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Artigos de revistas sobre o tema "Geology, Structural South Australia Flinders Ranges"

Autor: Grafiati

Publicado: 4 de junho de 2021

Última modificação: 1 de fevereiro de 2022

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1

Groves, I. M., C. E. Carman, and W. J. Dunlap. "Geology of the Beltana Willemite Deposit, Flinders Ranges, South Australia." Economic Geology 98, no. 4 (June 1, 2003): 797–818. http://dx.doi.org/10.2113/gsecongeo.98.4.797.

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2

Betts, Marissa J., Timothy P. Topper, James L. Valentine, Christian B. Skovsted, John R. Paterson, and Glenn A. Brock. "A new early Cambrian bradoriid (Arthropoda) assemblage from the northern Flinders Ranges, South Australia." Gondwana Research 25, no. 1 (January 2014): 420–37. http://dx.doi.org/10.1016/j.gr.2013.05.007.

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3

Eickhoff, K. H., C. C. Von Der Borch, and A. E. Grady. "Proterozoic canyons of the Flinders Ranges (South Australia): submarine canyons or drowned river valleys?" Sedimentary Geology 58, no. 2-4 (August 1988): 217–35. http://dx.doi.org/10.1016/0037-0738(88)90070-x.

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4

Thomas, Matilda, Jonathan D. A. Clarke, Victor A. Gostin, George E. Williams, and Malcolm R. Walter. "The Flinders Ranges and surrounds, South Australia: a window on astrobiology and planetary geology." Episodes 35, no. 1 (March 1, 2012): 226–35. http://dx.doi.org/10.18814/epiiugs/2012/v35i1/022.

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5

Sandiford, Mike, Eike Paul, and Thomas Flottmann. "Sedimentary thickness variations and deformation intensity during basin inversion in the Flinders Ranges, South Australia." Journal of Structural Geology 20, no. 12 (December 1998): 1721–31. http://dx.doi.org/10.1016/s0191-8141(98)00088-1.

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6

Brugger, Joël, Ngaire Long, D. C. McPhail, and Ian Plimer. "An active amagmatic hydrothermal system: The Paralana hot springs, Northern Flinders Ranges, South Australia." Chemical Geology 222, no. 1-2 (October 2005): 35–64. http://dx.doi.org/10.1016/j.chemgeo.2005.06.007.

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7

Lubiniecki, D. C., R. C. King, S. P. Holford, M. A. Bunch, S. B. Hore, and S. M. Hill. "Cenozoic structural evolution of the Mount Lofty Ranges and Flinders Ranges, South Australia, constrained by analysis of deformation bands." Australian Journal of Earth Sciences 67, no. 8 (February 9, 2020): 1097–115. http://dx.doi.org/10.1080/08120099.2019.1695227.

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8

Vidal‐Royo, Oskar, Mark G. Rowan, Oriol Ferrer, Mark P. Fischer, J. Carl Fiduk, David P. Canova, Thomas E. Hearon, and Katherine A. Giles. "The transition from salt diapir to weld and thrust: Examples from the Northern Flinders Ranges in South Australia." Basin Research 33, no. 5 (June 23, 2021): 2675–705. http://dx.doi.org/10.1111/bre.12579.

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9

Counts, John W., and Kathryn J. Amos. "Sedimentology, depositional environments and significance of an Ediacaran salt-withdrawal minibasin, Billy Springs Formation, Flinders Ranges, South Australia." Sedimentology 63, no. 5 (April 1, 2016): 1084–123. http://dx.doi.org/10.1111/sed.12250.

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10

McMahon, William J., Alexander G. Liu, Benjamin H. Tindal, and Maarten G. Kleinhans. "Ediacaran life close to land: Coastal and shoreface habitats of the Ediacaran macrobiota, the Central Flinders Ranges, South Australia." Journal of Sedimentary Research 90, no. 11 (November 30, 2020): 1463–99. http://dx.doi.org/10.2110/jsr.2020.029.

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ABSTRACT The Rawnsley Quartzite of South Australia hosts some of the world's most diverse Ediacaran macrofossil assemblages, with many of the constituent taxa interpreted as early representatives of metazoan clades. Globally, a link has been recognized between the taxonomic composition of individual Ediacaran bedding-plane assemblages and specific sedimentary facies. Thorough characterization of fossil-bearing facies is thus of fundamental importance for reconstructing the precise environments and ecosystems in which early animals thrived and radiated, and distinguishing between environmental

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11

Paul, E., T. Flöttmann, and M. Sandiford. "Structural geometry and controls on basement‐involved deformation in the northern Flinders Ranges, Adelaide Fold Belt, South Australia." Australian Journal of Earth Sciences 46, no. 3 (June 1999): 343–54. http://dx.doi.org/10.1046/j.1440-0952.1999.00711.x.

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12

Backé, Guillaume, Graham Baines, David Giles, Wolfgang Preiss, and Andrew Alesci. "Basin geometry and salt diapirs in the Flinders Ranges, South Australia: Insights gained from geologically-constrained modelling of potential field data." Marine and Petroleum Geology 27, no. 3 (March 2010): 650–65. http://dx.doi.org/10.1016/j.marpetgeo.2009.09.001.

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13

Laflamme, Marc, James G. Gehling, and Mary L. Droser. "Deconstructing an Ediacaran frond: three-dimensional preservation of Arborea from Ediacara, South Australia." Journal of Paleontology 92, no. 3 (March 14, 2018): 323–35. http://dx.doi.org/10.1017/jpa.2017.128.

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AbstractExquisitely preserved three-dimensional examples of the classic Ediacaran (late Neoproterozoic; 570–541 Ma) frond Charniodiscus arboreus Jenkins and Gehling, 1978 (herein referred to as Arborea arborea Glaessner in Glaessner and Daily, 1959) are reported from the Ediacara Member, Rawnsley Quartzite of South Australia, and allow for a detailed reinterpretation of its functional morphology and taxonomy. New specimens cast in three dimensions within sandy event beds showcase detailed branching morphology that highlights possible internal features that are strikingly different from rangeom

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14

COOPER, BARRY J., and JAMES B. JAGO. "ROBERT BEDFORD (1874–1951), THE KYANCUTTA MUSEUM, AND A UNIQUE CONTRIBUTION TO INTERNATIONAL GEOLOGY." Earth Sciences History 37, no. 2 (January 1, 2018): 416–43. http://dx.doi.org/10.17704/1944-6178-37.2.416.

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Robert Bedford (1874–1951), based in the isolated community of Kyancutta in South Australia, was a unique contributor to world geology, specifically in the field of meteorites and fossil archaeocyatha. Born Robert Arthur Buddicom in Shropshire, UK, he was an Oxford graduate who worked as a scientist in Freiberg, Naples, Birmingham and Shrewsbury as well as with the Natural History Museum, Kensington and the Plymouth Museum in the United Kingdom. He was a Fellow of the Geological Society of London, 1899–1910. In 1915, Buddicom changed his surname to Bedford and relocated to South Australia. Dur

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15

Haberlah, David, Martin A. J. Williams, Galen Halverson, Grant H. McTainsh, Steven M. Hill, Tomas Hrstka, Patricio Jaime, Alan R. Butcher, and Peter Glasby. "Loess and floods: High-resolution multi-proxy data of Last Glacial Maximum (LGM) slackwater deposition in the Flinders Ranges, semi-arid South Australia." Quaternary Science Reviews 29, no. 19-20 (September 2010): 2673–93. http://dx.doi.org/10.1016/j.quascirev.2010.04.014.

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16

Gannaway Dalton, C. Evelyn, Katherine A. Giles, Mark G. Rowan, Richard P. Langford, Thomas E. Hearon, and J. Carl Fiduk. "Sedimentologic, stratigraphic, and structural evolution of minibasins and a megaflap formed during passive salt diapirism: The Neoproterozoic Witchelina diapir, Willouran Ranges, South Australia." Journal of Sedimentary Research 90, no. 2 (February 20, 2020): 165–99. http://dx.doi.org/10.2110/jsr.2020.9.

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ABSTRACT This study documents the growth of a megaflap along the flank of a passive salt diapir as a result of the long-lived interaction between sedimentation and halokinetic deformation. Megaflaps are nearly vertical to overturned, deep minibasin stratal panels that extend multiple kilometers up steep flanks of salt diapirs or equivalent welds. Recent interest has been sparked by well penetrations of unidentified megaflaps that typically result in economic failure, but their formation is also fundamental to understanding the early history of salt basins. This study represents one of the firs

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17

Gregory, Courtney. "Geothermal Energy Potential at Paralana, Northern Flinders Ranges, South Australia." Journal of the Virtual Explorer 20 (2005). http://dx.doi.org/10.3809/jvirtex.2005.00135.

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18

U. Singh. "Ooids and Cements from the Late Precambrian of the Flinders Ranges, South Australia." SEPM Journal of Sedimentary Research Vol. 57 (1987). http://dx.doi.org/10.1306/212f8ac1-2b24-11d7-8648000102c1865d.

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19

LEMON, NICHOLAS M., and ANDREW McG. "Late Proterozoic Source Rocks Associated with Diapirs in the Central Flinders Ranges, South Australia." AAPG Bulletin 76 (1992). http://dx.doi.org/10.1306/f4c8fc50-1712-11d7-8645000102c1865d.

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20

LEMON, NICHOLAS M. "Abstract: Sea Level Influence On Diapir Movement: Enorama Diapir, Flinders Ranges, South Australia ." AAPG Bulletin 83 (1999) (1999). http://dx.doi.org/10.1306/c9ebbf9b-1735-11d7-8645000102c1865d.

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21

Gehling, James G., and Bruce Runnegar. "Phyllozoon and Aulozoon: key components of a novel Ediacaran death assemblage in Bathtub Gorge, Heysen Range, South Australia." Geological Magazine, July 29, 2021, 1–14. http://dx.doi.org/10.1017/s0016756821000509.

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Abstract The recognition of fossiliferous horizons both below and above the classical Ediacara levels of the Flinders Ranges, South Australia, significantly expands the potential of this candidate World Heritage succession. Here we document a small window into the biology and taphonomy of the late Ediacaran seafloor within the new Nilpena Sandstone Member of the Rawnsley Quartzite in Bathtub Gorge, northern Heysen Range. A 1 m2 slab extracted from the gorge, now on permanent display at the South Australian Museum, has a death assemblage dominated by the erniettomorph Phyllozoon hanseni Jenkins

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22

N. M. Lemon (2). "Physical Modeling of Sedimentation Adjacent to Diapirs and Comparison with Late Precambrian Oratunga Breccia Body in Central Flinders Ranges, South Australia." AAPG Bulletin 69 (1985). http://dx.doi.org/10.1306/ad462c59-16f7-11d7-8645000102c1865d.

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23

Holford, Simon P., Paul F. Green, Ian R. Duddy, Richard R. Hillis, Steven M. Hill, and Martyn S. Stoker. "Preservation of late Paleozoic glacial rock surfaces by burial prior to Cenozoic exhumation, Fleurieu Peninsula, Southeastern Australia." Journal of the Geological Society, June 21, 2021, jgs2020–250. http://dx.doi.org/10.1144/jgs2020-250.

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The antiquity of the Australian landscape has long been the subject of debate, with some studies inferring extraordinary longevity (>108 myr) for some subaerial landforms dating back to the early Paleozoic. A number of early Permian glacial erosion surfaces in the Fleurieu Peninsula, southeastern Australia, provide an opportunity to test the notion of long-term subaerial emergence, and thus tectonic and geomorphic stability, of parts of the Australian continent. Here we present results of apatite fission track analysis (AFTA) applied to a suite of samples collected from localities where gla

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