Stratigraphy, Diagenesis, and Structural Deformation of the Monterey Formation, Central California Coast

Stratigraphy, Diagenesis, and Structural Deformation of the Monterey Formation, Central California Coast
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Total Pages : 0
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ISBN-10 : 1565763580
ISBN-13 : 9781565763586
Rating : 4/5 (586 Downloads)

Book Synopsis Stratigraphy, Diagenesis, and Structural Deformation of the Monterey Formation, Central California Coast by : Richard J. Behl

Download or read book Stratigraphy, Diagenesis, and Structural Deformation of the Monterey Formation, Central California Coast written by Richard J. Behl and published by . This book was released on 2018 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: This field trip guidebook uses the Miocene Monterey Formation as a natural laboratory to understand the origin, distribution and physical properties of biogenic, siliceous and organic-rich mudrocks deposited from clastic-starved, upwelling systems above marginal marine basins. Based on a successful week-long, professional short-course led for many years by the authors, the guidebook teaches how to distinguish types of siliceous, calcareous/dolomitic, phosphatic and organic-rich rocks and to understand relationships between depositional environment, sediment and rock composition, diagenetic evolution, and bedding style or stacking patterns. Knowledge of the chemical and mineralogic character and the physical properties of these rocks is then applied to understand variations in mechanical stratigraphy and fracture architecture that can enhance prediction of petroleum reservoir properties.The field guide takes the user to spectacular, classic outcrops of different facies of the Miocene Monterey Formation exposed along the coast of southern and central California. The great heterogeneity of the Monterey Formation permits investigation of siliceous, calcareous, phosphatic and carbonaceous mudrocks and their different properties and deformational behavior that can be applied to other mudstones around the world. Their occurrence within a complex and varied tectonically active setting provides exposures that presenting different aspects, perspectives and styles of deformation from extension to compression to strike-slip faulting, with bedding-scale to formational-scale expressions.


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