Geologic evolution of the Precambrian rocks in Northern Utah and adjacent areas

K.C. Condie*

*Corresponding author for this work

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

Surface sedimentary rocks in northern Utah and adjacent areas are unconformably underlain by granite-gneiss- migmatite complexes of Precambrian age. General review of the geologic evolution of these Precambrian terranes is given based on existing geologic and geochronologic data.

Original languageEnglish
Pages (from-to)71-95
Number of pages25
JournalUtah Geol & Mineralogical Survey-Bul 82
Publication statusPublished - May 1969
Externally publishedYes

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