Geology of the Applebush Hill area, south Antelope Valley, Nye County, Nevada

Loading...
Thumbnail Image

Authors

Scales, Bert

Issue Date

1961

Type

Thesis

Language

en_US

Keywords

Geology , Applebush Hill , Antelope Valley , Nye County , Nevada , Geography , Stratigraphy , Cambrain , Ordovivian , Pogonip , Limestone , Quartzite , Alluvium , Volcanic , Structure , Folds , Faults , Miogeosynclinal , Mackay Theses and Dissertations Grant Collection

Research Projects

Organizational Units

Journal Issue

Alternative Title

Abstract

Lower Paleozoic rocks of an eastern miogeosynclinal assemblage have been mapped and studied in detail in the Applebush Hill area. Their stratigraphic, paleontological, and structural aspects have been correlated to the investigations of previous workers in adjacent areas. Minor treatment has been given to the volcanic rocks. The eastern assemblage is composed predominantly of clastic limestones ranging in age from Upper Cambrian to Niagaran. The volcanic rocks are probably of Early Tertiary age. Major folding is limited to Applebush Hill in the southern portion of the area. Normal faulting of considerable displacement persists throughout the area and forms two distinctive patterns.

Description

Online access for this thesis was created in part with support from the Institute of Museum and Library Services (IMLS) administered by the Nevada State Library, Archives and Public Records through the Library Services and Technology Act (LSTA). To obtain a high quality image or document please contact the DeLaMare Library at https://unr.libanswers.com/ or call: 775-784-6945.

Citation

Publisher

University of Nevada, Reno

License

In Copyright(All Rights Reserved)

Journal

Volume

Issue

PubMed ID

DOI

ISSN

EISSN