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Tectonic and magmatic controls on the metal composition of some cenozoic hydrothermal systems of the northwestern US

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5164004
 [1]
  1. Univ. of Oregon, Eugene, OR (United States). Dept. of Geological Sciences
Many Cenozoic, Au-Ag-rich, hydrothermal systems in the northwestern US have formed in two distinct magmatic and tectonic environments: (1) andesitic volcanic piles'' or arcs yield intrusion-related, porphyry-style Cu-Mo-B mineralization and acid-sulfate, advanced argillic alteration; base-metal rich (Pb-Zn-Ag-Ba-Au-Mn), adularia-sericite, epithermal veins form in the peripheral propylitically-altered areas; and (2) Au-Se-Sb-As[+-]Ag-rich, Pb-Zn-Ba-Mn poor, adularia-sericite epithermal deposits in rhyolitic (commonly ash-flow tuffs), andesitic, and locally bimodal volcanic terrains undergoing significant extension or transtension. Porphyry Cu-Mo mineralization, acid-sulfate/advanced-argillic alteration, and base-metal rich veins are apparently absent in the second/environment, possibly owing in part to smaller amounts of magmatic volatiles entering the hydrothermal system. Examples of type 1 are the Miocene Cascades in WA and OR (e.g., Bohemia district) and the Miocene Virginia Range in NW Nevada (Washington Hill and Comstock districts). Examples of type 2 are the deposits at Republic and Wenatchee, WA, which formed during extension in the Eocene; DeLamar, ID and Sleeper, NV, which formed during the onset of rapid Basin and Range extension following Mid Miocene flood-basalt activity; and Wind Mtn., Sulfur, Florida Canyon, and possibly Rosebud, NV.
OSTI ID:
5164004
Report Number(s):
CONF-9305259--
Conference Information:
Journal Name: Geological Society of America, Abstracts with Programs; (United States) Journal Volume: 25:5
Country of Publication:
United States
Language:
English