"Many continents are bounded or traversed by vast fault networks that move laterally. As well as being major tectonic features, these strike-slip regimes are vital for the world's natural resources - petroleum, water, and geothermal energy. This volume provides a comprehensive overview and critical reference of these settings"--
"Many continents are bounded or traversed by vast fault networks that move laterally. As well as being major tectonic features, these strike-slip regimes are vital for the world's natural resources - petroleum, water, and geothermal energy. This volume provides a comprehensive overview and critical reference of these settings"--Hinweis: Dieser Artikel kann nur an eine deutsche Lieferadresse ausgeliefert werden.
Michal Nem¿ok was a research professor at the Energy and Geoscience Institute of the University of Utah, USA for twenty-two years, until 2022. Now he runs his own company, RM Geology, and has a part-time position in the Faculty of Mining and Geology at the Technical University Ostrava, Czech Republic. He is the co-author of Thrustbelts: Structural Architecture, Thermal Regimes and Petroleum Systems (2005, Cambridge University Press) and author of Rifts and Passive Margins: Structural Architecture, Thermal Regimes, and Petroleum Systems (2016, Cambridge University Press).
Inhaltsangabe
Introduction 1. Basic description of structural architecture in transform margin settings 2. Mechanics of strike-slip faulting and transition to drift phases 3. Determination of continental, proto-oceanic and oceanic crustal boundaries 4. Determination of timing of strike-slip events and continental breakup along transforms 5. Role of lithospheric composition and compositional variations in evolving structural styles 6. Role of pre-existing anisotropy in evolving strike-slip structural styles 7. Role of syn-tectonic deposition and erosion in evolving structural styles 8. Fluid flow systems and magmatism 9. Role of pre-tectonic heat flow in thermal regimes 10. Role of stratigraphic and structural architecture in thermal regimes 11. Role of syn-tectonic deposition and erosion in thermal regimes 12. The role of deformation on thermal regimes of transform margins 13. Role of fluid flow on thermal regime 14. Models of source rock distribution, maturation and expulsion 15. Models of reservoir quality distribution 16. Sealing characteristics 17. Models of hydrocarbon migration 18. Trapping styles References Index.
Introduction 1. Basic description of structural architecture in transform margin settings 2. Mechanics of strike-slip faulting and transition to drift phases 3. Determination of continental, proto-oceanic and oceanic crustal boundaries 4. Determination of timing of strike-slip events and continental breakup along transforms 5. Role of lithospheric composition and compositional variations in evolving structural styles 6. Role of pre-existing anisotropy in evolving strike-slip structural styles 7. Role of syn-tectonic deposition and erosion in evolving structural styles 8. Fluid flow systems and magmatism 9. Role of pre-tectonic heat flow in thermal regimes 10. Role of stratigraphic and structural architecture in thermal regimes 11. Role of syn-tectonic deposition and erosion in thermal regimes 12. The role of deformation on thermal regimes of transform margins 13. Role of fluid flow on thermal regime 14. Models of source rock distribution, maturation and expulsion 15. Models of reservoir quality distribution 16. Sealing characteristics 17. Models of hydrocarbon migration 18. Trapping styles References Index.
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