Author: Steven Bruce Bachman
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 368
Book Description
Sedimentation and Margin Tectonics of the Coastal Belt Franciscan, Mendocino Coast, Northern California
Author: Steven Bruce Bachman
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 368
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 368
Book Description
Tectono-Magmatism, Metallogenesis, and Sedimentation at Convergent Margins
Author: Meng Wang
Publisher: Frontiers Media SA
ISBN: 2832537693
Category : Science
Languages : en
Pages : 214
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.
Publisher: Frontiers Media SA
ISBN: 2832537693
Category : Science
Languages : en
Pages : 214
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.
Tectonics and Sedimentation Along the California Margin
Northern California Coastal Processes Annotated Bibliography
Sedimentation and Tectonics in the Early Tertiary Continental Borderland of Central California
Author: Tor Helge Nilsen
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 72
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 72
Book Description
General Design Memorandum for Offshore Breakwater Harbor Entrance Protection, Noyo River and Harbor, Mendocino County, California
Trench-forearc Geology
Author: Jeremy K. Leggett
Publisher: Wiley-Blackwell
ISBN:
Category : Science
Languages : en
Pages : 606
Book Description
Publisher: Wiley-Blackwell
ISBN:
Category : Science
Languages : en
Pages : 606
Book Description
Tectonics, Sedimentation, and Evolution of the Eel River and Associated Coastal Basins of Northern California
Author: Herman Schymiczek
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 156
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 156
Book Description
Geological Survey Professional Paper
Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 48
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 48
Book Description