Thematische Bibliographien / Diapirs South Australia Flinders Ranges

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  1. Zeitschriftenartikel
  2. Dissertationen
  3. Bücher
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  5. Konferenzberichte

Auswahl der wissenschaftlichen Literatur zum Thema „Diapirs South Australia Flinders Ranges“

Autor: Grafiati
Veröffentlicht am 4. Juni 2021
Zuletzt aktualisiert am 1. Februar 2022

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Zeitschriftenartikel zum Thema "Diapirs South Australia Flinders Ranges"

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Reilly, M. R. W., und S. C. Lang. „A PONDED BASIN FLOOR FAN OUTCROP ANALOGUE: BUNKERS SANDSTONE, NORTHERN FLINDERS RANGES, AUSTRALIA“. APPEA Journal 43, Nr. 1 (2003): 537. http://dx.doi.org/10.1071/aj02028.

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The Donkey Bore Syncline in the Northern Flinders Ranges of South Australia contains a generally finegrained deepwater succession of Early Cambrian age (Bunkers Sandstone) that outcrops on three sides of a syncline and flanks an active salt diapir to the east (Wirrealpa Diapir). Within the succession lies a basal sand-prone interval interpreted as a basin floor fan (BFF) ponded within a mini-basin on a topographically complex slope.The BFF comprises over 30 m of section with deposits that are dominantly massive clean sandstone beds (0.1– 3 m thick) that are stacked or interbedded with siltstones and pinch out along strike.Eight stratigraphic sections and accompanying spectral gamma ray logs (using a hand held scintillometer) were measured through the BFF. Using spectral gamma ray log analysis combined with stratigraphic logs, four alternative correlation panels were constructed.Quantitative analysis of sand-prone intervals interpreted in each of the panels provided data on the vertical and horizontal connectivity within the BFF as different correlation methods were explored and the geological model improved. Quantitative analysis of vertical and horizontal connectivity values indicates a high degree of heterogeneity within the BFF, with poor–moderate vertical connectivity, with individual beds rarely correlating >500 m along strike. This heterogeneity is poorly resolved using conventional wireline log suites, but is greatly improved if spectral gamma ray logs are used (especially Thorium).The data set provides a high-resolution analogue for understanding the internal architecture of deepwater hydrocarbon reservoirs.
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2

Backé, Guillaume, Graham Baines, David Giles, Wolfgang Preiss und 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, Nr. 3 (März 2010): 650–65. http://dx.doi.org/10.1016/j.marpetgeo.2009.09.001.

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Fernandes, Blaise I. L., Kathryn J. Amos, Tobias H. D. Payenberg und Simon Lang. „An outcrop analogue for deepwater salt withdrawal mini-basins: lateral and vertical variations in basin-fill“. APPEA Journal 58, Nr. 2 (2018): 809. http://dx.doi.org/10.1071/aj17200.

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Mini-basins are well known targets for petroleum exploration as they can contain significant hydrocarbon reserves, such as in the Gulf of Mexico. Though mini-basins have been studied before, their reservoir rock distributions remain poorly predictable. This is especially the case where mini-basins are near salt-diapirs. The Donkey Bore Syncline in the Flinders Ranges, South Australia, presents an excellently exposed deepwater mini-basin reservoir analogue. Detailed outcrop study, including vertical and lateral logged sections presented here, shed considerable light on the depositional system, especially with regards to depositional style and stages of basin-fill. Based on the observed facies and deposit geometries, the authors have been able to detect the change from a carbonate to a siliciclastic deposition system and interpret mini-basin-fill initiation and progradation processes. Sandy gravity-flow deposit lobe areas are identified, enclosed within shales. Along with paleocurrent data, these enable the description and interpretation of basin-fill stages and the lateral character of reservoir-analogue depositional tracts. This will be useful for better interpretation of mini-basin turbidite sequences and will help reduce uncertainties in subsurface exploration. This may also improve prediction of basin-fill where well spacing is inadequate.
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Vidal‐Royo, Oskar, Mark G. Rowan, Oriol Ferrer, Mark P. Fischer, J. Carl Fiduk, David P. Canova, Thomas E. Hearon und Katherine A. Giles. „The transition from salt diapir to weld and thrust: Examples from the Northern Flinders Ranges in South Australia“. Basin Research 33, Nr. 5 (23.06.2021): 2675–705. http://dx.doi.org/10.1111/bre.12579.

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Snow, Michael R., Allan Pring und Nicole Allen. „Minerals of the Wooltana Cave, Flinders Ranges, South Australia“. Transactions of the Royal Society of South Australia 138, Nr. 2 (Januar 2014): 214–30. http://dx.doi.org/10.1080/03721426.2014.11649009.

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Groves, I. M., C. E. Carman und W. J. Dunlap. „Geology of the Beltana Willemite Deposit, Flinders Ranges, South Australia“. Economic Geology 98, Nr. 4 (01.06.2003): 797–818. http://dx.doi.org/10.2113/gsecongeo.98.4.797.

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Lemon, N. M. „A Neoproterozoic fringing stromatolite reef complex, Flinders Ranges, South Australia“. Precambrian Research 100, Nr. 1-3 (März 2000): 109–20. http://dx.doi.org/10.1016/s0301-9268(99)00071-6.

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Walshe, Keryn. „Aboriginal occupation at Hawker Lagoon, southern Flinders Ranges, South Australia“. Australian Archaeology 60, Nr. 1 (Januar 2005): 24–33. http://dx.doi.org/10.1080/03122417.2005.11681801.

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Woon, E., und M. W. Wallace. „Petrogenesis of Neoproterozoic Allochthonous Reef Carbonates, Flinders Ranges, South Australia“. ASEG Extended Abstracts 2006, Nr. 1 (Dezember 2006): 1–4. http://dx.doi.org/10.1071/aseg2006ab198.

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Jago, J. B., J. G. Gehling, M. J. Betts, G. A. Brock, C. R. Dalgarno, D. C. García-Bellido, P. G. Haslett et al. „The Cambrian System in the Arrowie Basin, Flinders Ranges, South Australia“. Australian Journal of Earth Sciences 67, Nr. 7 (11.12.2018): 923–48. http://dx.doi.org/10.1080/08120099.2018.1525431.

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Dissertationen zum Thema "Diapirs South Australia Flinders Ranges"

1

Mendis, Premalal J. „The origin of the geological structures, diapirs, grabens, and barite veins in the Flinders Ranges, South Australia“. Title page, abstract and contents only, 2002. http://web4.library.adelaide.edu.au/theses/09PH/09phm5389.pdf.

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Bibliography: leaves [156-167] Map 1. Parachilna, sheet SH 54-13 / compiled by P. Reid and W.V. Preiss. 2nd ed. [Adelaide] : Primary Industries & Resources SA, 1999. 1 map : col ; 69 x 100 cm. (South Australia. Geological Survey. Geological atlas 1:250 000 series ; sheet SH 54-13) -- map 2. Geology of the Flinders Ranges National Park. Parkside, S. Aust. : Mines and Energy South Australia, 1994. 1 map : col. ; 84 x 60 cm. Scale: 1:75 000.
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Cooper, Andrew McGregor. „Late Proterozoic hydrocarbon potential and its association with diapirism in Blinman #2, Central Flinders Ranges, South Australia /“. Title page, abstract and contents only, 1991. http://web4.library.adelaide.edu.au/theses/09SB/09sbc776.pdf.

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Thesis (B. Sc.(Hons))--National Centre for Petroleum Geology and Geophysics, University of Adelaide, 1991.
"National grid reference 1:250 000 - Parachilna SH54-13." Includes bibliographical references (leaves 45-47).
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Hearon, IV Thomas E. „Analysis of salt-sediment interaction associated with steep diapirs and allochthonous salt| Flinders and willouran ranges, south australia, and the deepwater northern gulf of Mexico“. Thesis, Colorado School of Mines, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=3602617.

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The eastern Willouran Ranges and northern Flinders Ranges, South Australia contain Neoproterozoic and Cambrian outcrop exposures of diapiric breccia contained in salt diapirs, salt sheets and associated growth strata that provide a natural laboratory for testing and refining models of salt-sediment interaction, specifically allochthonous salt initiation and emplacement and halokinetic deformation. Allochthonous salt, which is defined as a sheet-like diapir of mobile evaporite emplaced at younger stratigraphic levels above the autochthonous source, is emplaced due to the interplay between the rate of salt supply to the front of the sheet and the sediment-accumulation rate, and may be flanked by low- to high-angle stratal truncations to halokinetic folds. Halokinetic sequences (HS) are localized (<1000 m) unconformity-bound successions of growth strata adjacent to salt diapirs that form as drape folds due to the interplay between salt rise rate (R) and sediment accumulation rate (A). HS stack to form tabular and tapered composite halokinetic sequences (CHS), which have narrow and broad zones of thinning, respectively. The concepts of CHS formation are derived from outcrops in shallow water to subaerial depositional environments in La Popa Basin, Mexico and the Flinders Ranges, South Australia. Current models for allochthonous salt emplacement, including surficial glacial flow, advance above subsalt shear zones and emplacement along tip thrusts, do not address how salt transitions from steep feeders to low-angle sheets and the model for the formation of halokinetic sequences has yet to be fully applied or tested in a deepwater setting. Thus, this study integrates field data from South Australia with subsurface data from the northern Gulf of Mexico to test the following: (1) current models of allochthonous salt advance and subsalt deformation using structural analysis of stratal truncations adjacent to outcropping salt bodies, with a focus on the transition from steep diapirs to shallow salt sheets in South Australia; and (2) the outcrop-based halokinetic sequence model using seismic and well data from the Auger diapir, located in the deepwater northern Gulf of Mexico. Structural analysis of strata flanking steep diapirs and allochthonous salt in South Australia reveals the transition from steep diapirs to shallowly-dipping salt sheets to be abrupt and involves piston-like breakthrough of roof strata, freeing up salt to flow laterally. Two models explain this transition: 1) salt-top breakout, where salt rise occurs inboard of the salt flank, thereby preserving part of the roof beneath the sheet; and 2) salt-edge breakout, where rise occurs at the edge of the diapir with no roof preservation. Shear zones, fractured or mixed `rubble zones' and thrust imbricates are absent in strata beneath allochthonous salt and adjacent to steep diapirs. Rather, halokinetic drape folds, truncated roof strata and low- and high-angle bedding intersections are among the variety of stratal truncations adjacent to salt bodies in South Australia. Interpretation and analysis of subsurface data around the Auger diapir reveals similar CHS geometries, stacking patterns and ratios of salt rise and sediment accumulation rates, all of which generally corroborate the halokinetic sequence model. The results of this study have important implications for salt-sediment interaction, but are also critical to understanding and predicting combined structural-stratigraphic trap geometry, reservoir prediction and hydrocarbon containment in diapir-flank settings.

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Higgins, Jonathan. „The Pamatta Pass Canyon Complex : Neoproterozoic Wonoka Formation, Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09SB/09sbh636.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1998.
National Grid Reference:-Orroroo Sheet SI 54-1 (1:250,000 Geological Series). One col. folded map in pocket on back cover. Includes bibliographical references (8 leaves ).
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Fuller, Margaret. „Early Cambrian corals from the Moorowie Formation, Eastern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09SM/09smf967.pdf.

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Chow, Angie N. C. „Geomorphic evolution of the Mt. Arden Creek Valley, southern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbc552.pdf.

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Thesis (B. Sc. (Hons.))--University of Adelaide, Dept. of Geology, 1993.
On title page: National grid reference Orroroo SI 54-1 6533-4 (1:250 000). Includes bibliographical references (leaves 8-11).
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Meredith, Kirsten. „Geological history of the Waukarie Creek Canyon complex, southern Flinders Ranges, South Australia /“. Title page and contents only, 1997. http://web4.library.adelaide.edu.au/theses/09SB/09sbm559.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1998.
National Grid reference Port Augusta SI 53-4 Orroroo SI 54-1. Includes bibliographical references (leaves 41-43).
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Nitschke, Nicholas Leigh. „Identification of aeolian dust mantles in the semi-arid Flinders Ranges, South Australia /“. Title page, table of contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09ENVSH/09envshn732.pdf.

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Chor, Carly Choi-Choo. „Palaeohydrology of a late Pleistocene wetland in the central Flinders Ranges, South Australia /“. Title page, contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09SB/09sbc5511.pdf.

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Greene, Susan J. „A geomorphological and sedimentological study of a climbing dune, Northern Flinders Ranges, South Australia /“. Title page, contents and abstract only, 1994. http://web4.library.adelaide.edu.au/theses/09AR/09arg8118.pdf.

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Bücher zum Thema "Diapirs South Australia Flinders Ranges"

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Selby, J. Corridors through time: The geology of the Flinders Ranges, South Australia. Netley, S. Australia: State Publishing, 1990.

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Dobre, Cil. THE FLINDERS RANGES - SOUTH AUSTRALIA. Oz Scapes, 2000.

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(Photographer), Pete Dobre', Hrsg. Arkaroola: Northern Flinders Ranges, South Australia. Oz Scapes, 2000.

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O'Neil, Viking. South Australia: The Flinders Ranges in Color. Viking, 1988.

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Dolby, Tim, und Rohan Clarke. Finding Australian Birds. CSIRO Publishing, 2014. http://dx.doi.org/10.1071/9781486300846.

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Finding Australian Birds is a guide to the special birds found across Australia's vastly varied landscapes. From the eastern rainforests to central deserts, Australia is home to some 900 species of birds. This book covers over 400 Australian bird watching sites conveniently grouped into the best birding areas, from one end of the country to the other. This includes areas such as Kakadu in the Top End and rocky gorges in the central deserts of the Northern Territory, the Great Barrier Reef in Queensland, rainforests distributed along the eastern Australian seaboard, some of the world's tallest forests in Tasmania, the Flinders Ranges and deserts along the iconic Strzelecki and Birdsville Tracks in South Australia, and the mallee temperate woodlands and spectacular coastlines in both Victoria and south west Western Australia. Each chapter begins with a brief description of the location, followed by a section on where to find the birds, which describes specific birdwatching sites within the location's boundaries, and information on accommodation and facilities. The book also provides a comprehensive 'Bird Finding Guide', listing all of Australia's birds with details on their abundance and where exactly to see them. Of value to both Australian birdwatchers and international visitors, this book will assist novices, birders of intermediate skill and keen 'twitchers' to find any Australian species.
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Buchteile zum Thema "Diapirs South Australia Flinders Ranges"

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Williams, Martin. „Flinders Ranges, South Australia: Solving the Puzzle (1993–2007)“. In Nile Waters, Saharan Sands, 149–56. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-25445-6_18.

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Dyson, Ian A., und Mark G. Rowan. „Geology of a Welded Diapir and Flanking Mini-Basins in the Flinders Ranges of South Australia“. In Salt Sediment Interactions and Hydrocarbon Prospectivity: Concepts, Applications, and Case Studies for the 21st Century: 24th Annual, 69–89. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 2004. http://dx.doi.org/10.5724/gcs.04.24.0069.

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Gannaway, C. E., K. A. Giles, R. A. Kernen, M. G. Rowan und T. E. Hearon. „Comparison of the Depositional and Halokinetic History of Suprasalt and Subsalt Minibasins at Patawarta Diapir, Flinders Ranges, South Australia“. In Sedimentary Basins: Origin, Depositional Histories, and Petroleum Systems. SEPM Society for Sedimentary Geology, 2014. http://dx.doi.org/10.5724/gcs.14.33.0428.

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Crossing, A. R., und V. A. Gostin. „Isotopic signatures of carbonates associated with Sturtian (Neoproterozoic) glacial facies, central Flinders Ranges, South Australia“. In Earth's Glacial Record, 165–75. Cambridge University Press, 1994. http://dx.doi.org/10.1017/cbo9780511628900.013.

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Dyson, Ian A. „Interpreted Shallow and Deep-Water Depositional Systems of the Beltana Mini-Basin in the Northern Flinders Ranges, South Australia“. In Salt Sediment Interactions and Hydrocarbon Prospectivity: Concepts, Applications, and Case Studies for the 21st Century: 24th Annual, 997–1030. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 2004. http://dx.doi.org/10.5724/gcs.04.24.0997.

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Konferenzberichte zum Thema "Diapirs South Australia Flinders Ranges"

1

Kernen, Rachelle, Elizabeth Anthony, Jason Ricketts, Julian Biddle und Jose A. Garcia. „THERMAL ALTERATION HISTORY OF NEOPROTEROZOIC BASALT XENOLITHS IN THE PATAWARTA AND WITCHELINA DIAPIRS, FLINDERS AND WILLOURAN RANGES, SOUTH AUSTRALIA“. In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289119.

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Giles, Sarah, Rachelle Kernen, Asmara Lehrmann und Katherine Giles. „EVOLUTION OF A SUPRASALT MINIBASIN: NEOPROTEROZOIC (EDIACARAN) PATAWARTA SALT SHEET, FLINDERS RANGES, SOUTH AUSTRALIA“. In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289435.

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Lehrmann, Asmara, Rachelle Kernen, Sarah Giles und Katherine Giles. „TIMING OF ALLOCHTHONOUS SALT EMPLACEMENT OF THE NEOPROTEROZOIC (EDIACARAN) PATAWARTA SALT SHEET, FLINDERS RANGES, SOUTH AUSTRALIA: EVIDENCE FROM THE SUBSALT MINIBASIN“. In 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289392.

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Mcmahon, William, Alex G. Liu, Benjamin Tindal und M. G. Kleinhans. „EDIACARAN LIFE CLOSE TO LAND: COASTAL AND SHOREFACE HABITATS OF THE EDIACARAN MACROBIOTA, THE CENTRAL FLINDERS RANGES, SOUTH AUSTRALIA“. In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355663.

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