Author: Publisher:
ISBN:
Category : Geology
Languages : en
Pages : 576
Book Description
Geology of the Las Vegas Area, Clark County, Nevada
Author: SP007: Bibliography of Nevada geology and mineral resources through 1980, an alphabetical listing by author
Author: Publisher: NV Bureau of Mines & Geology
ISBN:
Category :
Languages : en
Pages : 188
Book Description
Bibliography of Theses in Geology, 1967-1970
Author: Dederick C. WardPublisher: Geological Society of America
ISBN: 0813721431
Category : Dissertations, Academic
Languages : en
Pages : 449
Book Description
Geological Survey Professional Paper
Author: U.S. Geological Survey Professional Paper
Author: Geological Survey Professional Paper
Author: Geological Survey (U.S.)Publisher:
ISBN:
Category :
Languages : en
Pages : 604
Book Description
The Mississippian and Pennsylvanian (Carboniferous) Systems in the United States
Author: R024: Bibliography of Nevada mining and geology, 1966-1970
Author: Publisher: NV Bureau of Mines & Geology
ISBN:
Category :
Languages : en
Pages : 66
Book Description
The Pennsylvanian-early Permian Bird Spring Carbonate Shelf, Southeastern California
Author: Calvin H. StevensPublisher: Geological Society of America
ISBN: 0813724295
Category : Science
Languages : en
Pages : 90
Book Description
"The Bird Spring Shelf in southeastern California, along with coeval turbidite basins to the west, records a complex history of Pennsylvanian and Early Permian sedimentation, sea-level changes, and deformation along this part of the western North American continental margin. In this work we describe and figure the fusulinids, including several new species, and establish detailed correlations between deposits of the shelf and the flanking basins. We then use these correlations to reconstruct the depositional history, paleogeography, and deformational history of the region. This work adds significant detail to existing interpretations of the late Paleozoic as a time of major tectonic instability on the continental margin of southeastern California as it changed from a relatively passive margin, which had persisted through most of the Paleozoic, to an active convergent margin that would characterize the Mesozoic."--Publisher's website.
Author: