1984
DOI: 10.1016/0375-6742(84)90090-6
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Geological, geochemical, stable isotope, and fluid inclusion characteristics of epithermal gold mineralization, Velvet District, Nevada

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Cited by 5 publications
(3 citation statements)
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“…Tertiary rocks that underlie the diatomite-bearing tuffaceous sedimentary rock unit (Tts) are not well exposed in the central part of the study area and were not studied. The stratigraphy and lithology of pre-diatomite, Miocene sedimentary and volcanic rocks of the Velvet area, about 3 km south of the Tunnel Hill mine, were briefly described by Masterson and Kyle (1984). The pre-diatomite rhyolite flows, tuffs, and volcaniclastic sedimentary rocks of the Velvet area (Masterson and Kyle, 1984) are lithologically similar to units in the Trinity Pass area that I interpret to be younger than diatomite.…”
Section: Comments On Geologic Unitsmentioning
confidence: 93%
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“…Tertiary rocks that underlie the diatomite-bearing tuffaceous sedimentary rock unit (Tts) are not well exposed in the central part of the study area and were not studied. The stratigraphy and lithology of pre-diatomite, Miocene sedimentary and volcanic rocks of the Velvet area, about 3 km south of the Tunnel Hill mine, were briefly described by Masterson and Kyle (1984). The pre-diatomite rhyolite flows, tuffs, and volcaniclastic sedimentary rocks of the Velvet area (Masterson and Kyle, 1984) are lithologically similar to units in the Trinity Pass area that I interpret to be younger than diatomite.…”
Section: Comments On Geologic Unitsmentioning
confidence: 93%
“…The stratigraphy and lithology of pre-diatomite, Miocene sedimentary and volcanic rocks of the Velvet area, about 3 km south of the Tunnel Hill mine, were briefly described by Masterson and Kyle (1984). The pre-diatomite rhyolite flows, tuffs, and volcaniclastic sedimentary rocks of the Velvet area (Masterson and Kyle, 1984) are lithologically similar to units in the Trinity Pass area that I interpret to be younger than diatomite. More geologic mapping and geochronologic studies are needed on to better define age relations and possible multiple cycles of rocks having similar features.…”
Section: Comments On Geologic Unitsmentioning
confidence: 93%
“…In the Trinity Mining District, brecciated quartz veins contain silver and gold in rhyolitic volcanic rocks (Lincoln, 1923;Johnson, 1977). In the Velvet Mining District, hydrothermal breccia and associated opal, chalcedony, and alunite, host gold-arsenic mineralized rocks in argillically altered Tertiary ash-flow tuff (Vanderburg, 1936a;Johnson, 1977;Masterson and Kyle, 1984). The mineralized rocks comprise veinlets, breccia fillings, and disseminations.…”
Section: Central Zone Epithermal Tractsmentioning
confidence: 99%