A5076671459- Geological and Geochemical Analysis
- Geomagnetism and Paleomagnetism Studies
- Paleontology and Stratigraphy of Fossils
- Geology and Paleoclimatology Research
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- earthquake and tectonic studies
- Geological and Geophysical Studies
- Geological Studies and Exploration
- Geological formations and processes
- Hydrocarbon exploration and reservoir analysis
- Geochemistry and Elemental Analysis
- Geochemistry and Geochronology of Asian Mineral Deposits
- Astro and Planetary Science
- South Asian Cinema and Culture
- Evolution and Paleontology Studies
- Methane Hydrates and Related Phenomena
- Magnetic and Electromagnetic Effects
- Seismic Waves and Analysis
- Marine and environmental studies
- Earthquake Detection and Analysis
- Scientific Research and Discoveries
- Politics and Conflicts in Afghanistan, Pakistan, and Middle East
- Geotechnical and Geomechanical Engineering
- Pleistocene-Era Hominins and Archaeology
University of Florida
2016-2025
State Key Laboratory of Continental Dynamics
2024
Northwest University
2024
Planetary Science Institute
2022-2023
Russian Academy of Sciences
2014
Volcano Corporation (United States)
2004
Norwegian Geological Survey
1998-2003
Université Toulouse III - Paul Sabatier
2003
Centre National de la Recherche Scientifique
2003
Kōchi University
2003
Research Article| October 01, 1993 Paleomagnetic constraints on timing of the Neoproterozoic breakup Rodinia and Cambrian formation Gondwana C. McA. Powell; Powell 1Geology Department, University Western Australia, Nedlands, Australia 6009, Search for other works by this author on: GSW Google Scholar Z. X. Li; Li M. W. McElhinny; McElhinny J. G. Meert; Meert 2Department Geological Sciences, Michigan, Ann Arbor, Michigan 48109-1063 K. Park 3Continental Geoscience Division, Survey Canada, 601...
Abstract The Pan-African Damara orogenic system records Gondwana amalgamation involving serial suturing of the Congo–São Francisco and Río de la Plata cratons (North Gondwana) from 580 to 550 Ma, before with Kalahari–Antarctic (South as part 530 Ma Kuunga–Damara orogeny. Closure Adamastor Ocean was diachronous Araçuaí Belt southwards, peak sinistral transpressional deformation followed by craton overthrusting foreland basin development at 580–550 in Kaoko 545–530 Gariep Belt. Peak...