough. Elles delimitent ou recoupent d'epais bassins sedimentaires et connectent le sfm aux decrochements de l'ile nord ainsi qu'aux chevauchements frontaux de la subduction. La morphologie de la plaque plongeante controle fortement la geometrie et l'activite sismique des structures de la plaque superieure. Le couplage sismique, avec l'obliquite de la convergence, contribue largement a la geometrie des reliefs ainsi qu'a la distribution de la deformation decrochante. La topographie de la zone de transition traduit le partage de la deformation: il s'exprime au-dessus de la subduction par une chaine en decrochement et une chaine en compression. Le controle de la tectonique sur le relief permet de determiner les traces de nouvelles failles actives qui se connectent a la faille alpine. Le mnt suggere en outre que les coulissements cumules atteignent 15 a 50 km sur les decrochements
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Books on the topic "Marlborough"

1

Alatalo, Susan. Marlborough. Charleston, SC: Arcadia, 2004.

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R, Jones J. Marlborough. Cambridge: Cambridge University Press, 1993.

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Phyllis, Tuchman, and Seattle Art Museum, eds. Chihuly Marlborough. 2nd ed. [S.l: s.n.], 2001.

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Bowker, Richard. Marlborough Street. Garden City, N.Y: Doubleday, 1987.

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Benson, E. F. Sketches from Marlborough. Harleston, Norfolk: Hermitage Books, 1992.

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Kalaugher, Mike. The Marlborough mystery. Auckland, N.Z: Tandem Press, 2001.

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Treasure, Dorothy. Francis Frith's Marlborough. Salisbury, Wiltshire: Frith Book Co., 2001.

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Robertson, Kevin. The Marlborough Branch: The railways of Savernake and Marlborough. Pinner: Irwell Press, 1990.

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Chandler, David. Marlborough as military commander. 3rd ed. Speldhurst: Spellmount, 1989.

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Brooks, Cynthia. Marlborough wines and vines. Renwick: Graham and Cynthia Brooks, 1992.

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Book chapters on the topic "Marlborough"

1

McCulloch, Gary. "Marlborough and Harrow." In Cyril Norwood and the Ideal of Secondary Education, 79–99. New York: Palgrave Macmillan US, 2007. http://dx.doi.org/10.1057/9780230603523_6.

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Thompson, R. W. "Chapter VI." In The Yankee Marlborough, 92–114. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-7.

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Thompson, R. W. "Chapter III." In The Yankee Marlborough, 44–60. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-4.

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Thompson, R. W. "Chapter XI." In The Yankee Marlborough, 183–94. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-14.

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Thompson, R. W. "Chapter I." In The Yankee Marlborough, 21–35. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-2.

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Thompson, R. W. "Chapter II." In The Yankee Marlborough, 36–43. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-3.

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Thompson, R. W. "Chapter XIII." In The Yankee Marlborough, 208–30. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-16.

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Thompson, R. W. "Chapter XVIII." In The Yankee Marlborough, 323–54. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-22.

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Thompson, R. W. "Chapter VII." In The Yankee Marlborough, 117–32. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-9.

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Thompson, R. W. "Chapter IX." In The Yankee Marlborough, 149–62. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003194057-11.

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Conference papers on the topic "Marlborough"

1

Shanmuganathan, Subana, Ana Perez Kuroki, Ajit Narayanan, and Philip Sallis. "Modelling the seasonal climate variability and its effects on vintage wines from Marlborough, NZ." In 2011 Eighth International Conference on Fuzzy Systems and Knowledge Discovery (FSKD 2011). IEEE, 2011. http://dx.doi.org/10.1109/fskd.2011.6020061.

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Harbert, Sarah A., Alison R. Duvall, Rebecca Flowers, Gregory E. Tucker, Phaedra Upton, and Paul B. O'Sullivan. "EXHUMATION, MOUNTAIN BUILDING, AND LANDSCAPE EVOLUTION ACROSS THE MARLBOROUGH FAULT SYSTEM, SOUTH ISLAND, NEW ZEALAND." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321199.

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Witcher, Taylor Anne. "TESTING MODELS OF LITHOSPHERIC RHEOLOGY IN NEW ZEALAND: POSTSEISMIC COULOMB STRESS CHANGES CAUSED BY THE 1848 MARLBOROUGH EARTHQUAKE." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-277932.

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Duvall, Alison R., Camille Collett, Rebecca M. Flowers, Gregory E. Tucker, and Phaedra Upton. "TIMING AND STYLE OF KAIKOURA RANGE DEVELOPMENT AND MARLBOROUGH FAULTING, SOUTH ISLAND, NEW ZEALAND, FROM LOW-TEMPERATURE THERMOCHRONOLOGY." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302099.

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Reports on the topic "Marlborough"

1

Drew, Dennis M. Marlborough's Ghost: Eighteenth-Century Warfare in the Nuclear Age. Fort Belvoir, VA: Defense Technical Information Center, April 1985. http://dx.doi.org/10.21236/ada424804.

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