ORCID Profile
0000-0002-9757-745X
Current Organisation
University of Melbourne
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Research Topics
In Research Link Australia (RLA), "Research Topics" refer to ANZSRC FOR and SEO codes. These topics are either sourced from ANZSRC FOR and SEO codes listed in researchers' related grants or generated by a large language model (LLM) based on their publications.
Top 5 Research Topics
ANZSRC Field of Research (FoR)
Geology | Geotectonics | Geodynamics | Tectonics | Geophysics | Geochronology And Isotope Geochemistry | Geochronology | Geochemistry | Basin Analysis | Sedimentology | Igneous And Metamorphic Petrology | Structural Geology | Petroleum Geology | Geomechanics and Resources Geotechnical Engineering | Resources Engineering and Extractive Metallurgy | Petroleum and Reservoir Engineering | Other Stratigraphy (Incl. Sequence Stratigraphy) | Geology Not Elsewhere Classified | Seismology and Seismic Exploration | Simulation And Modelling | Geomorphology and Regolith and Landscape Evolution | Archaeological Science | Climatology (Incl. Palaeoclimatology) | Radiometrics | Mathematical Sciences Not Elsewhere Classified | Environmental Sciences Not Elsewhere Classified | Structural Geology | Geophysics Not Elsewhere Classified
ANZSRC Socio-Economic Objective (SEO)
Earth sciences | Expanding Knowledge in the Earth Sciences | Natural Hazards not elsewhere classified | Other | Management of Greenhouse Gas Emissions from Mineral Resource Activities | Management of Greenhouse Gas Emissions from Electricity Generation | Mineral Exploration not elsewhere classified | Mathematical sciences | Climate variability | Geothermal Energy Extraction | Oil and Gas Extraction | Renewable energy not elsewhere classified (e.g. geothermal) | Oil and gas | Uranium | Geothermal Energy | Oil and Gas Exploration | Exploration | Natural Hazards in Coastal and Estuarine Environments | Geothermal Exploration | Copper Ore Exploration |
Related Links
Publications
Geomorphic constraints on the Late Neogene tectonics of the Otway Range, Victoria
Publisher: Informa UK Limited
Date: 02-2003
Phase relationships in Buchan facies series pelitic assemblages: calculations with application to andalusite-staurolite parageneses in the Mount Lofty Ranges, South Australia
Publisher: Springer Science and Business Media LLC
Date: 03-1992
DOI: 10.1007/BF00310886
Style and timing of late Quaternary faulting on the Lake Edgar fault, southwest Tasmania, Australia: Implications for hazard assessment in intracratonic areas
Publisher: Geological Society of America
Date: 2011
Archeological and historical database on the medieval earthquakes of the central himalaya: Ambiguities and inferences
Publisher: Seismological Society of America (SSA)
Date: 24-10-2013
DOI: 10.1785/0220130077
Cenozoic deformation in the Otway Basin, southern Australian margin: implications for the origin and nature of post-breakup compression at rifted margins
Publisher: Wiley
Date: 17-01-2014
DOI: 10.1111/BRE.12035
Origin of the in situ stress field in south-eastern Australia
Publisher: Wiley
Date: 04-08-2004
India‐Asia convergence: Insights from burial and exhumation of the Xigaze fore‐arc basin, south Tibet
Publisher: American Geophysical Union (AGU)
Date: 05-2017
DOI: 10.1002/2017JB014080
GipNet - Baseline Environmental Data Gathering and Measurement Technology Validation for Nearshore Marine Carbon Storage
Publisher: Elsevier BV
Date: 07-2017
Late Neogene strandlines of southern Victoria: A unique record of eustasy and tectonics in southeast Australia
Publisher: Informa UK Limited
Date: 04-2005
A staurolite-talc assemblage in tourmaline-phlogopite-chlorite schist from northern Victoria Land, Antarctica, and its petrogenetic significance
Publisher: Springer Science and Business Media LLC
Date: 10-1984
DOI: 10.1007/BF00381290
Sapphirine and spinel phase relationships in the system FeO-MgO-Al2 O3 -SiO2 -TiO2 -O2 in the presence of quartz and hypersthene
Publisher: Springer Science and Business Media LLC
Date: 1988
DOI: 10.1007/BF00371910
Evaluating slab-plate coupling in the Indo-Australian plate
Publisher: Geological Society of America
Date: 2005
DOI: 10.1130/G20898.1
Granite production in the Delamerian Orogen, South Australia
Publisher: Geological Society of London
Date: 09-2002
Modes of active intraplate deformation, Flinders Ranges, Australia
Publisher: American Geophysical Union (AGU)
Date: 17-11-2005
DOI: 10.1029/2004TC001679
The long-term thermal consequences of rifting: Implications for basin reactivation
Publisher: Wiley
Date: 28-02-2003
Geochemistry and geochronology of the Rathjen Gneiss: Implications for the early tectonic evolution of the Delamerian Orogen
Publisher: Informa UK Limited
Date: 06-1999
Mechanical consequences of granite emplacement during high-T, low-P metamorphism and the origin of anticlockwise PT paths
Publisher: Elsevier BV
Date: 10-1991
Lifespan of mountain ranges scaled by feedbacks between landsliding and erosion by rivers
Publisher: Springer Science and Business Media LLC
Date: 06-2013
DOI: 10.1038/NATURE12218
Abstract: An important challenge in geomorphology is the reconciliation of the high fluvial incision rates observed in tectonically active mountain ranges with the long-term preservation of significant mountain-range relief in ancient, tectonically inactive orogenic belts. River bedrock erosion and sediment transport are widely recognized to be the principal controls on the lifespan of mountain ranges. But the factors controlling the rate of erosion and the reasons why they seem to vary significantly as a function of tectonic activity remain controversial. Here we use computational simulations to show that the key to understanding variations in the rate of erosion between tectonically active and inactive mountain ranges may relate to a bidirectional coupling between bedrock river incision and landslides. Whereas fluvial incision steepens surrounding hillslopes and increases landslide frequency, landsliding affects fluvial erosion rates in two fundamentally distinct ways. On the one hand, large landslides overwhelm the river transport capacity and cause upstream build up of sediment that protects the river bed from further erosion. On the other hand, in delivering abrasive agents to the streams, landslides help accelerate fluvial erosion. Our models illustrate how this coupling has fundamentally different implications for rates of fluvial incision in active and inactive mountain ranges. The coupling therefore provides a plausible physical explanation for the preservation of significant mountain-range relief in old orogenic belts, up to several hundred million years after tectonic activity has effectively ceased.
The 2008 Wenchuan earthquake and active tectonics of Asia
Publisher: Elsevier BV
Date: 03-2011
High geothermal gradient metamorphism during thermal subsidence
Publisher: Elsevier BV
Date: 11-1998
The metamorphic evolution of granulites at Fyfe Hills; implications for Archaean crustal thickness in Enderby Land, Antarctica
Publisher: Wiley
Date: 06-1985
Contribution of deviatoric stresses to metamorphic P‐T paths: an example appropriate to low‐P, high‐T metamorphism
Publisher: Wiley
Date: 07-1994
Impacts of LNG Export and Market Power on Australian Electricity Market Dynamics, 2016–2019
Publisher: Springer Science and Business Media LLC
Date: 09-11-2020
Holocene climate change in arid Australia from speleothem and alluvial records
Publisher: SAGE Publications
Date: 12-07-2010
Abstract: New high-resolution MC-ICPMS U/Th ages and C and O isotopic analyses from a Holocene speleothem in arid south-central Australia provide evidence for increased effective precipitation (EP) relative to present at c. 11.5 ka and c. 8—5 ka, peak moisture at 7—6 ka, and onset of an arid climate similar to present by c. 5 ka. δ 18 O and δ 13 C time-series data exhibit marked ( +1‰) contemporaneous excursions over base-line values of −5.3‰ and −11.0‰, respectively, suggesting pronounced moisture variability during the early middle Holocene ‘climatic optimum’. Optically stimulated luminescence and 14 C ages from nearby terraced aggradational alluvial deposits indicate a paucity of large floods in the Late Pleistocene and at least five large flood events in the last c. 6 kyr, interpreted to mark an increased frequency of extreme rainfall events in the middle Holocene despite overall reduced EP. Increased EP in south-central Australia during the early to middle Holocene resulted from (1) decreased El Niño-Southern Oscillation (ENSO) variability, which reduced the frequency of El Niño-triggered droughts, (2) the prevalence of a more La Niña-like mean climatic state in the tropical Pacific Ocean, which increased available atmospheric moisture, and (3) a southward shift in the Intertropical Convergence Zone (ICTZ), which allowed tropical summer storms associated with the Australian summer monsoon (ASM) to penetrate deeper into the southern part of the continent. The onset of heightened aridity and apparent increase in large flood frequency at c. 5 ka is interpreted to indicate the establishment of an ENSO-like climate in arid Australia in the late Holocene, consistent with a variety of other terrestrial and marine proxies. The broad synchroneity of Holocene climate change across much of the Australian continent with changes in ENSO behavior suggests strong teleconnections amongst ENSO and the other climate systems such as the ASM, Indian Ocean Dipole, and Southern Annular Mode.
Contrasting styles of Proterozoic crustal evolution: A hot-plate tectonic model for Australian terranes
Publisher: Geological Society of America
Date: 08-2005
DOI: 10.1130/G21544AR.1
Abstract: Proterozoic terranes in Australia record complex tectonic histories in the interval 1900– 1400 Ma that have previously been interpreted by means of simple intracratonic or plate-tectonic models. However, these models do not fully account for (1) repeated tectonic reactivation (both orogenesis and rifting), (2) mainly high-temperature–low-pressure metamorphism, (3) rifting and sag creating thick sedimentary basins, (4) the nature and timing of voluminous felsic magmatism, (5) relatively large aspect ratio orogenic belts, and (6) a general paucity of diagnostic plate-boundary features. A key to understanding these histories is the observation that Australian Proterozoic terranes are characterized by an extraordinary, but heterogeneous, enrichment of the heat-producing elements. This enrichment must contribute to long-term lithospheric weakening, and thus we advocate a hybrid lithospheric evolution model with two tectonic switches: plate-boundary–derived stresses and heat-producing-element–related lithospheric weakening. The Australian Proterozoic crustal growth record is therefore a function of the magnitude of these stresses, the way in which the heat-producing elements are distributed, and how both of these change with time.
Quaternary faults of south-central Australia: Palaeoseismicity, slip rates and origin
Publisher: Informa UK Limited
Date: 04-2006
A trapdoor mechanism for slab tearing and melt generation in the northern Andes
Publisher: No publisher found
Date: 2018
Deformation volume and cleavage development in metasedimentary rocks from the Ballarat slate belt
Publisher: Elsevier BV
Date: 1988
Heat refraction and low‐pressure metamorphism in the northern Flinders Ranges, South Australia
Publisher: Informa UK Limited
Date: 06-1995
Structural evolution of the lanterman metamorphic complex, northern victoria land, Antarctica
Publisher: Informa UK Limited
Date: 07-1985
Secular trends in the thermal evolution of metamorphic terrains
Publisher: Elsevier BV
Date: 10-1989
Stalagmite growth perturbations from the Kumaun Himalaya as potential earthquake recorders
Publisher: Springer Science and Business Media LLC
Date: 12-12-2016
Some causes and consequences of high-temperature, low-pressure metamorphism in the eastern mt lofty ranges, south australia
Publisher: Informa UK Limited
Date: 06-1995
Some remarks on the stability of blueschists and related high P-low T assemblages in continental orogens
Publisher: Elsevier BV
Date: 1991
The Fingerprints of Flexure in Slab Seismicity
Publisher: American Geophysical Union (AGU)
Date: 08-2020
DOI: 10.1029/2019TC005894
Neotectonics of southeastern Australia: Linking the Quaternary faulting record with seismicity and in situ stress
Publisher: Geological Society of America
Date: 2003
Cenozoic low temperature cooling history of the Northern Tethyan Himalaya in Zedang, SE Tibet and its implications
Publisher: Elsevier BV
Date: 03-2015
Did the Delamerian Orogeny Start in the Neoproterozoic?
Publisher: University of Chicago Press
Date: 09-2009
DOI: 10.1086/600866
Enhanced intraplate seismicity along continental margins: Some causes and consequences
Publisher: Elsevier BV
Date: 10-2008
Shear-zone deformation in the Yackandandah Granite, northeast Victoria
Publisher: Informa UK Limited
Date: 06-1988
High radiogenic heat-producing granites and metamorphism- An example from the western Mount Isa inlier, Australia
Publisher: Geological Society of America
Date: 1999
Current strain accumulation in the hinterland of the northwest Himalaya constrained by landscape analyses, basin-wide denudation rates, and low temperature thermochronology
Publisher: Elsevier BV
Date: 11-2017
Post-collisional exhumation of the Indus-Yarlung suture zone and Northern Tethyan Himalaya, Saga, SW Tibet
Publisher: Elsevier BV
Date: 12-2018
Detrital zircon U-Pb and 40Ar/39Ar hornblende ages from the Aileu Complex, Timor-Leste: Provenance and metamorphic cooling history
Publisher: Geological Society of London
Date: 12-12-2014
DOI: 10.1144/JGS2012-065
Amphibolites with staurolite and other aluminous minerals: Calculated mineral equilibria in NCFMASH
Publisher: Wiley
Date: 2000
Distribution of palaeozoic reworking in the Western Arunta Region and northwestern Amadeus Basin from 40Ar/39Ar thermochronology: Implications for the evolution of intracratonic basins
Publisher: Wiley
Date: 18-05-2009
Thermal weakening localizes intraplate deformation along the southern Australian continental margin
Publisher: Elsevier BV
Date: 05-2011
Isotopic (U-Pb, Nd) and geochemical constraints on the origins of the Aileu and Gondwana sequences of Timor
Publisher: Elsevier BV
Date: 02-2017
Source of the Lachlan fold belt flysch linked to convective removal of the lithospheric mantle and rapid exhumation of the Delamerian-Ross fold belt
Publisher: Geological Society of America
Date: 1996
Mechanics of basin inversion
Publisher: Elsevier BV
Date: 05-1999
The origins of the Australian stress field
Publisher: Elsevier BV
Date: 07-1995
Geodynamics: Complex subduction
Publisher: Springer Science and Business Media LLC
Date: 08-2010
DOI: 10.1038/NGEO928
Observations on the tectonic evolution of the southern Adelaide Fold Belt
Publisher: Elsevier BV
Date: 11-1992
Deep crustal metamorphism during continental extension: modern and ancient examples
Publisher: Elsevier BV
Date: 08-1986
Uranium-series isotope and thermal constraints on the rate and depth of silicic magma genesis
Publisher: Geological Society of London
Date: 2008
DOI: 10.1144/SP304.9
Seismic response to slab rupture and variation in lithospheric structure beneath the Savu Sea, Indonesia
Publisher: Elsevier BV
Date: 03-2010
Geomorphic and cosmogenic nuclide constraints on escarpment evolution in an intraplate setting, Darling Escarpment, Western Australia
Publisher: Wiley
Date: 10-03-2011
DOI: 10.1002/ESP.2058
Rb Sr dating of differentiated cleavage from the upper Adelaidean metasediments at Hallett Cove, southern Adelaide fold belt
Publisher: Elsevier BV
Date: 12-1995
Conductive incubation and the origin of dome-and-keel structure in Archean granite-greenstone terrains: A model based on the eastern Pilbara Craton, Western Australia
Publisher: American Geophysical Union (AGU)
Date: 27-01-2004
DOI: 10.1029/2002TC001452
Sm-Nd isotopic evidence for the provenance of sediments from the Adelaide Fold Belt and southeastern Australia with implications for episodic crustal addition
Publisher: Elsevier BV
Date: 04-1993
TOPO-OZ: Insights into the various modes of intraplate deformation in the Australian continent
Publisher: Elsevier BV
Date: 09-2009
Long-term thermal consequences of the redistribution of heat-producing elements associated with large-scale granitic complexes
Publisher: Wiley
Date: 2002
The big crunch: Physical and chemical expressions of arc/continent collision in the Western Bismarck arc
Publisher: Elsevier BV
Date: 02-2010
Ridge torques and continental collision in the Indian-Australian plate
Publisher: Geological Society of America
Date: 1995
Metamorphic events in the eastern Arunta Inlier, Part 1. Metamorphic petrology
Publisher: Elsevier BV
Date: 02-1995
Multi-stage exhumation history of the West Kunlun orogen and the amalgamation of the Tibetan Plateau
Publisher: Elsevier BV
Date: 12-2019
Retrospective modeling of the merit-order effect on wholesale electricity prices from distributed photovoltaic generation in the Australian National Electricity Market
Publisher: Elsevier BV
Date: 07-2013
Estimating the value of electricity storage in an energy-only wholesale market
Publisher: Elsevier BV
Date: 12-2015
Structural geometry of a thick-skinned fold-thrust belt termination: The Olary Block in the Adelaide Fold Belt, South Australia
Publisher: Informa UK Limited
Date: 04-2000
Beryllium and other trace elements in paragneisses and anatectic veins of the ultrahigh-temperature Napier complex, Enderby land, East Antarctica: The role of sapphirine
Publisher: Oxford University Press (OUP)
Date: 13-01-2006
Modelling the contempory stress field and its implications for hydrocarbon exploration.
Publisher: Informa UK Limited
Date: 03-1997
DOI: 10.1071/EG997088
Buried inset-valleys in the eastern Yilgarn Craton, Western Australia: Geomorphology, age, and allogenic control
Publisher: University of Chicago Press
Date: 07-2005
DOI: 10.1086/430244
Geomorphology reveals active décollement geometry in the central Himalayan seismic gap
Publisher: GeoScienceWorld
Date: 12-03-2015
DOI: 10.1130/L407.1
Evolution of Ataúro Island: Temporal constraints on subduction processes beneath the Wetar zone, Banda Arc
Publisher: Elsevier BV
Date: 06-2011
Intraplate deformation in central Australia, the link between subsidence and fault reactivation
Publisher: Elsevier BV
Date: 05-1999
Tectonic feedback, intraplate orogeny and the geochemical structure of the crust: A central Australian perspective
Publisher: Geological Society of London
Date: 2001
Asymmetric extension associated with uplift and subsidence in the Transantarctic Mountains and Ross Embayment
Publisher: Elsevier BV
Date: 12-1986
The mechanics of clay smearing along faults
Publisher: Geological Society of America
Date: 2008
DOI: 10.1130/G24975A.1
Tectonic geomorphology of Australia
Publisher: Geological Society of London
Date: 2010
DOI: 10.1144/SP346.13
Thermometrically inferred cooling rates from the Plattengneis, Koralm region, Eastern Alps
Publisher: Elsevier BV
Date: 07-1994
Why are the continents just so?
Publisher: Wiley
Date: 24-05-2010
Atmospheric mercury in the Latrobe Valley, Australia: Case study June 2013
Publisher: University of California Press
Date: 2021
DOI: 10.1525/ELEMENTA.2021.00072
Abstract: Gaseous elemental mercury observations were conducted at Churchill, Victoria, in Australia from April to July, 2013, using a Tekran 2537 analyzer. A strong diurnal variation with daytime average values of 1.2–1.3 ng m–3 and nighttime average values of 1.6–1.8 ng m–3 was observed. These values are significantly higher than the Southern Hemisphere average of 0.85–1.05 ng m–3. Churchill is in the Latrobe Valley, approximately 150 km East of Melbourne, where approximately 80% of Victoria’s electricity is generated from low-rank brown coal from four major power stations: Loy Yang A, Loy Yang B, Hazelwood, and Yallourn. These aging generators do not have any sulfur, nitrogen oxide, or mercury air pollution controls. Mercury emitted in the 2015–2016 year in the Latrobe Valley is estimated to have had an externalized health cost of $AUD88 million. Air pollution mercury simulations were conducted using the Weather Research and Forecast model with Chemistry at 3 × 3 km resolution. Electrical power generation emissions were added using mercury emissions created from the National Energy Market’s 5-min energy distribution data. The strong diurnal cycle in the observed mercury was well simulated (R2 = .49 and P value = 0.00) when soil mercury emissions arising from several years of wet and dry deposition in a radius around the power generators was included in the model, as has been observed around aging lignite coal power generators elsewhere. These results indicate that long-term air and soil s ling in power generation regions, even after the closure of coal fired power stations, will have important implications to understanding the airborne mercury emissions sources.
Climatic variability in Central Indian Himalaya during the last ∼1800 years: Evidence from a high resolution speleothem record
Publisher: Elsevier BV
Date: 08-2013
The origin of Archaean gneisses in the Fyfe Hills Region, Enderby Land; field occurrence, petrography and geochemistry
Publisher: Elsevier BV
Date: 1986
A high-resolution, calibrated airborne radiometric dataset applied to the estimation of crustal heat production in the Archaean northern Pilbara Craton, Western Australia
Publisher: Elsevier BV
Date: 2004
The tilting continent: A new constraint on the dynamic topographic field from Australia
Publisher: Elsevier BV
Date: 09-2007
Author Correction: Next-generation seismic model of the Australian crust from synchronous and asynchronous ambient noise imaging
Publisher: Springer Science and Business Media LLC
Date: 09-05-2023
Tectonic feedback and the ordering of heat producing elements within the continental lithosphere
Publisher: Elsevier BV
Date: 11-2002
Thermal and mechanical controls on the evolution of archean crustal deformation: Examples from Western Australia
Publisher: American Geophysical Union
Date: 2006
DOI: 10.1029/164GM10
The structural evolution of the Fyfe Hills-Khmara Bay region, Enderby Land, East Antarctica
Publisher: Informa UK Limited
Date: 12-1984
Landscape responses to intraplate tectonism: Quantitative constraints from 10Be nuclide abundances
Publisher: Elsevier BV
Date: 09-2007
On the importance of minding one's Ps and Ts: metamorphic processes and quantitative petrology
Publisher: Wiley
Date: 20-05-2010
The hot southern continent: Heat flow and heat production in Australian Proterozoic terranes
Publisher: Geological Society of America
Date: 2003
U-series isotope and geodynamic constraints on mantle melting processes beneath the Newer Volcanic Province in South Australia
Publisher: Elsevier BV
Date: 09-2007
Detecting landscape transience with in situ cosmogenic 14C and 10Be
Publisher: Elsevier BV
Date: 10-2019
The origin of retrograde shear zones in the Napier Complex: implications for the tectonic evolution of Enderby Land, Antarctica
Publisher: Elsevier BV
Date: 1985
Sedimentary thickness variations and deformation intensity during basin inversion in the Flinders Ranges, South Australia
Publisher: Elsevier BV
Date: 12-1998
Distinguishing tectonic from climatic controls on range‐front sedimentation
Publisher: Wiley
Date: 20-09-2007
Rupture Characteristics and Bedrock Structural Control of the 2016 Mw 6.0 Intraplate Earthquake in the Petermann Ranges, Australia
Publisher: Seismological Society of America (SSA)
Date: 12-05-2020
DOI: 10.1785/0120190266
Abstract: The 20 May 2016 surface-rupturing intraplate earthquake in the Petermann Ranges is the largest onshore earthquake to occur in the Australian continent in 19 yr. We use in situ and Interferometric Synthetic Aperture Radar surface observations, aftershock distribution, and the fitting of P-wave source spectra to determine source properties of the Petermann earthquake. Surface observations reveal a 21-km-long surface rupture trace (strike=294°±29°) with heterogeneous vertical displacements (& .1–0.96 m). Aftershock arrays suggest a triangular-shaped rupture plane (dip ≈ 30°) that intersects the subsurface projection of the major geophysical structure (Woodroffe thrust [WT]) proximal to the preferred location of the mainshock hypocenter, suggesting the mainshock nucleated at a fault junction. Footwall seismicity includes apparent southwest-dipping Riedel-type alignments, including possible activation of the deep segment of the WT. We estimate a moment magnitude (Mw) of 6.0 and a corner frequency (fc) of 0.2 Hz, respectively, from spectral fitting of source spectra in the 0.02–2 Hz frequency band. These translate into a fault area of 124 km2 and an average slip of 0.36 m. The estimated stress drop of 2.2 MPa is low for an intraplate earthquake we attribute this to low-frictional slip (effective coefficient of friction & .015) along rupture-parallel phyllosilicate-rich surfaces within the host rock fabric with possible additional contributions from elevated pore-fluid pressures.
Seismic moment release during slab rupture beneath the Banda Sea
Publisher: Oxford University Press (OUP)
Date: 08-2008
A new strategy for discrete element numerical models: 2. Sandbox applications
Publisher: American Geophysical Union (AGU)
Date: 05-2007
DOI: 10.1029/2006JB004558
Changes in stable isotope ratios of metapelites and marbles during regional metamorphism, Mount Lofty Ranges, South Australia: implications for crustal scale fluid flow
Publisher: Springer Science and Business Media LLC
Date: 07-1995
DOI: 10.1007/BF00306509
Corrigendum to “Multi-stage exhumation history of the West Kunlun orogen and the amalgamation of the Tibetan Plateau” [Earth Planet. Sci. Lett. 528 (2019) 115833](S0012821X19305254)(10.1016/j.epsl.2019.115833)
Publisher: Elsevier BV
Date: 2020
Plate-scale potential-energy distributions and the fragmentation of ageing plates
Publisher: Elsevier BV
Date: 08-1994
High-precision geothermobarometry across the high Himalayan metamorphic sequence, Langtang Valley, Nepal
Publisher: Wiley
Date: 11-2000
Rb/Sr dating of differentiated cleavage from the upper Adelaidean metasediments at Hallett Cove, southern Adelaide fold belt
Publisher: Elsevier BV
Date: 09-1994
Palaeozoic synorogenic sedimentation in central and northern Australia: A review of distribution and timing with implications for the evolution of intracontinental orogens
Publisher: Informa UK Limited
Date: 12-2001
A trapdoor mechanism for slab tearing and melt generation in the northern Andes
Publisher: Geological Society of America
Date: 09-11-2019
DOI: 10.1130/G45429.1
Controls on the locus of intraplate deformation in central Australia
Publisher: Elsevier BV
Date: 10-1998
Long-term thermal consequences of tectonic activity at Mount Isa, Australia: Implications for polyphase tectonism in the proterozoic
Publisher: Geological Society of London
Date: 2001
Heat flow and inferred ground surface temperature history at Tynong North, southeastern Australia
Publisher: Informa UK Limited
Date: 18-08-2017
Recent contribution of sediments and fluids to the mantle's volatile budget
Publisher: Springer Science and Business Media LLC
Date: 20-11-2012
DOI: 10.1038/NGEO1325
Regional geochemistry and continental heat flow: Implications for the origin of the South Australian heat flow anomaly
Publisher: Elsevier BV
Date: 30-11-2000
The fingerprints of flexure in slab seismicity
Publisher: California Digital Library (CDL)
Date: 27-09-2019
40Ar/39Ar thermochronology of the Kampa Dome, southern Tibet: Implications for tectonic evolution of the North Himalayan gneiss domes
Publisher: Elsevier BV
Date: 08-2006
Low thermal Peclet number intraplate orogeny in central Australia
Publisher: Elsevier BV
Date: 07-2002
Origins of large-volume, compositionally zoned volcanic eruptions
Publisher: American Geophysical Union (AGU)
Date: 12-2010
DOI: 10.1029/2009JB007195
Mantle-lithospheric deformation and crustal metamorphism with some speculations on the thermal and mechanical significance of the Tauern Event, Eastern Alps
Publisher: Elsevier BV
Date: 02-1995
Tectonic stresses in the African plate: constraints on the ambient lithospheric stress state
Publisher: Geological Society of America
Date: 1994
Lower crustal rheological expression in inverted basins
Publisher: Geological Society of London
Date: 2006
Metamorphic evolution of aluminous granulites from Labwor Hills, Uganda
Publisher: Springer Science and Business Media LLC
Date: 02-1987
DOI: 10.1007/BF00381271
Present-day stresses, seismicity and Neogene-to-Recent tectonics of Australia's ‘passive’ margins: intraplate deformation controlled by plate boundary forces
Publisher: Geological Society of London
Date: 2008
DOI: 10.1144/SP306.3
Structural geometry and controls on basement-involved deformation in the northern Flinders Ranges, Adelaide Fold Belt, South Australia
Publisher: Informa UK Limited
Date: 06-1999
Interactions of 3D mantle flow and continental lithosphere near passive margins
Publisher: Elsevier BV
Date: 03-2010
Bedrock erosion and relief production in the northern Flinders Ranges, Australia
Publisher: Wiley
Date: 2007
DOI: 10.1002/ESP.1459
A description of metamorphic PTt paths with implications for low-P high-T metamorphism
Publisher: Elsevier BV
Date: 04-1995
Late proterozoic deformation in the amadeus basin, central Australia
Publisher: Informa UK Limited
Date: 09-1992
Granite genesis and the mechanics of convergent orogenic belts with application to the southern Adelaide Fold Belt
Publisher: Geological Society of America
Date: 1992
DOI: 10.1130/SPE272-P83
Some remarks on high‐temperature—low‐pressure metamorphism in convergent orogens
Publisher: Wiley
Date: 05-1991
A granulite facies kalsilite-leucite-hibonite association from Punalur, Southern India
Publisher: Springer Science and Business Media LLC
Date: 02-1991
DOI: 10.1007/BF01166894
Next-generation seismic model of the Australian crust from synchronous and asynchronous ambient noise imaging
Publisher: Springer Science and Business Media LLC
Date: 02-03-2023
DOI: 10.1038/S41467-023-36514-Z
Abstract: The proliferation of seismic networks in Australia has laid the groundwork for high-resolution probing of the continental crust. Here we develop an updated 3D shear-velocity model using a large dataset containing nearly 30 years of seismic recordings from over 1600 stations. A recently-developed ambient noise imaging workflow enables improved data analysis by integrating asynchronous arrays across the continent. This model reveals fine-scale crustal structures at a lateral resolution of approximately 1-degree in most parts of the continent, highlighted by 1) shallow low velocities ( .2 km/s) well correlated with the locations of known sedimentary basins, 2) consistently faster velocities beneath discovered mineral deposits, suggesting a whole-crustal control on the mineral deposition process, and 3) distinctive crustal layering and improved characterization of depth and sharpness of the crust-mantle transition. Our model sheds light on undercover mineral exploration and inspires future multi-disciplinary studies for a more comprehensive understanding of the mineral systems in Australia.
Petrogenesis of cordierite-orthoamphibole assemblages from the Springton region, South Australia
Publisher: Springer Science and Business Media LLC
Date: 12-1990
DOI: 10.1007/BF00306411
Tectonic framework for the Cenozoic cratonic basins of Australia
Publisher: Informa UK Limited
Date: 07-2009
A study of the design of inclined wellbores with regard to both mechanical stability and fracture intersection, and its application to the Australian North West Shelf
Publisher: Elsevier BV
Date: 12-1994
Australian Proterozoic high-temperature, low-pressure metamorphism in the conductive limit
Publisher: Geological Society of London
Date: 1998
Some isostatic and thermal consequences of the vertical strain geometry in convergent orogens
Publisher: Elsevier BV
Date: 05-1990
Provenance of Late Triassic sediments in central Lhasa terrane, Tibet and its implication
Publisher: Elsevier BV
Date: 05-2014
High-T, low-P metamorphism in the Palaeoproterozoic Halls Creek Orogen, northern Australia: the middle crustal response to a mantle-related transient thermal pulse
Publisher: Wiley
Date: 02-2002
Palaeozoic Intraplate Crustal Anatexis in the Mount Painter Province, South Australia: Timing, Thermal Budgets and the Role of Crustal Heat Production
Publisher: Oxford University Press (OUP)
Date: 08-09-2006
Constraining the age of Liuqu Conglomerate, southern Tibet: Implications for evolution of the India-Asia collision zone
Publisher: Elsevier BV
Date: 09-2015
A fourier spectral method to measure the thermal diffusivity of soil
Publisher: ASTM International
Date: 10-07-2020
DOI: 10.1520/GTJ20180300
High radiogenic heat-producing granites and metamorphism-An example from the western Mount Isainlier, Australia: Reply
Publisher: Geological Society of America
Date: 2000
Cenozoic Eucla Basin and associated palaeovalleys, southern Australia — Climatic and tectonic influences on landscape evolution, sedimentation and heavy mineral accumulation
Publisher: Elsevier BV
Date: 2008
Synorogenic morphotectonic evolution of the Gangdese batholith, South Tibet: Insights from lowerature thermochronology
Publisher: American Geophysical Union (AGU)
Date: 2016
DOI: 10.1002/2015GC006047
U–Pb SHRIMP zircon geochronology and T–t–d history of the Kampa Dome, southern Tibet
Publisher: Elsevier BV
Date: 2008
Early Proterozoic metamorphism at The Granites gold mine, Northern Territory: implications for the timing of fluid production in high- temperature, low-pressure terranes
Publisher: Society of Economic Geologists
Date: 08-1993
The P–T record of synchronous magmatism, metamorphism and deformation at Petrel Cove, southern Adelaide Fold Belt
Publisher: Wiley
Date: 27-03-2002
Constraints on the current rate of deformation and surface uplift of the Australian continent from a new seismic database and low-T thermochronological data
Publisher: Informa UK Limited
Date: 03-2900
Five Years of Declining Annual Consumption of Grid-Supplied Electricity in Eastern Australia: Causes and Consequences
Publisher: Elsevier BV
Date: 08-2015
Corona textures between kyanite, garnet and gedrite in gneisses from Errabiddy, Western Australia
Publisher: Wiley
Date: 07-1987
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