Author: Win Swe
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 192
Book Description
Stratigraphy and Structure of Late Mesozoic Rocks South and Southeast of Clear Lake, California
Journal of Research of the U.S. Geological Survey
Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 872
Book Description
Scientific notes and summaries of investigations in geology, hydrology, and related fields.
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 872
Book Description
Scientific notes and summaries of investigations in geology, hydrology, and related fields.
Stratigraphy of Paleozoic and Lower Mesozoic Rocks in the Northern Sierra Terrane, California
Author: David S. Harwood
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 90
Book Description
Revised stratigraphic and structural interpretations of predominantly volcanic and basinal rocks; catalog of 118 old and new fossil localities.
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 90
Book Description
Revised stratigraphic and structural interpretations of predominantly volcanic and basinal rocks; catalog of 118 old and new fossil localities.
Geological Survey Bulletin
Abstracts for 1968: Abstracts of papers submitted for seven meetings with which the Society was associated
Author: Geological Society of America
Publisher: Geological Society of America
ISBN: 0813721210
Category : Geology
Languages : en
Pages : 733
Book Description
Publisher: Geological Society of America
ISBN: 0813721210
Category : Geology
Languages : en
Pages : 733
Book Description
Tectonic Setting and Lithology of the Winterhaven Formation
Author: Gordon Haxel
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 28
Book Description
Analyzes the lithology of a sequence of supercrustal rocks in southeaternmost California and southwesternmost Arizona known as the Winterhaven Formation, presenting data on its geologic setting, stratigraphy, metamorphism and deformation, basil contact, and age; and providing conclusions concerning its tectonic significance.
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 28
Book Description
Analyzes the lithology of a sequence of supercrustal rocks in southeaternmost California and southwesternmost Arizona known as the Winterhaven Formation, presenting data on its geologic setting, stratigraphy, metamorphism and deformation, basil contact, and age; and providing conclusions concerning its tectonic significance.
Stratigraphy and Structure of Mesozoic and Cenozoic Rocks, Nipomo Quadrangle, Southern Coast Ranges, California
Author: Clarence A. Hall
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 24
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 24
Book Description
Bibliography of Theses in Geology, 1967-1970
Author: Dederick C. Ward
Publisher: Geological Society of America
ISBN: 0813721431
Category : Dissertations, Academic
Languages : en
Pages : 449
Book Description
Publisher: Geological Society of America
ISBN: 0813721431
Category : Dissertations, Academic
Languages : en
Pages : 449
Book Description
Special Papers
Stratigraphy and Structure of the Late Precambrian - Early Cambrian Clastic Metasedimentary Rocks of the Baldwin Lake Area, San Bernardino Mountains, California
Author: David Lynn Tyler
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 6
Book Description
The San Bernardino Mountains are the easternmost range of the Transverse Ranges of southern California, Precambrian crystalline rocks, and Late Precambrian and Paleozoic metasedimentary rocks are exposed in several roof pendants in the Mesozoic plutonic rocks which comprise the bulk of the range. The Late Precambrian - Early Cambrian clastic shelf sequence in chronologic order includes 1) the white quartzite of the Stirling Quartzite Equivalent; 2) the gray quartzite and phyllite of the Wood Canyon Formation; 3) the vitreous white Zabriskie Quartzite; and 4) carbonate ahd schist of the Carrara Formation. These rocks probably constitute a part of the initial deposits along the eastern margin of the Cordilleran miogeosyncline. Middle Cambrian to Permian shelf carbonates overlay the clastic sequence. The Precambrian crystalline rocks and the sedimentary rocks were deformed and metamorphosed to upper greenschist (biotite) grade, probably in Late Masozoic time. The rocks are folded into a northeast-vergent overturned anticline which is overridden by a somewhat later thrust of similar vergenz. Dominantly post-tectonic acid and intermediate plutons of the Mesozoic Sierran magmatic arc intrude the metamorphic rocks. Right-lateral strike-slip faults and gravity slides of Cenozoic age modify the Mesozoic structure. These features are related to the final uplift of the San Bernardino Mountains.
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 6
Book Description
The San Bernardino Mountains are the easternmost range of the Transverse Ranges of southern California, Precambrian crystalline rocks, and Late Precambrian and Paleozoic metasedimentary rocks are exposed in several roof pendants in the Mesozoic plutonic rocks which comprise the bulk of the range. The Late Precambrian - Early Cambrian clastic shelf sequence in chronologic order includes 1) the white quartzite of the Stirling Quartzite Equivalent; 2) the gray quartzite and phyllite of the Wood Canyon Formation; 3) the vitreous white Zabriskie Quartzite; and 4) carbonate ahd schist of the Carrara Formation. These rocks probably constitute a part of the initial deposits along the eastern margin of the Cordilleran miogeosyncline. Middle Cambrian to Permian shelf carbonates overlay the clastic sequence. The Precambrian crystalline rocks and the sedimentary rocks were deformed and metamorphosed to upper greenschist (biotite) grade, probably in Late Masozoic time. The rocks are folded into a northeast-vergent overturned anticline which is overridden by a somewhat later thrust of similar vergenz. Dominantly post-tectonic acid and intermediate plutons of the Mesozoic Sierran magmatic arc intrude the metamorphic rocks. Right-lateral strike-slip faults and gravity slides of Cenozoic age modify the Mesozoic structure. These features are related to the final uplift of the San Bernardino Mountains.