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Rapid Eocene extension in the Robinson district, White Pine County, Nevada; constraints from super 40 Ar/ super 39 Ar dating.

Gans, Phillip B; Seedorff, Eric; Fahey, Patrick L; Hasler, Richard W; Maher, David J; Jeanne, Richard A; Shaver, Stephen A (2001) Rapid Eocene extension in the Robinson district, White Pine County, Nevada; constraints from super 40 Ar/ super 39 Ar dating. Geology Boulder. 29; 6, Pages 475-478. 2001.

AuthorsGans, Phillip B; Seedorff, Eric; Fahey, Patrick L; Hasler, Richard W; Maher, David J; Jeanne, Richard A; Shaver, Stephen A
Year2001
TitleRapid Eocene extension in the Robinson district, White Pine County, Nevada; constraints from super 40 Ar/ super 39 Ar dating.
SourceGeology Boulder. 29; 6, Pages 475-478. 2001.
PublisherGeological Society of America GSA. Boulder, CO, United States. 2001.
Document typeSerial
ISSN0091-7613
GeoRef2001-043113
Keywordsabsolute-age; accommodation-zones; Ar-Ar; Basin-and-Range-Province; Cenozoic-; dates-; emplacement-; Eocene-; extension-; igneous-rocks; Nevada-; North-America; Paleogene-; rates-; rhyolites-; Robinson-mining-district; tectonics-; Tertiary-; tilt-; United-States; volcanic-rocks; White-Pine-County-Nevada
DOI10.1130/0091-7613(2001)029<0475:REEITR>2.0.CO;2

Abstract

Precise super 40 Ar/ super 39 Ar ages on pretectonic, syntectonic, and posttectonic rhyolites from the Robinson mining district, which is within a highly extended domain in east-central Nevada, indicate that extreme extension approximately 400% occurred in fewer than 900 k.y. during the Eocene. The duration of extension is tightly delimited by an Eocene lacustrine unit that was horizontal prior to extension and by younger rhyolitic units. The rhyolites represent at least five eruptive episodes, including the preextensional and synextensional rhyolite of White Hill emplaced between 37.6 and 37.4 Ma, and the postextensional rhyolite of Garnet Hill emplaced at 36.7 Ma, although some of it is perhaps as old as 37.1 Ma. Thus, the duration of extreme extension at Robinson was between 0.9 and 0.3 m.y., comparable to or shorter than other highly extended areas in western North America. The extensional domain in east-central Nevada is a composite feature, produced by localized, episodic, rapid extension that began in early Eocene time and continued to at least middle Miocene time.

13 samples from this reference

SampleRock nameMajorTraceIsotope
Ar2Rhyolite
Ar3Rhyolite
Ar4Rhyolite
Ar5Rhyolite
Ar5Rhyolite
Ar6Rhyolite
Ar7Rhyolite
Ar8Rhyolite
Ar8Rhyolite
Ar8Rhyolite
Ar8Rhyolite
Ar9Rhyolite
Lot1127Rhyolite