The geochemical results show the most anomalous part of the study area to be the White Mountain Fault zone along the northwestern range front. Silver, lead, and zinc mineralization in calcareous rocks, porphyry copper in dikes, gold-arsenic quartz vein deposits, tungsten and molybdenum tactite mineralization, and argillic alteration zones are indicated. Titanium and molybdenum were detected in Jeffery Mine Canyon, an area known for rutile deposits.
Citation Information
Publication Year | 1983 |
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Title | Map and interpretation of geochemical anomalies in the White Mountains, Blanco Mountain, Birch Creek, and Black Canyon Roadless Areas, White Mountains, California and Nevada |
DOI | 10.3133/mf1361B |
Authors | Michael F. Diggles |
Publication Type | Report |
Publication Subtype | USGS Numbered Series |
Series Title | Miscellaneous Field Studies Map |
Series Number | 1361 |
Index ID | mf1361B |
Record Source | USGS Publications Warehouse |