On the causes of 18O-depletion and 18O/16O homogenization during regional metamorphism; the East Humboldt Range core complex, Nevada

A series of detailed, meter-scale traverses across various metamorphic and igneous lithologies were performed at Lizzies Basin and at the structurally higher Angel Lake locality. The studies were performed in order to more fully understand the isotopic evolution of the terrane.

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Bibliographic Details
Published inContributions to mineralogy and petrology Vol. 119; no. 1; pp. 68 - 82
Main Authors Peters, Mark T., Wickham, Stephen M.
Format Journal Article
LanguageEnglish
Published Heidelberg Springer Nature B.V 01.02.1995
Subjects
Geology
Metamorphism
Mineralogy
Minerals
Petrology
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Summary:A series of detailed, meter-scale traverses across various metamorphic and igneous lithologies were performed at Lizzies Basin and at the structurally higher Angel Lake locality. The studies were performed in order to more fully understand the isotopic evolution of the terrane.
ISSN:0010-7999
1432-0967
DOI:10.1007/BF00310718