Author: Kenneth L. FingerPublisher:
ISBN:
Category : Foraminifera
Languages : en
Pages : 276
Book Description
Atlas of California Neogene Foraminifera
Author: Kenneth L. FingerPublisher:
ISBN:
Category : Foraminifera
Languages : en
Pages : 276
Book Description
Biostratigraphic Atlas of Miocene Foraminifera from the Monterey and Modelo Formations, Central and Southern California
Author: Kenneth L. FingerPublisher:
ISBN:
Category : Animals, Fossil
Languages : en
Pages : 184
Book Description
Neogene Planktonic Foraminifera
Author: James P. KennettPublisher:
ISBN:
Category : Science
Languages : en
Pages : 296
Book Description
U.S. Geological Survey Bulletin
Author: Special Publication - Cushman Foundation for Foraminiferal Research
Author: Post-Miocene Right Separation on the San Gabriel and Vasquez Creek Faults, with Supporting Chronostratigraphy, Western San Gabriel Mountains, California
Author: Larry A. BeyerPublisher:
ISBN:
Category : Faults (Geology)
Languages : en
Pages : 52
Book Description
The right lateral San Gabriel Fault Zone in southern California extends from the northwestern corner of the Ridge Basin southeastward to the eastern end of the San Gabriel Mountains. It bifurcates to the southeast in the northwestern San Gabriel Mountains. The northern and older branch curves eastward in the range interior. The southern younger branch, the Vasquez Creek Fault, curves southeastward to merge with the Sierra Madre Fault Zone, which separates the San Gabriel Mountains from the northern Los Angeles Basin margin. An isolated exposure of partly macrofossiliferous nearshore shallow-marine sandstone, designated the Gold Canyon beds, is part of the southwest wall of the fault zone 5.5 km northwest of the bifurcation. These beds contain multiple subordinate breccia-conglomerate lenses and are overlain unconformably by folded Pliocene-Pleistocene Saugus Formation fanglomerate. The San Gabriel Fault Zone cuts both units.
U.S. Geological Survey Professional Paper
Author: Foraminifera and their Applications
Author: Robert Wynn JonesPublisher: Cambridge University Press
ISBN: 1107036402
Category : Science
Languages : en
Pages : 407
Book Description
A one-stop practical guide to foraminifera with numerous case studies demonstrating their applications, for graduate students, micropalaeontologists and industry professionals.
Recognition of Middle Miocene Foraminifers in Highly Indurated Rocks of the Monterey Formation, Coastal Santa Maria Province, Central California
Author: Kenneth L. FingerPublisher:
ISBN:
Category : Diatoms, Fossil
Languages : en
Pages : 132
Book Description
A Manual of Practical Laboratory and Field Techniques in Palaeobiology
Author: O.R. GreenPublisher: Springer Science & Business Media
ISBN: 940170581X
Category : Science
Languages : en
Pages : 542
Book Description
The user This manual is designed for the use of geo-scientists with an interest and need in developing palaeobiological materials as a potential source of data. To meet this objective practical procedures have been formatted for use by both professional and semi professional students with an initial understanding of palaeo biological research aims as a primary source of scientific data. I have attempted to provide an explanation and understanding of practical procedures which may be required by students undertaking palaeobiological projects as part of a degree course. The layout of this manual should be particularly beneficial in the instruction and training of geotechnologists and museum preparators. Graduate students and scientists requiring an outline of a preparation procedure will also be able to use the manual as a reference from which to assess the suitability of a procedure. This manual is also intended for use by the "committed amateur". Many of the techniques described in this manual have been devised by non-palaeontologists, and developed from methods used in archaeology, zoology and botany, as well as other areas of geology. A considerable number of the methods can be undertaken by the amateur, and in the case of many of the field procedures, should be used. This will ensure that specimens and samples can be conserved in such a manner as to facilitate any later research, and not invalidate the results of subsequent geochemical analytical techniques which might be employed.