Author: Orville Lee Bandy
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 0
Book Description
Radiometric Dating and Paleontologic Zonation
Author: Orville Lee Bandy
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 0
Book Description
Publisher:
ISBN:
Category : Geology, Stratigraphic
Languages : en
Pages : 0
Book Description
Radiometric Dating and Paleontologic Zonation
Author: Orville L. Bandy
Publisher: Geological Society of America
ISBN: 0813721245
Category : Science
Languages : en
Pages : 255
Book Description
Publisher: Geological Society of America
ISBN: 0813721245
Category : Science
Languages : en
Pages : 255
Book Description
Geophysical Abstracts ...
Author:
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 876
Book Description
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 876
Book Description
Abstracts of North American Geology
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1128
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 1128
Book Description
Geophysical Abstracts
Author: Geological Survey (U.S.)
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 890
Book Description
Publisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 890
Book Description
U.S. Geological Survey Bulletin
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 278
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 278
Book Description
Conglomerates of the Upper Middle Eocene to Lower Miocene Sespe Formation Along the Santa Ynez Fault
Author: Jeffrey L. Howard
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 64
Book Description
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 64
Book Description
U.S. Geological Survey Bulletin
Author: Colin F. Williams
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 214
Book Description
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.
Publisher:
ISBN:
Category : Argillite
Languages : en
Pages : 214
Book Description
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.
Miocene Extension and Post-Miocene Transpression Offshore of South-central California
Author: Christopher C. Sorlien
Publisher:
ISBN:
Category : Basins (Geology)
Languages : en
Pages : 74
Book Description
Publisher:
ISBN:
Category : Basins (Geology)
Languages : en
Pages : 74
Book Description
U.S. Geological Survey Professional Paper
Author:
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 64
Book Description
Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 64
Book Description