Geology of the Central Part of the Fillmore Quadrangle, Ventura County, California

Geology of the Central Part of the Fillmore Quadrangle, Ventura County, California PDF Author: American Association of Petroleum Geologists. Pacific Section
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 152

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Geological Survey Professional Paper

Geological Survey Professional Paper PDF Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 210

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Geological Survey Professional Paper

Geological Survey Professional Paper PDF Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category :
Languages : en
Pages : 494

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U.S. Geological Survey Professional Paper

U.S. Geological Survey Professional Paper PDF Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 864

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U.S. Geological Survey Bulletin

U.S. Geological Survey Bulletin PDF Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 278

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Geology and Mineral Resources Study of Southern Ventura County, California

Geology and Mineral Resources Study of Southern Ventura County, California PDF Author: California. Division of Mines and Geology
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 120

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Open-file Report

Open-file Report PDF Author:
Publisher:
ISBN:
Category : Geological surveys
Languages : en
Pages : 128

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U.S. Geological Survey Bulletin

U.S. Geological Survey Bulletin PDF Author: Colin F. Williams
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 214

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Phosphatic concretions occur within diatomite in the upper part of the Miocene Monterey Formation near Lompoc, Calif. Absence of disruption of fine laminar bedding in the associated sediment by the concretions shows that they formed after complete compaction of the enclosing sediment.The concretions exhibit a strongly concentric color, chemical, and mineralogic zonation. Many of them are composed of a nucleus in which vivianite is the dominant mineral. Amorphous ferric phosphate, mitridatite, and francolite are the dominant phosphatic phases in successive layers toward the surface of the concretions. Cd and As contents increase tenfold from the nucleus outward, reaching a maximum of 2,000 ppm, whereas Ni content, with a maximum of 720 ppm, and Co content show the opposite trend. This mineralogy and elemental composition favor accretion under conditions of continuously increasing Eh and pH, during uplift into the fresh-ground-water zone of the terrestrial environment. Shale-normalized rare-earth-element patterns, however, suggest a marine source for the elements biogenic debris consisting of opal-A, organic matter, and carbonates of the enclosing sediment.

Conglomerates of the Upper Middle Eocene to Lower Miocene Sespe Formation Along the Santa Ynez Fault

Conglomerates of the Upper Middle Eocene to Lower Miocene Sespe Formation Along the Santa Ynez Fault PDF Author: Jeffrey L. Howard
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 64

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Sedimentation and Tectonics in the Early Tertiary Continental Borderland of Central California

Sedimentation and Tectonics in the Early Tertiary Continental Borderland of Central California PDF Author: Tor Helge Nilsen
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 72

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