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Complex subduction
2010
Nature Geoscience
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Mechanics of basin inversion
1999
Tectonophysics
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Hand and Sandiford, 1999) . ...
In a companion paper (Hand and Sandiford, 1999) the results of the analysis presented in this paper are applied to the development of intracratonic orogeny associated with basin inversion in central ...
doi:10.1016/s0040-1951(99)00023-2
fatcat:4urtphqgr5dzfla4kc2gcaop6i
Interacting Intraplate Fault Systems in Australia: The 2012 Thorpdale, Victoria Seismic Sequences
2019
Journal of Geophysical Research - Solid Earth
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, 2003; Sandiford & Quigley, 2009) . ...
In Southeastern Australia, deformation is slow with strain rates estimated to be less than 10 −9 year −1 (Sandiford et al., 2004) . ...
doi:10.1029/2018jb016945
fatcat:bym4zg6sunappeys2hsbwosl4q
Tectonic geomorphology of Australia
2010
Geological Society Special Publication
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2003a; Sandiford et al. 2004) . ...
Further details have been given by Sandiford (2003b). ...
doi:10.1144/sp346.13
fatcat:kmqxogmycbhind3zngm4pfi7ym
Dynamic Antarctic Ice: Agent for Mid-Pleistocene Transition
2007
PAGES news
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Bowler and miKe sandiford
School of Earth Sciences, University of Melbourne, Australia; jbowler@unimelb.edu.au
Ma; b) Shaded relief image of the Murray Basin derived from the Shuttle Radar (SRTM) ...
doi:10.22498/pages.15.2.16
fatcat:hsm3cr4sqngh3eozmxgupekc44
Enhanced intraplate seismicity along continental margins: Some causes and consequences
2008
Tectonophysics
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Sandiford, 2003) . ...
Sandiford, 1999) . ...
doi:10.1016/j.tecto.2008.06.004
fatcat:o4tcoh3yszgcjakmybup7wk4bu
Seismic moment release during slab rupture beneath the Banda Sea
2008
Geophysical Journal International
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The highest intermediate depth moment release rates in Indonesia occur in the slab beneath the largely submerged segment of the Banda arc in the Banda Sea to the east of Roma, termed the Damar Zone. The most active, western-part of this zone is characterised by down-dip extension, with moment release rates (~10 18 Nm/yr per 50 kms strike length) implying the slab is stretching at ~10 -14 s -1 consistent with near complete slab decoupling across the 100-200 km depth range. Differential vertical
doi:10.1111/j.1365-246x.2008.03838.x
fatcat:hpurrkgb7fcwngjninzhiayvbm
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... tretching along the length of the Damar Zone is consistent with a slab rupture front at ~100-200kms depth beneath Roma propagating eastwards at ~100 kms/myr. Complexities in the slab deformation field are revealed by a narrow zone of anomalous in-plane P-axis trends beneath Damar, where sub-horizontal constriction suggests extreme stress concentrations ~ 100 kms ahead of the slab rupture front. Such stress concentrations may explain the anomalously deep ocean gateways in this region, in which case ongoing slab rupture may have played a key role in modulating the Indonesian throughflow in the Banda Sea over the last few million years.
Modes of active intraplate deformation, Flinders Ranges, Australia
2005
Tectonics
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Sandiford, D. L. Hansen, and M. Quigley (2005), Modes of active intraplate deformation, Flinders Ranges, Australia, Tectonics, 24, TC6006, ...
Sandiford et al. [1998] have previously investigated the rheological response of the Brace-Goetze lithosphere to the burial of a radiogenic basement beneath a cover sequence, while Sandiford and McLaren ...
The interested reader is referred to both Sandiford et al. [1998] and Sandiford and McLaren [2002] for full details of the
TC6006 CÉ LÉ RIER ET AL.: ACTIVE DEFORMATION, FLINDERS RANGES model parameters ...
doi:10.1029/2004tc001679
fatcat:oyracycopzh63ee75hns6bd2va
High geothermal gradient metamorphism during thermal subsidence
1998
Earth and Planetary Science Letters
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Sandiford and Hand's [16] approach was essentially parametric in as much as they did not address the geological setting in which such conditions are likely to prevail. ...
As discussed by Sandiford and Hand [16] this model appears broadly consistent with modern heat flow-surface heat production data in a number of HGGM terranes in Australia. ...
doi:10.1016/s0012-821x(98)00183-6
fatcat:l25rdgsprve45b3eyiduaxq7zm
Lower crustal rheological expression in inverted basins
2006
Geological Society Special Publication
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1999; Hansen & Nielsen 2002; Sandiford et al. 2003) . ...
In particular, the lower crust and upper Sandiford 1999 ). ...
doi:10.1144/gsl.sp.2006.253.01.14
fatcat:nzocvy373zhetcwrymzjw624fa
Hydrogeological implications of active tectonics in the Great Artesian Basin, Australia
2019
Hydrogeology Journal
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Sandiford and Quigley 2009 ). ...
Sandiford 2003; Sandiford et al. 2004; Celerier et al. 2005 ). This has been attributed to progressive build-up of Fig. 9 Lake Eyre Basin smoothed surface topography (1°median filter). ...
doi:10.1007/s10040-019-02046-4
fatcat:czxttubzdbferixzx6wjgk67yq
Low thermal Peclet number intraplate orogeny in central Australia
2002
Earth and Planetary Science Letters
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The late Phanerozoic Alice Springs Orogen in central Australia is an archetypal intraplate orogen characterised by a dense, granulitic core exhumed from beneath a carapace comprising a highly radiogenic granitic mid-upper crust and sediments deposited in a shallow intracratonic basin. Exhumation occurred in large part along a crustal penetrative fault system, the Redbank Shear Zone, producing one of the largest gravity anomalies (V150 mgal) known from the continental interiors. The lithospheric
doi:10.1016/s0012-821x(02)00723-9
fatcat:6ckm6qbj2jeotlierf7tsrhemy
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... strength implied by the preservation of this anomaly for more than 300 Myr raises the intriguing conundrum of what localised the intraplate deformation in the first place. Available biostratigraphic and thermochronologic data imply bulk convergence rates of less than 1 mm/yr for the orogen as a whole, several orders of magnitude lower than typical of plate margin orogens. The thermal and mechanical evolution of intraplate orogens deformed at such low thermal Peclet numbers differs in fundamental ways from plate margin orogens. In particular, at such low thermal Peclet numbers the conductive response to exhumation of heat sources cools the mid to deep crust during progressive orogenic activity. This is consistent with the hypothesis that the density structure and associated gravity anomalies may have been locked-in by virtue of the strength acquired during the orogenic process provided that the lithospheric strength changes associated with a reduction in average crustal temperature of 20^30 ‡C are of the same order as the forces that drive intraplate deformation. ß 2002 Elsevier Science B.V. All rights reserved. Keywords: thermal properties; heat sources; intraplate processes; orogenic belts 0012-821X / 02 / $^see front matter ß 2002 Elsevier Science B.V. All rights reserved. PII: S 0 0 1 2 -8 2 1 X ( 0 2 ) 0 0 7 2 3 -9 *
Intraplate deformation in central Australia, the link between subsidence and fault reactivation
1999
Tectonophysics
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Karner, 1991; Watts, 1992; Sandiford, 1999) . ...
Neil and Houseman, 1997; Sandiford and Hand, 1998a) . ...
doi:10.1016/s0040-1951(99)00009-8
fatcat:brx5o35qqfbyfbty53pfqwwq2u
Estimating the value of electricity storage in an energy-only wholesale market
2015
Applied Energy
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The 2008 Wenchuan earthquake and active tectonics of Asia
2011
Journal of Asian Earth Sciences
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