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Journal articles on the topic 'Adelaide Fold Belt'

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Published: 10 December 2022

Last updated: 20 February 2023

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1

Clifford, Peter, Stewart Greenhalgh, Greg Houseman, and Frank Graeber. "3-D seismic tomography of the Adelaide fold belt." Geophysical Journal International 172, no. 1 (January 2008): 167–86. http://dx.doi.org/10.1111/j.1365-246x.2007.03606.x.

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2

Griessmann, Martin, and Andreas Schmidt-Mumm. "Gold mineralisation in the Adelaide Fold Belt — Preliminary results." Journal of Geochemical Exploration 101, no. 1 (April 2009): 43. http://dx.doi.org/10.1016/j.gexplo.2008.12.030.

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3

Jenkins, Richard J. F., and Mike Sandiford. "Observations on the tectonic evolution of the southern Adelaide Fold Belt." Tectonophysics 214, no. 1-4 (November 1992): 27–36. http://dx.doi.org/10.1016/0040-1951(92)90188-c.

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4

Paul, E., M. Sandiford, and T. Flöttmann. "Structural geometry of a thick‐skinned fold‐thrust belt termination: The Olary Block in the Adelaide Fold Belt, South Australia." Australian Journal of Earth Sciences 47, no. 2 (April 2000): 281–89. http://dx.doi.org/10.1046/j.1440-0952.2000.00779.x.

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5

Turner, Simon, Mike Sandiford, Thomas Flöttmann, and John Foden. "dating of differentiated cleavage from the upper Adelaidean metasediments at Hallett Cove, southern Adelaide fold belt: Reply." Journal of Structural Geology 17, no. 12 (December 1995): 1801–3. http://dx.doi.org/10.1016/0191-8141(95)00093-s.

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6

Preiss, Wolfgang V. "dating of differentiated cleavage from the upper Adelaidean metasediments at Hallett Cove, southern Adelaide fold belt: Discussion." Journal of Structural Geology 17, no. 12 (December 1995): 1797–800. http://dx.doi.org/10.1016/0191-8141(95)00094-t.

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7

Turner, Simon, Mike Sandiford, Thomas Flöttmann, and John Foden. "Rb/Sr dating of differentiated cleavage from the upper Adelaidean metasediments at Hallett Cove, southern Adelaide fold belt." Journal of Structural Geology 16, no. 9 (September 1994): 1233–41. http://dx.doi.org/10.1016/0191-8141(94)90066-3.

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8

Sandiford, Mike, John Foden, Shaohua Zhou, and Simon Turner. "Granite genesis and the mechanics of convergent orogenic belts with application to the southern Adelaide Fold Belt." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83, no. 1-2 (1992): 83–93. http://dx.doi.org/10.1017/s026359330000777x.

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ABSTRACTTwo models for the heating responsible for granite generation during convergent deformation may be distinguished on the basis of the length- and time-scales associated with the thermal perturbation, namely: (1) long-lived, lithospheric-scale heating as a conductive response to the deformation, and (2) transient, localised heating as a response to advective heat sources such as mantle-derived melts. The strong temperature dependence of lithospheric rheology implies that the heat advected within rising granites may affect the distribution and rates of deformation within the developing orogen in a way that reflects the thermal regime attendant on granite formation; this contention is supported by numerical models of lithospheric deformation based on the thin-sheet approximation. The model results are compared with geological and isotopic constraints on granite genesis in the southern Adelaide Fold Belt where intrusion spans a 25 Ma convergent deformation cycle, from about 516 to 490 Ma, resulting in crustal thickening to 50–55 km. High-T metamorphism in this belt is spatially restricted to an axis of magmatic activity where the intensity and complexity of deformation is significantly greater, and may have started earlier, than in adjacent low-grade areas. The implication is that granite generation and emplacement is a causative factor in localising deformation, and on the basis of the results of the mechanical models suggests that granite formation occurred in response to localised, transient crustal heating by mantle melts. This is consistent with the Nd- and Sr-isotopic composition of the granites which seems to reflect mixed sources with components derived both from the depleted contemporary mantle and the older crust.

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9

Flo¨ttmann, Thomas, and Patrick James. "Influence of basin architecture on the style of inversion and fold-thrust belt tectonics—the southern Adelaide Fold-Thrust Belt, South Australia." Journal of Structural Geology 19, no. 8 (August 1997): 1093–110. http://dx.doi.org/10.1016/s0191-8141(97)00033-3.

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10

Alias, G., M. Sandiford, M. Hand, and B. Worley. "TheP-Trecord of synchronous magmatism, metamorphism and deformation at Petrel Cove, southern Adelaide Fold Belt." Journal of Metamorphic Geology 20, no. 3 (April 2002): 351–63. http://dx.doi.org/10.1046/j.1525-1314.2002.00373.x.

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11

Gibson, H. J., and K. Stüwe. "Multiphase cooling and exhumation of the southern Adelaide Fold Belt: constraints from apatite fission track data." Basin Research 12, no. 1 (March 18, 2000): 31–45. http://dx.doi.org/10.1046/j.1365-2117.2000.00110.x.

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12

McKirdy, David M., Jamie M. Burgess, Nicholas M. Lemon, Xinke Yu, Andrew M. Cooper, Victor A. Gostin, Richard J. F. Jenkins, and Ross A. Both. "A chemostratigraphic overview of the late Cryogenian interglacial sequence in the Adelaide Fold-Thrust Belt, South Australia." Precambrian Research 106, no. 1-2 (February 2001): 149–86. http://dx.doi.org/10.1016/s0301-9268(00)00130-3.

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13

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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14

Schmidt, Phillip W., and George E. Williams. "Palaeomagnetism of the ejecta-bearing Bunyeroo Formation, late Neoproterozoic, Adelaide fold belt, and the age of the Acraman impact." Earth and Planetary Science Letters 144, no. 3-4 (November 1996): 347–57. http://dx.doi.org/10.1016/s0012-821x(96)00169-0.

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15

Yassaghi, A., P. R. James, and T. Flottmann. "Geometric and kinematic evolution of asymmetric ductile shear zones in thrust sheets, southern Adelaide Fold–Thrust Belt, South Australia." Journal of Structural Geology 22, no. 7 (July 2000): 889–912. http://dx.doi.org/10.1016/s0191-8141(00)00016-x.

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16

Jenkins, Richard J. F., David M. McKirdy, Clinton B. Foster, Teresa O'Leary, and Stephen D. Pell. "The record and stratigraphie implications of organic-walled microfossils from the Ediacaran (terminal Proterozoic) of South Australia." Geological Magazine 129, no. 4 (July 1992): 401–10. http://dx.doi.org/10.1017/s001675680001949x.

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AbstractTwo assemblages of organic-walled microfossils have been recognized in drillcore samples from the late Proterozoic Rodda Beds in theeastern Officer Basin, South Australia. The fossils include tube-like remains and large, simple and sculptured acritarchs. Lithostratigraphic studies and seismic information, in conjunction with previous (albeit limited) acritarch finds, allow local correlation of the Rodda Beds with Ediacaran or terminal Proterozoic sequences in the northern Adelaide Fold Belt (site of the nominated Ediacaran stratotype). The new palynofloras are comparable withacritarch assemblages in the Amadeus Basin of central Australia, and suggest tentative correlations with sequences in China and the U.S.S.R. The presence of isotopically heavy marine carbonate in the lower fossiliferous horizons of the Rodda Beds (σ13CPDB = +3 to +6%0) is consistent with isotopic data from the equivalent interval in China. In contrast, the upper fossiliferous strata occur higher in the Rodda Beds where carbonate is significantly lighter (σ13CPDB = -1 to + 3%0).

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17

Teasdale, J. P., L. L. Pryer, P. G. Stuart-Smith, K. K. Romine, M. A. Etheridge, T. S. Loutit, and D. M. Kyan. "STRUCTURAL FRAMEWORK AND BASIN EVOLUTION OF AUSTRALIA’S SOUTHERN MARGIN." APPEA Journal 43, no. 1 (2003): 13. http://dx.doi.org/10.1071/aj02001.

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The structural evolution of all of the Southern Margin Basins can be explained by episodic reactivation of basement structures in respect to a specific sequence of tectonic events. Three geological provinces dominate the basement geology of the Southern Margin basins. The Eyre, Ceduna, Duntroon and Polda Basins overlie basement of the Archean to Proterozoic Gawler-Antarctic Craton. The Otway and Sorell Basins overlie basement of the Neoproterozoic-early Palaeozoic Adelaide- Kanmantoo Fold Belt. The Bass and Gippsland Basins overlie basement of the Palaeozoic Lachlan Fold Belt. The contrasting basement terranes within the three basement provinces and the structures within and between them significantly influenced the evolution and architecture of the Southern Margin basins.The present-day geometry was established during three Mesozoic extensional basin phases:Late Jurassic–Early Cretaceous NW–SE transtension forming deep rift basins to the west and linked pullapart basins and oblique graben east of the Southwest Ceduna Accommodation Zone; Early–Mid Cretaceous NE–SW extension; and Late Cretaceous NNE–SSW extension leading to continental breakup. At least three, potentially trap forming, inversion events have variably influenced the Southern Margin basins; Mid Cretaceous, Eocene, and Miocene-Recent. Volcanism occurred along the margin during the Late Cretaceous and sporadically through the Tertiary.First-order structural control on Mesozoic rifting and breakup were east–west trending basement structures of the southern Australian fracture zone. Second-order controls include:Proterozoic basement shear zones and/or terrane boundaries in the western Gawler Craton, which controlled basin evolution in the Eyre and Ceduna Subbasins; Neoproterozoic structures, which significantly influenced basin evolution in the Ceduna sub-basin; Cambro-Ordovician basement shear zones and/or terrane boundaries, which were a primary control on basin evolution in the Otway and Sorell Basins; and Palaeozoic structures in the Lachlan Fold Belt, which controlled basin evolution in the Bass and Gippsland Basins.A SEEBASE™ (Structurally Enhanced view of Economic Basement) model for the Southern Margin basins has been constructed to show basement topography. When used in combination with a rigorous interpretation of the structural evolution of the margin, it provides a foundation for basin phase and source rock distribution, hydrocarbon fluid focal points and trap type/distribution.

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18

Jago, J. B., J. C. Gum, A. C. Burtt, and P. W. Haines. "Stratigraphy of the Kanmantoo Group: A critical element of the Adelaide Fold Belt and the Palaeo‐Pacific plate margin, Eastern Gondwana." Australian Journal of Earth Sciences 50, no. 3 (June 2003): 343–63. http://dx.doi.org/10.1046/j.1440-0952.2003.00997.x.

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19

Tappert, R., J. Foden, K. Muehlenbachs, and K. Wills. "Garnet Peridotite Xenoliths and Xenocrysts from the Monk Hill Kimberlite, South Australia: Insights into the Lithospheric Mantle beneath the Adelaide Fold Belt." Journal of Petrology 52, no. 10 (August 12, 2011): 1965–86. http://dx.doi.org/10.1093/petrology/egr036.

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20

Turner, Simon, John Foden, Mike Sandiford, and David Bruce. "Sm-Nd isotopic evidence for the provenance of sediments from the Adelaide Fold Belt and southeastern Australia with implications for episodic crustal addition." Geochimica et Cosmochimica Acta 57, no. 8 (April 1993): 1837–56. http://dx.doi.org/10.1016/0016-7037(93)90116-e.

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21

CHEN, Y. D., and S. F. LIU. "Precise U–Pb zircon dating of a post-D2 meta-dolerite: constraints for rapid tectonic development of the southern Adelaide Fold Belt during the Cambrian." Journal of the Geological Society 153, no. 1 (January 1996): 83–90. http://dx.doi.org/10.1144/gsjgs.153.1.0083.

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22

Marshak, Stephen, and T. Flöttmann. "Structure and origin of the Fleurieu and Nackara Arcs in the Adelaide fold-thrust belt, South Australia: Salient and recess development in the Delamerian Orogen." Journal of Structural Geology 18, no. 7 (July 1996): 891–908. http://dx.doi.org/10.1016/0191-8141(96)00016-8.

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23

YASSAGHI, A., P. R. JAMES, T. FLOTTMANN, and C. N. WINSOR. "P-T conditions and kinematics of shear zones from the southern Adelaide Fold-Thrust Belt, South Australia: insights into the dynamics of a deeply eroded orogenic wedge." Australian Journal of Earth Sciences 51, no. 2 (April 2004): 301–17. http://dx.doi.org/10.1111/j.1400-0952.2004.01059.x.

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24

Turner, Simon, Janne Blichert-Toft, Bruce Schaefer, Francis Albarède, and John Foden. "A reappraisal of the evolution of the palaeo-Pacific margin of Gondwana from the Pb and Os isotope systematics of igneous rocks from the southern Adelaide fold belt, South Australia." Gondwana Research 45 (May 2017): 152–62. http://dx.doi.org/10.1016/j.gr.2017.01.006.

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25

Flöttmann, Thomas, Pat James, Jamie Rogers, and Tim Johnson. "Early Palaeozoic foreland thrusting and basin reactivation at the Palaeo-Pacific margin of the southeastern Australian Precambrian Craton: a reappraisal of the structural evolution of the Southern Adelaide Fold-Thrust Belt." Tectonophysics 234, no. 1-2 (June 1994): 95–116. http://dx.doi.org/10.1016/0040-1951(94)90206-2.

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26

Turner, Simon, Trevor Ireland, John Foden, Elena Belousova, Gerhard Wörner, and Jelte Keeman. "A comparison of granite genesis in the Adelaide Fold Belt and Glenelg River Complex using U-Pb, Hf and O isotopes in zircon." Journal of Petrology, October 11, 2022. http://dx.doi.org/10.1093/petrology/egac102.

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Abstract We present new U-Pb ages and Hf and O isotope data for zircon from I-, S- and A-type granites from both the western and eastern edges of the Delamerian Orogen in southeastern Australia. The I-type Tanunda Creek Gneiss contains zircon populations of 507 ± 4 Ma and 492 ± 6 Ma inferred to reflect igneous and metamorphic ages, respectively. The I-type Palmer Granite yielded an age of 509 ± 3 Ma and the Port Elliot S-type Granite has a magmatic age of 508 ± 7 Ma. Inherited zircon in these granites range from 1092 to 3343 Ma, probably derived from assimilation of Adelaide Group sediments. The Murray Bridge A-type Granite is 490 ± 2 Ma in age and lacks inherited zircon. In the Glenelg River Complex, a S-type migmatite from near Harrow contains a complex zircon population. It is most likely ~ 500 Ma in age and has inherited zircon of 550-700, 1000-1100 and 2437 Ma, hence matching those from the Kanmantoo Group. From this and detrital zircons ages we infer that only the Kanmantoo Group extends across the Murray Basin into the Glenelg River Complex. The Wando Tonalite and Loftus Creek I-type granites yielded ages of 501 ± 2 Ma and 486 ± 3 Ma, respectively. Zircon from the Dergholm Granite has suffered Pb loss and the best age estimate for this granite is 488 ± 5 Ma. Combining all the granite data together, εHft and δ18O in the magmatic zircon range from 5.6 to -10.3 and from 5.8 to 8.1, respectively, and are well correlated. The zircon indicate the same temporal and compositional evolution of granitic petrogenesis across ~ 300 km of strike, reaffirming the notion that these terranes form part of the same orogen. Westward-directed subduction caused orogenic thickening, heating and increasing amounts of crustal contribution. This was followed by convective thinning of the thickened mantle lithosphere and a return to more primitive magmas lacking significant crustal contributions. It contrasts significantly with inferred granite petrogenesis and tectonic style in the younger Lachlan and New England Fold Belts further east that were not built upon extended cratonic lithosphere.

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27

"Problems in structural correlation from low to high metamorphic grade: examples from the Halls Creek Mobile Zone, East Kimberleys, and the Adelaide Fold Belt." Journal of Structural Geology 7, no. 3-4 (January 1985): 489. http://dx.doi.org/10.1016/0191-8141(85)90051-3.

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