Tectonic Evolution of Northern California PDF Download
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Author: M. C. Blake
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 84
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Book Description
Author: M. C. Blake
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 84
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Book Description
Author: Raymond Sullivan
Publisher: Geological Society of America
ISBN: 0813712173
Category : Science
Languages : en
Pages :
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Book Description
"Mount Diablo and the geology of the Central California Coast Ranges are the subject of a volume celebrating the Northern California Geological Society's 75th anniversary. The breadth of research illustrates the complex Mesozoic to Cenozoic tectonic evolution of the plate boundary"--
Author: Adam M. Booth
Publisher: Geological Society of America
ISBN: 0813700620
Category : Science
Languages : en
Pages :
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Book Description
Author: Kevin T. Biddle
Publisher:
ISBN:
Category : Nature
Languages : en
Pages : 346
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Book Description
Author: Douglas M. Morton
Publisher: Geological Society of America
ISBN: 0813712114
Category : Science
Languages : en
Pages : 774
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Book Description
"This book includes petrology, geochronology, and regional aspects of individual plutons, as well as evolution of the Peninsular Ranges batholith. Several chapters deal with geophysical, chemical, and isotopic based interpretations of the genesis and evolution of the batholith. An accompanying DVD contains detailed colored maps and chemical, isotopic, mineralogic, and physical properties data"--Provided by publisher.
Author: Michael J. Soreghan
Publisher: Geological Society of America
ISBN: 9780813723471
Category : Science
Languages : en
Pages : 274
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Book Description
Author: Arthur W. Snoke
Publisher: Geological Society of America
ISBN: 0813724104
Category : Science
Languages : en
Pages : 524
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Book Description
Accompanying CD-ROM includes additional images and maps.
Author: Meng Wang
Publisher: Frontiers Media SA
ISBN: 2832537693
Category : Science
Languages : en
Pages : 214
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Book Description
Convergent plate margins are important places for material and energy recycling of the Earth, in particular major sites for continental growth, reworking, and recycling. They exhibit as narrow belt structure in the rigid outer layer of the Earth, corresponding to subduction zones at lithospheric mantle depths and orogenic belts at crustal depths. The type, geometry, and thermal structure of subduction zones have critical impacts on subduction processes and nature of products, resulting in a variety of magmatic rocks and ore deposits at convergent margins. Identification and classification of the physical structure and chemical variation at convergent margins as well as confirming their correlation with specific subduction types and stages are of pivotality to understand the spatiotemporal interaction between asthenosphere and lithosphere in orogenic belts. For places where magmatic arcs get partially or entirely destroyed by surface and/or subduction erosion, adjacent sedimentary rocks are ideal geological records for paleotectonic reconstruction.
Author: Thomas H. Anderson
Publisher: Geological Society of America
ISBN: 0813725135
Category : Science
Languages : en
Pages : 629
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Book Description
"The objective of this volume is to characterize geologic relationships and settings at the margin of the Laurasia plate from Middle Jurassic to the Early Cretaceous, overlapping the time of the opening of the central Atlantic basin, with the intent of assessing the compatibility of the features with contemporaneous, sinistral fault movement"--Introduction, page v.
Author: Raymond V. Ingersoll
Publisher: Geological Society of America
ISBN: 0813725402
Category : Science
Languages : en
Pages : 768
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Book Description
Through a remarkable combination of intellect, self-confidence, engaging humility, and prodigious output of published work, William R. Dickinson influenced and challenged three generations of sedimentary geologists, igneous petrologists, tectonicists, sandstone petrologists, archaeologists, and other geoscientists. A key figure in the plate-tectonic revolution of the 1960s and 1970s, he explained how the distribution of sediments on Earth's surface could be traced to tectonic processes, and is widely recognized as a founder of modern sedimentary basin analysis. This volume consists of 31 chapters related to Dickinson's research interests; many of the authors are his former students, their students, and their students' students, demonstrating his continuing profound influence. The papers in this volume are an impressive tribute to the depth and breadth of Bill Dickinson's contributions to the geosciences.
