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Geologic and paleomagnetic studies at the Stonewall Mountain and Black Mountain volcanic centers, southern Nevada
AuthorWeiss, Steven Isaac
Geological Sciences and Engineering
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5 X 10 years. The interval between eruptions of these two ash-flow sheets is thus inferred to have been less than this, and perhaps less than 100 years, precluding a significant amount of magmatic differentiation during the repose interval.
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Subjectsubalkaline rhyolitic tuffs
Civet Cat Canyon Member
Stonewall Flat Tuff
outflow sheet tuffs
near-vent facies trachytic tuffs
Stonewall Mountain volcanic center
pre-crystallization tilt-block terrane
Black Mountain volcanic center
Thirsty Canyon Tuff
reverse polarity thermoremanent magnetization
geomagnetic field polarity transition
anomalous geomagnetic field orientation
polarity transition interval duration
peralkaline rhyolitic tuffs