A5004188350- Geological and Geochemical Analysis
- earthquake and tectonic studies
- Geochemistry and Geologic Mapping
- High-pressure geophysics and materials
- Paleontology and Stratigraphy of Fossils
- Geological and Geophysical Studies
- Geology and Paleoclimatology Research
- Geological formations and processes
- Geochemistry and Elemental Analysis
- Geomagnetism and Paleomagnetism Studies
- Geological Studies and Exploration
- Astro and Planetary Science
- Hydrocarbon exploration and reservoir analysis
- Mineralogy and Gemology Studies
- Geological and Geophysical Studies Worldwide
- Radioactive element chemistry and processing
- Clay minerals and soil interactions
- Planetary Science and Exploration
- Marine animal studies overview
- Geological Modeling and Analysis
- Paleontology and Evolutionary Biology
- Geological Formations and Processes Exploration
- Maritime and Coastal Archaeology
- Isotope Analysis in Ecology
- Pleistocene-Era Hominins and Archaeology
The University of Adelaide
2014-2023
University of Aberdeen
2016
Utrecht University
2002
The Antarctic Ross and the Australian Delamerian orogenies are consequence of stress transfer to outboard trailing edge newly assembled Gondwana supercontinent. This tectonic reorganization occurred in Early Middle Cambrian on completion Pan‐African deformation subduction along sutures between eastern western Gondwanan continental fragments. Before this, Neoproterozoic rocks Australia were formed a passive margin record dispersion Rodinia with consequent opening proto‐Pacific. Our new U‐Pb...
Research Article| October 01, 1992 Some geodynamic and compositional constraints on "postorogenic" magmatism Simon Turner; Turner 1Department of Geology Geophysics, University Adelaide, GPO Box 498, Adelaide 5001, Australia Search for other works by this author on: GSW Google Scholar Mike Sandiford; Sandiford John Foden Author Article Information Publisher: Geological Society America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print 0091-7613 (1992) 20 (10): 931–934....
Research Article| May 01, 2014 Detrital zircons in basement metasedimentary protoliths unveil the origins of southern India Diana Plavsa; Plavsa † 1Tectonics, Resources and Exploration (TRaX), School Earth Environmental Sciences, University Adelaide, SA 5005, Australia †E-mail: diana.plavsa@adelaide.edu.au. Search for other works by this author on: GSW Google Scholar Alan S. Collins; Collins Justin L. Payne; Payne John D. Foden; Foden Chris Clark; Clark 2The Institute Geoscience (TIGeR),...
Tectonic models for the latest Paleoproterozoic to earliest Mesoproterozoic evolution of eastern Australia (circa 1620–1500 Ma) are diverse and either emphasize plume or plate margin activity, neither which satisfactorily explains all geological observations. The dichotomy is largely attributed geochemical, spatial temporal data that suggest voluminous A‐type felsic magmas related, whereas distribution arc‐related intense orogenic overprint activity. salient events include magmatism at circa...
Abstract Gondwana amalgamated along a suite of Himalayan‐scale collisional orogens, the roots which lace continents Africa, South America, and Antarctica. The Southern Granulite Terrane India is generally well‐exposed, exhumed, Gondwana‐forming orogen that preserves record tectonic evolution eastern margin East African Orogen during Ediacaran‐Cambrian (circa 600–500 Ma) as central formed. deformation associated with closure Mozambique Ocean collision Indian African/Madagascan cratonic...