Paleozoic metasediments in the northern Ruby Mountains, Nevada
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Abstract
New evidence indicates that high-grade regionally metamorphosed marble and quartzite in the northern Ruby Mountains are Paleozoic strata. Correlation is based on a match of the lithologic sequence to strata of Cambrian to Devonian age in nearby areas; particularly diagnostic is a brown dolomite at the base of the Cambrian carbonate sequence. The metamorphic complex contrasts with unmetamorphosed terranes exposed in nearby areas, and apparently formed in the Mesozoic as part of a metamorphic infrastructure.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Paleozoic metasediments in the northern Ruby Mountains, Nevada |
| Series title | GSA Bulletin |
| DOI | 10.1130/0016-7606(1971)82[259:PMITNR]2.0.CO;2 |
| Volume | 82 |
| Issue | 1 |
| Year Published | 1971 |
| Language | English |
| Publisher | Geological Society of America |
| Contributing office(s) | Geology, Minerals, Energy, and Geophysics Science Center |
| Description | 6 p. |
| First page | 259 |
| Last page | 264 |
| Country | United States |
| State | Nevada |
| Other Geospatial | Ruby Mountains |