A5086795464- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- High-pressure geophysics and materials
- Geology and Paleoclimatology Research
- Planetary Science and Exploration
- earthquake and tectonic studies
- Astro and Planetary Science
- Geological Studies and Exploration
- Space Exploration and Technology
- Paleontology and Stratigraphy of Fossils
- Geological formations and processes
- Geomagnetism and Paleomagnetism Studies
- Hydrocarbon exploration and reservoir analysis
- Geological and Geophysical Studies
- Geological and Geophysical Studies Worldwide
- Methane Hydrates and Related Phenomena
- Space Science and Extraterrestrial Life
- Geological Formations and Processes Exploration
- Geochemistry and Elemental Analysis
- Marine and environmental studies
- Induction Heating and Inverter Technology
- Global Energy and Sustainability Research
- Pleistocene-Era Hominins and Archaeology
- Metal complexes synthesis and properties
- Linguistic research and analysis
Carleton University
2015-2024
National Research Tomsk State University
2015-2024
Yale University
2020-2023
Lund University
2023
Harvard University Press
2023
Wyoming Department of Education
2023
University of Wyoming
2023
University of Johannesburg
2021
Planetary Science Institute
2020
American Society For Engineering Education
2020
Large igneous provinces (LIPs) are high volume, short duration pulses of intraplate magmatism consisting mainly flood basalts and their associated plumbing system, but also may include silicic components carbonatites. Many LIPs have an radiating diabase dyke swarm, which typically converges on a cratonic margin, identifies mantle plume centre, is linked to breakup or attempted form that margin. We hypothesize every major margin in Canada can be with LIP, we attempt identify this LIP. To end,...
Establishing how tectonic plates have moved since deep time is essential for understanding Earth's geodynamic system has evolved and operates, thus answering longstanding questions such as what “drives” plate tectonics. Such knowledge a key component of Earth System science, implications wide ranging fields from core-mantle-crust interaction evolution, geotectonic phenomena mountain building magmatic basin histories, the episodic formation preservation resources, to global sea-level changes,...
▪ Abstract Mantle plumes are recognized by domal uplift, triple junction rifting, and especially the presence of a large igneous province (LIP), dominated in Phanerozoic flood basalts, Proterozoic exposed plumbing system dykes, sills, layered intrusions. In Archean, greenstone belts that contain komatiites have been linked to plumes. addition, some carbonatites kimberlites may originate from stalled beneath thick lithosphere. Geochemistry isotopes can be used test characterize plume origin...
▪ Abstract Earth, Venus, and Mars all exhibit populations of giant (radiating, linear, arcuate) mafic dike swarms hundreds to >2000 km in length. On Earth the dikes are exposed by erosion, while on Venus their presence is mainly inferred from associated volcanic morphology surface deformation. The apparent absence plate tectonics geologic record means that observed population remains geometrically intact, has fragmented swarms. About 30 radiating have so far been identified but with...