Thermochronologic data from the southern Stillwater Range, Nevada
September 25, 2020
This dataset contains apatite and zircon U-Th(He)data, 4He/3He thermochronologic data, and apatite fission-track data from the southern Stillwater Range, Nevada
Citation Information
| Publication Year | 2020 |
|---|---|
| Title | Thermochronologic data from the southern Stillwater Range, Nevada |
| DOI | 10.5066/P94QAABV |
| Authors | Samuel A Johnstone, Joseph P Colgan, David L. Shuster |
| Product Type | Data Release |
| Record Source | USGS Digital Object Identifier Catalog |
| USGS Organization | Geosciences and Environmental Change Science Center |
| Rights | This work is marked with CC0 1.0 Universal |
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Timing of Cenozoic extension in the southern Stillwater Range and Dixie Valley, Nevada
The Dixie Valley fault bounds the east side of the Stillwater Range in west‐central Nevada and last ruptured in 1954. Offset basalts indicate that slip began more recently than ~14 Ma, and prior work has interpreted the southern segment as an active low‐angle normal fault. Oligocene igneous rocks in the southern Stillwater Range were steeply tilted during large‐magnitude extension prior to ~14 Ma.
Authors
Joseph Colgan, Samuel Johnstone, David L. Shuster
Related Content
Timing of Cenozoic extension in the southern Stillwater Range and Dixie Valley, Nevada
The Dixie Valley fault bounds the east side of the Stillwater Range in west‐central Nevada and last ruptured in 1954. Offset basalts indicate that slip began more recently than ~14 Ma, and prior work has interpreted the southern segment as an active low‐angle normal fault. Oligocene igneous rocks in the southern Stillwater Range were steeply tilted during large‐magnitude extension prior to ~14 Ma.
Authors
Joseph Colgan, Samuel Johnstone, David L. Shuster