Lineaments and faults in Quaternary and late Tertiary deposits in the southern part of the Walker Lane are potentially active and form patterns that are anomalous with respect to the typical fault patterns in most of the Great Basin. Little work has been done to identify and characterize these faults, with the exception of those in the Death Valley-Furnace Creek (DVFCFZ) fault system and those in and near the Nevada Test Site. Four maps at a scale of 1:100,000 summarize the existing knowledge about these lineaments and faults based on extensive aerial-photo interpretation, limited field investigations, and published geologic maps. The lineaments and faults in all four maps can be divided geographically into two groups. The first group inclu...
Evaluation of surface faulting that may pose a hazard to prospective surface facilities is an import...
The Mine Mountain area is a small range of hills on the west side of the central Yucca Flat basin on...
The French Peak accommodation zone (FPAZ) forms an east-trending bedrock structural high in the Neva...
Faults and fault-related lineaments in Quaternary and late Tertiary deposits in the southern part of...
Southern Nevada is geologically and structurally complex. Detailed geologic mapping is critical to t...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...
Detailed mapping and structural analysis of upper Proterozoic and Paleozoic rocks in the CP Hills of...
Major strike-slip faults are common structural features in the late-Cenozoic tectonic framework of t...
The 76-km-long Black Mountains fault zone (BMFZ)bounds the western margin of the Black Mountains int...
Most of the rocks in the Stone Cabin Fault Zone in the Horse Range, Nevada are folded, faulted, and ...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...
New geologic map, tectonic, geomorphologic, and terrestrial cosmogenic nuclide (TCN) geochronologic ...
The Rock Valley fault system trends northeasterly through the southeast corner of the Nevada Test Si...
The author has identified the following significant results. Geologic reconnaissance guided by analy...
Evaluation of surface faulting that may pose a hazard to prospective surface facilities is an import...
The Mine Mountain area is a small range of hills on the west side of the central Yucca Flat basin on...
The French Peak accommodation zone (FPAZ) forms an east-trending bedrock structural high in the Neva...
Faults and fault-related lineaments in Quaternary and late Tertiary deposits in the southern part of...
Southern Nevada is geologically and structurally complex. Detailed geologic mapping is critical to t...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...
Detailed mapping and structural analysis of upper Proterozoic and Paleozoic rocks in the CP Hills of...
Major strike-slip faults are common structural features in the late-Cenozoic tectonic framework of t...
The 76-km-long Black Mountains fault zone (BMFZ)bounds the western margin of the Black Mountains int...
Most of the rocks in the Stone Cabin Fault Zone in the Horse Range, Nevada are folded, faulted, and ...
Online access for this thesis was created in part with support from the Institute of Museum and Libr...
This paper describes the geology of an area six miles wide and 67 miles long, extending from the cre...
New geologic map, tectonic, geomorphologic, and terrestrial cosmogenic nuclide (TCN) geochronologic ...
The Rock Valley fault system trends northeasterly through the southeast corner of the Nevada Test Si...
The author has identified the following significant results. Geologic reconnaissance guided by analy...
Evaluation of surface faulting that may pose a hazard to prospective surface facilities is an import...
The Mine Mountain area is a small range of hills on the west side of the central Yucca Flat basin on...
The French Peak accommodation zone (FPAZ) forms an east-trending bedrock structural high in the Neva...