Many of the world's continents are bounded or traversed by vast fault networks that move laterally, like the well-known San Andreas Fault. As well as being major tectonic features of the Earth's surface, these strike-slip regimes are vitally important to the world's natural resources - petroleum, water, and geothermal energy. This book covers all aspects of these regimes; how they initiate; how they develop; and the natural resources associated with them. Numerous global case studies illustrate structural development, thermal and fluid flow implications, and commercial applicability. No other…mehr
Many of the world's continents are bounded or traversed by vast fault networks that move laterally, like the well-known San Andreas Fault. As well as being major tectonic features of the Earth's surface, these strike-slip regimes are vitally important to the world's natural resources - petroleum, water, and geothermal energy. This book covers all aspects of these regimes; how they initiate; how they develop; and the natural resources associated with them. Numerous global case studies illustrate structural development, thermal and fluid flow implications, and commercial applicability. No other book provides such a comprehensive overview of these settings, and this volume will stand as a critical reference of the state of knowledge of strike-slip terrains and transform margins. It will be invaluable for a broad range of readers, from advanced students of geology and researchers specializing in strike-slip regimes to geoscientists and managers involved in natural resources and energy solutions.
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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