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Artículos de revistas sobre el tema "Orogenic belts – New South Wales"

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Publicado: 4 de junio de 2021
Última modificación: 31 de enero de 2023

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1

Glen, R. A., R. Spencer, A. Willmore, V. David, and R. J. Scott. "Junee – Narromine Volcanic Belt, Macquarie Arc, Lachlan Orogen, New South Wales: components and structure." Australian Journal of Earth Sciences 54, no. 2-3 (2007): 215–41. http://dx.doi.org/10.1080/08120090601146805.

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2

Roberts, J., X. Wang, and M. Fanning. "Stratigraphy and correlation of Carboniferous ignimbrites, Rocky Creek region, Tamworth Belt, Southern New England Orogen, New South Wales*." Australian Journal of Earth Sciences 50, no. 6 (2003): 931–54. http://dx.doi.org/10.1111/j.1400-0952.2003.01035.x.

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3

Shang, Zhi, and Yongqing Chen. "Petrogenesis and Tectonic Implications of Early Paleozoic Magmatism in Awen Gold District, South Section of the Truong Son Orogenic Belt, Laos." Minerals 12, no. 8 (2022): 923. http://dx.doi.org/10.3390/min12080923.

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The Truong Son orogenic belt (TSOB) is one of the most important orogenic belts in the Indochina block. There are numerous mafic to felsic intrusions in the Early Paleozoic caused by the Tethyan orogeny. However, the tectono-magmatic evolution of the TSOB in the Early Paleozoic is still unclear. In this paper, zircon U-Pb dating, whole-rock geochemistry, and the Sr-Nd isotopic data of the Early Paleozoic magmatic rocks have been systematically investigated to explore the petrogenesis and tectonic significance of these rocks in the TSOB. Based on our new results integrated with previous geologi
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4

Glen, R. A., and D. Wyborn. "Inferred thrust imbrication, deformation gradients and the Lachlan Transverse Zone in the Eastern Belt of the Lachlan Orogen, New South Wales." Australian Journal of Earth Sciences 44, no. 1 (1997): 49–68. http://dx.doi.org/10.1080/08120099708728293.

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5

Yılmaz, Yücel. "Southeast Anatolian Orogenic Belt revisited (geology and evolution)." Canadian Journal of Earth Sciences 56, no. 11 (2019): 1163–80. http://dx.doi.org/10.1139/cjes-2018-0170.

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The Southeast Anatolian Orogenic Belt consists of the Arabian Platform, a zone of imbrication, and a nappe zone. The Arabian Platform is represented by a thick marine succession. The zone of imbrication is a narrow belt sandwiched between the Arabian Platform and the nappes. The nappes are the highest tectonic unit. They consist of two continental slivers separated by ophiolitic associations representing oceanic environments. They were involved in the orogenic development and formed two metamorphic belts. The oceanic environment survived by the end of Middle Eocene. A northward subduction bega
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6

Wakelin-King, Gresley. "Using geomorphology to assess contour furrowing in western New South Wales, Australia." Rangeland Journal 33, no. 2 (2011): 153. http://dx.doi.org/10.1071/rj10080.

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This study examines landscape rehabilitation treatments installed 20–40 years ago in the Western Catchment of NSW. Treatment outcomes were assessed using geomorphic criteria, because geomorphic processes are fundamental to ecological permanence. Contour furrowing creates artificial runoff-runon sets which intercept runoff (resistance to flow by windrows microrelief and surface roughness) and promote infiltration (artificial permeability by ripping). As originally conceived, after windrows subside, flow resistance would be afforded by surface roughness under belts of vegetation. This study show
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7

Sial, Alcides Nobrega, Claudio Gaucher, Aroldo Misi, et al. "Correlations of some Neoproterozoic carbonate-dominated successions in South America based on high-resolution chemostratigraphy." Brazilian Journal of Geology 46, no. 3 (2016): 439–88. http://dx.doi.org/10.1590/2317-4889201620160079.

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ABSTRACT: This report reviews and incorporates new elemental and isotope chemostratigraphic data for correlation of Neoproterozoic carbonate-dominated successions in South America (Argentina, Bolivia, Brazil, Paraguay and Uruguay). These thick mixed carbonate/siliciclastic successions were largely deposited in epicontinental basins or accumulated on passive margins on the edges of cratons (e.g. São Francisco, Amazonia, Rio Apa Block, Pampia and Río de la Plata paleocontinents) during extensional events related to the rifting of the Rodinia Supercontinent. From the stratigraphic point of view,
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8

Downes, P. M., P. K. Seccombe, and G. R. Carr. "Sulfur- and lead-isotope signatures of orogenic gold mineralisation associated with the Hill End Trough, Lachlan Orogen, New South Wales, Australia." Mineralogy and Petrology 94, no. 3-4 (2008): 151–73. http://dx.doi.org/10.1007/s00710-008-0012-7.

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9

Seddon, Julian, Stuart Doyle, Mark Bourne, Richard Maccallum, and Sue Briggs. "Biodiversity benefits of alley farming with old man saltbush in central western New South Wales." Animal Production Science 49, no. 10 (2009): 860. http://dx.doi.org/10.1071/ea08280.

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Agricultural production systems that also provide opportunities to conserve biodiversity will be a crucial component of integrated and sustainable land use in mixed farming landscapes and should be considered and evaluated. Alley farming is an innovative farming system that aims to increase farm profitability while also enhancing environmental outcomes. Alley farming incorporates belts of woody perennial plants such as trees or shrubs, interspersed with alleys of conventionally rotated cropping and livestock grazing land. In the present study, we assessed the impacts on terrestrial biodiversit
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10

Kroonenberg, S. B., E. W. F. de Roever, L. M. Fraga, et al. "Paleoproterozoic evolution of the Guiana Shield in Suriname: A revised model." Netherlands Journal of Geosciences - Geologie en Mijnbouw 95, no. 4 (2016): 491–522. http://dx.doi.org/10.1017/njg.2016.10.

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AbstractThe Proterozoic basement of Suriname consists of a greenstone–tonalite–trondhjemite–granodiorite belt in the northeast of the country, two high-grade belts in the northwest and southwest, respectively, and a large granitoid–felsic volcanic terrain in the central part of the country, punctuated by numerous gabbroic intrusions. The basement is overlain by the subhorizontal Proterozoic Roraima sandstone formation and transected by two Proterozoic and one Jurassic dolerite dyke swarms. Late Proterozoic mylonitisation affected large parts of the basement. Almost 50 new U–Pb and Pb–Pb zircon
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11

Tucker, R. D., J. Y. Roig, C. Delor, et al. "Neoproterozoic extension in the Greater Dharwar Craton: a reevaluation of the “Betsimisaraka suture” in MadagascarThis article is one of a series of papers published in this Special Issue on the theme of Geochronology in honour of Tom Krogh." Canadian Journal of Earth Sciences 48, no. 2 (2011): 389–417. http://dx.doi.org/10.1139/e10-034.

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The Precambrian shield of Madagascar is reevaluated with recently compiled geological data and new U–Pb sensitive high-resolution ion microprobe (SHRIMP) geochronology. Two Archean domains are recognized: the eastern Antongil–Masora domain and the central Antananarivo domain, the latter with distinctive belts of metamafic gneiss and schist (Tsaratanana Complex). In the eastern domain, the period of early crust formation is extended to the Paleo–Mesoarchean (3.32–3.15 Ga) and a supracrustal sequence (Fenerivo Group), deposited at 3.18 Ga and metamorphosed at 2.55 Ga, is identified. In the centr
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12

Burke, William B., Andrew K. Laskowski, Devon A. Orme, et al. "Record of Crustal Thickening and Synconvergent Extension from the Dajiamang Tso Rift, Southern Tibet." Geosciences 11, no. 5 (2021): 209. http://dx.doi.org/10.3390/geosciences11050209.

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North-trending rifts throughout south-central Tibet provide an opportunity to study the dynamics of synconvergent extension in contractional orogenic belts. In this study, we present new data from the Dajiamang Tso rift, including quantitative crustal thickness estimates calculated from trace/rare earth element zircon data, U-Pb geochronology, and zircon-He thermochronology. These data constrain the timing and rates of exhumation in the Dajiamang Tso rift and provide a basis for evaluating dynamic models of synconvergent extension. Our results also provide a semi-continuous record of Mid-Creta
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13

Wilkins, Colin, and Mike Quayle. "Structural Control of High-Grade Gold Shoots at the Reward Mine, Hill End, New South Wales, Australia." Economic Geology 116, no. 4 (2021): 909–35. http://dx.doi.org/10.5382/econgeo.4807.

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Abstract The Reward mine at Hill End hosts structurally controlled orogenic gold mineralization in moderately S plunging, high-grade gold shoots located at the intersection between a late, steeply W dipping reverse fault zone and E-dipping, bedding-parallel, laminated quartz veins (the Paxton’s vein system). The mineralized bedding-parallel veins are contained within the middle Silurian to Middle Devonian age, turbidite-dominated Hill End trough forming part of the Lachlan orogen in New South Wales. The Hill End trough was deformed in the Middle Devonian (Tabberabberan orogeny), forming tight,
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14

Alder, J. D., S. Hawley, T. Maung, et al. "PROSPECTIVITY OF THE OFFSHORE SYDNEY BASIN: A NEW PERSPECTIVE." APPEA Journal 38, no. 1 (1998): 68. http://dx.doi.org/10.1071/aj97004.

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Approximately 40 per cent of the 52,000 km2 Sydney Basin lies in shallow waters (less than 200 m) off the central New South Wales coast. Containing more than 5,000 m of Permo-Triassic marine and non-marine sediments, and having been the subject of several previous exploration campaigns, no wells have been drilled in the offshore despite widespread numerous occurrences of oil and gas onshore.The Sydney Basin, together with the Bowen and Gunnedah basins, form a major longitudinal Permo-Triassic basinal complex stretching 2,500 km down the eastern margin of Australia. Whereas the onset of this ba
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15

JAPAS, MARIA SILVIA, GUILLERMO HÉCTOR RÉ, SEBASTIÁN ORIOLO, and JUAN FRANCISCO VILAS. "Basement-involved deformation overprinting thin-skinned deformation in the Pampean flat-slab segment of the southern Central Andes, Argentina." Geological Magazine 153, no. 5-6 (2016): 1042–65. http://dx.doi.org/10.1017/s001675681600056x.

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AbstractIn the southern Central Andes, the Andean foreland was deformed due to Neogene shallowing of the Nazca slab beneath the South America plate. In this 27–33ºS Pampean flat-slab segment, the N-trending Argentine Precordillera transpressional fold-and-thrust belt and the Sierras Pampeanas broken foreland developed as a consequence of inward migration of the orogenic front. At 28ºS, a NNE-trending westward-dipping, thick Neogene synorogenic sequence is exposed in the Sierra de los Colorados, which shares deformation features of the Precordillera and the Sierras Pampeanas. Integration of new
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16

Sutherland, Frederick, Khin Zaw, Sebastien Meffre, et al. "Diversity in Ruby Geochemistry and Its Inclusions: Intra- and Inter- Continental Comparisons from Myanmar and Eastern Australia." Minerals 9, no. 1 (2019): 28. http://dx.doi.org/10.3390/min9010028.

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Ruby in diverse geological settings leaves petrogenetic clues, in its zoning, inclusions, trace elements and oxygen isotope values. Rock-hosted and isolated crystals are compared from Myanmar, SE Asia, and New South Wales, East Australia. Myanmar ruby typifies metasomatized and metamorphic settings, while East Australian ruby xenocrysts are derived from basalts that tapped underlying fold belts. The respective suites include homogeneous ruby; bi-colored inner (violet blue) and outer (red) zoned ruby; ruby-sapphirine-spinel composites; pink to red grains and multi-zoned crystals of red-pink-whi
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17

Dickins, J. "A History of Research on Hunter Fault System or "Lineament"." Earth Sciences History 6, no. 2 (1987): 205–13. http://dx.doi.org/10.17704/eshi.6.2.a686377183m24773.

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The Hunter Fault System or "Lineament" separates the Permian and Triassic of Sydney Basin in New South Wales from the relatively complicated region to the north and east with exposed Carboniferous and older rocks and an increasing amount of identified Permian. David in his inimitable fashion grasped the essentials in 1907. He noted that the fold movements began towards the end of the Upper Permian with an important phase between the Upper Coal Measures and the Narrabeen Series. He also noted the main north-south component. The interest kindled by David was reflected in the work of Browne, Care
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18

Holford, ICR, and AD Doyle. "The recovery of fertilizer phosphorus by wheat, its agronomic efficiency, and their relationship to soil phosphorus." Australian Journal of Agricultural Research 44, no. 8 (1993): 1745. http://dx.doi.org/10.1071/ar9931745.

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Phosphorus (P) uptake by wheat from both soil and fertilizer, the recovery of fertilizer P and its agronomic efficiency, and the fertilizer P required for maximum profit were measured in 55 wheat fertilizer experiments during 1986-89 in the northern and central wheat belts of New South Wales. Moisture conditions during crop growth had a dominant effect on all these parameters, whose values were generally highest in the wettest year (1988) and much lower in the driest year (1989). Lactate-extractable soil P was well correlated with each of these parameters, there being a different relationship
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19

Holford, ICR, and AD Doyle. "Influence of intensity/quantity characteristics of soil phosphorus tests on their relationships to phosphorus responsiveness of wheat under field conditions." Soil Research 30, no. 3 (1992): 343. http://dx.doi.org/10.1071/sr9920343.

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Six soil phosphorus tests (lactate, Brayl, Bray2, neutral fluoride, Olsen and Colwell) were regressed against potassium chloride-soluble phosphorus (intensity) and isotopically exchangeable phosphorus (quantity) measured in 59 soils of the northern and central wheat belts of New South Wales. Wheat nutrition experiments on these soils during 1986-89 measured yield responses to phosphate and nitrogen fertilizers. Soil tests varied widely in their correlations with yield responsiveness to phosphate, with the lactate and Bray2 tests accounting for more than twice the variance accounted for by othe
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20

Majorowicz, Jacek Andrew, Marek Grad, and Marcin Polkowski. "Terrestrial heat flow versus crustal thickness and topography – European continental study." International Journal of Terrestrial Heat Flow and Applications 2, no. 1 (2019): 17–21. http://dx.doi.org/10.31214/ijthfa.v2i1.30.

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The relation between heat flow, topography and Moho depth for recent maps of Europe is presented. Newest heat flow map of Europe is based on updated database of uncorrected heat flow values to which paleoclimatic correction is applied across the continental Europe (Majorowicz and Wybraniec 2010). Correction is depth dependent due to a diffusive thermal transfer of the surface temperature forcing, of which glacial–interglacial history has the largest impact. This explains some very low uncorrected heat flow values of 20–30 mW/m2in shallow boreholes in the shields, shallow basin areas of the cratons,
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21

Oliver, Y. M., E. C. Lefroy, R. Stirzaker, and C. L. Davies. "Deep-drainage control and yield: the trade-off between trees and crops in agroforestry systems in the medium to low rainfall areas of Australia." Australian Journal of Agricultural Research 56, no. 10 (2005): 1011. http://dx.doi.org/10.1071/ar04213.

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In the dryland cropping areas of southern Australia, at risk from dryland salinity, tree belts can improve water management by taking up water unused by crops, with the risk that crop yield will be reduced through competition. As there are few direct markets for tree products grown in the medium to low rainfall areas, the design of agroforestry systems becomes important in reducing the trade-off in crop yield. This study examined some factors that influence the trade-off between crop yield and deep-drainage control in order to develop design guidelines for medium to low rainfall agroforestry.
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22

Bean, Judith M., Gavin J. Melville, and Ronald B. Hacker. "Assessment of the potential of a range of microhabitats for use as seed production areas in moderately degraded rangelands in semiarid Australia." Rangeland Journal 39, no. 1 (2017): 49. http://dx.doi.org/10.1071/rj16095.

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Previous studies in mulga country with hard-setting red earth soils in north-west New South Wales, Australia, have demonstrated that small fenced seed production areas on local high points can contribute to regeneration of native perennial vegetation, and increases in the soil seedbank, on surrounding slopes. In this study the potential of seven microhabitats in this environment, each replicated twice, for use as seed production areas was assessed indirectly by a study of their functional characteristics and vegetation dynamics. Indices of landscape function (stability, infiltration and nutrie
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23

White, R. E., B. P. Christy, A. M. Ridley, et al. "SGS Water Theme: influence of soil, pasture type and management on water use in grazing systems across the high rainfall zone of southern Australia." Australian Journal of Experimental Agriculture 43, no. 8 (2003): 907. http://dx.doi.org/10.1071/ea02239.

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Eleven experimental sites in the Sustainable Grazing Systems (SGS) national experiment were established in the high rainfall zone (HRZ, >600 mm/year) of Western Australia, Victoria and New South Wales to measure components of the water balance, and pathways of water movement, for a range of pastures from 1997 to 2001. The effect of widely spaced river red gums (Eucalyptus camaldulensis) in pasture, and of belts of plantation blue gums (E. globulus), was studied at 2 of the sites. The soil types tested ranged from Kurosols, Chromosols and Sodosols, with different subsoil permeabilities, to H
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24

Morton, A. C., J. I. Chisholm, and D. Frei. "Provenance of Carboniferous sandstones in the central and southern parts of the Pennine Basin, UK: evidence from detrital zircon ages." Proceedings of the Yorkshire Geological Society, October 16, 2020, pygs2020–010. http://dx.doi.org/10.1144/pygs2020-010.

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New U-Pb isotopic analyses of detrital zircon grains from Namurian and Westphalian sandstones in the central and south parts of the Pennine Basin are combined with published analyses from the same region, to assess existing views on the nature and location of the source areas that supplied the clastic sediment. The study confirms that most sandstones were derived from distant areas to the north, west and south, and that a local source, in the Wales-Brabant High, also supplied sediment at times. The northern sources are thought to lie mainly in Laurentia (East Greenland), with some input from B
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25

Яроцкий, Г. П., and Х. О. Чотчаев. "The location and Potential Assessment of the Ore Regions in the South-Western Part of the Koryak Highland." Геология и геофизика Юга России, no. 1 (April 9, 2020). http://dx.doi.org/10.23671/vnc.2020.1.59068.

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Актуальность рассматриваемой темы в том, что орогенные пояса материковой части Камчатского края насыщены полезными ископаемыми, приуроченных к поясам, образованным последовательным приростом окраин континента от древних с северо-запада к юго-востоку. Такими поясами с месторождениями Ag, Au, Sn, Hg, S являются Северо-Западно-Корякский олигоценовый и Южно-Корякский миоценовый, образованные на северной и южной границе Центрально-Корякской окраины позднемелового континента. Они сформированы в олигоцене и миоцене изолированными вулканогенами локальных андезитовых полей, прорванных гранитоидами тект
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26

Chen, Yanfei, Zeming Zhang, Richard M. Palin, et al. "Late Triassic Orogenic Assembly of the Tibetan Plateau: Constraints from Magmatism and Metamorphism in the East Lhasa Terrane." Journal of Petrology 62, no. 6 (2021). http://dx.doi.org/10.1093/petrology/egab032.

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Abstract The early Mesozoic evolution of the Lhasa terrane, which represents a major component of the Himalayan–Tibetan orogen, remains highly controversial. In particular, geological units and events documented either side of the eastern Himalayan syntaxis (EHS) are poorly correlated. Here, we report new petrological, geochemical and geochronological data for cogenetic peraluminous S-type granites and metamorphic rocks (gneiss and schist) from the Motuo–Bomi–Chayu region of the eastern Lhasa terrane, located on the eastern flank of the EHS. Zircon U–Pb dating indicates that these units record
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27

"Late Cainozoic history of vegetation, fire, lake levels and climate, at Lake George, New South Wales, Australia." Philosophical Transactions of the Royal Society of London. B, Biological Sciences 311, no. 1151 (1985): 379–447. http://dx.doi.org/10.1098/rstb.1985.0156.

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The results of pollen, spore, algal and charcoal particle analyses from an 18 m core sample, dating from ca . 730000-0 a before present (B.P.), from Lake George are described along with an account of a five year study of modern pollen-rain from the same site. Also, pollen analyses of two isolated samples, dating about 4-7 Ma B.P., in a separate core from the same location are reported for comparison. The sedimentary sequence is dated by means of magnetostratigraphy and radiocarbon. The microfossil record from Lake George provides the longest relatively continuous Quaternary continental sequenc
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28

Wang, Huining, Fulai Liu, Zaibo Sun, et al. "A New HP–UHP Eclogite Belt Identified in the Southeastern Tibetan Plateau: Tracing the Extension of the Main Palaeo-Tethys Suture Zone." Journal of Petrology 61, no. 8 (2020). http://dx.doi.org/10.1093/petrology/egaa073.

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Abstract The Changning–Menglian orogenic belt (CMOB) in the southeastern Tibetan Plateau is an important link between the Longmu Co–Shuanghu suture (LCSS) in the northern Tibetan Plateau and the Chiang Mai–Inthanon and Bentong–Raub sutures in Thailand and Peninsular Malaysia. These belts and sutures are generally regarded as containing the remnants of the oceanic crust of the Palaeo-Tethys that formed by seafloor spreading as a result of the separation of Gondwana- and Eurasia-derived blocks during the Middle Cambrian. In this paper we report the first discovery of abundant unaltered and retro
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