Geology of the Point Sur-Lopez Point region, Coast Ranges, California: A part of the Southern California allochthon PDF Download
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Author: Clarence A. Hall, Jr.
Publisher: Geological Society of America
ISBN: 0813722667
Category : Science
Languages : en
Pages : 41
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Book Description
Author: Clarence A. Hall, Jr.
Publisher: Geological Society of America
ISBN: 0813722667
Category : Science
Languages : en
Pages : 41
Get Book
Book Description
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 224
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Book Description
Author: John C. Crowell
Publisher: Geological Society of America
ISBN: 9780813723679
Category : Science
Languages : en
Pages : 276
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Book Description
Author:
Publisher:
ISBN:
Category : Fish populations
Languages : en
Pages : 336
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Book Description
Author: Christopher C. Sorlien
Publisher:
ISBN:
Category : Basins (Geology)
Languages : en
Pages : 74
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Book Description
Author: Po Chen
Publisher: Springer
ISBN: 3319166042
Category : Science
Languages : en
Pages : 513
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Book Description
This book introduces a methodology for solving the seismic inverse problem using purely numerical solutions built on 3D wave equations and which is free of the approximations or simplifications that are common in classical seismic inversion methodologies and therefore applicable to arbitrary 3D geological media and seismic source models. Source codes provided allow readers to experiment with the calculations demonstrated and also explore their own applications.
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Category : Botany
Languages : en
Pages : 228
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Book Description
Author: William R. Dickinson
Publisher: Geological Society of America
ISBN: 0813723051
Category : Science
Languages : en
Pages : 53
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Book Description
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: Clarence A. Hall
Publisher: Geological Society of America
ISBN: 9780813723570
Category : Science
Languages : en
Pages : 502
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Book Description
Approximately 3000 middle and late Cenozoic nearshore marine molluscan taxa from western California are assigned to six time periods, spanning ~25 m.y. In this interdisciplinary study, western California is palinspastically restored for each of the time periods by backsliding and back-rotating large fault blocks or crustal units. Marine fossil assemblages are assigned to nearshore paleoclimatic regions or water masses within palinspastically restored California. In addition, this volume reveals positive feedback mechanisms between paleolatitudinal changes in sea-surface paleotemperature gradients and changes in the diversity of marine mollusks along the California coast through time; defines "equable" based effective temperatures; and analyzes extinction rates among macroinvertebrate marine taxa from coastal California and the possible causes of these extinctions. The late Paleogene to Neogene faunas reflect an increase in faunal diversity related to strengthened temperature gradients, greater extremes in sea-surface temperatures, reduction in temperateness, and the development of an embayed California coastline.
