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Precambrian crustal blocks in Minnesota : neodymium isotope evidence from basement and metasedimentary rocks

Author: S R Hemming; Gilbert N Hanson; Scott M McLennan; Geological Survey (U.S.)
Publisher: [Washington, D.C.] : U.S. G.P.O. ; Denver, CO : For sale by U.S. Geological Survey, Information Services, 1995.
Series: Contributions to Precambrian geology of Lake Superior region, ch. U.; U.S. Geological Survey bulletin, 1904-U.
Edition/Format:   Print book : National government publication : EnglishView all editions and formats
Summary:
Sm-Nd survey of Precambrian granitic and metasedimentary rocks collected from several geophysically defined blocks in central Minnesota confirms the presence of some fundamental geologic boundaries previously mapped on the basis of structure. The Malmo discontinuity an Early Proterozoic structure separates the Archean Minnesota River Valley ter- ranes from an Early Proterozoic (Penokean magmatic) terrane and the  Read more...
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Additional Physical Format: Online version:
Hemming, S. R.
Precambrian crustal blocks in Minnesota
(OCoLC)937435766
Material Type: Government publication, National government publication, Internet resource
Document Type: Book, Internet Resource
All Authors / Contributors: S R Hemming; Gilbert N Hanson; Scott M McLennan; Geological Survey (U.S.)
OCLC Number: 32746723
Notes: Shipping list no.: 1996-0040-P.
Description: iii, 15 pages : illustrations, maps ; 28 cm.
Series Title: Contributions to Precambrian geology of Lake Superior region, ch. U.; U.S. Geological Survey bulletin, 1904-U.
Other Titles: Neodymium isotope evidence from basement and metasedimentary rocks
Precambrian crustal blocks in Minnesota; neodymium isotope evidence
Technical Report Archive & Image Library (TRAIL)
Responsibility: by S.R. Hemming, G.N. Hanson, and S.M. McLennan.

Abstract:

Sm-Nd survey of Precambrian granitic and metasedimentary rocks collected from several geophysically defined blocks in central Minnesota confirms the presence of some fundamental geologic boundaries previously mapped on the basis of structure. The Malmo discontinuity an Early Proterozoic structure separates the Archean Minnesota River Valley ter- ranes from an Early Proterozoic (Penokean magmatic) terrane and the McGrath Gneiss dome of east-central Minnesota North of this boundary, the Penokean fold-and-thrust belt can be divided into fault-bounded terranes that were assembled during the Penokean orogeny. Each terrane within the study area has distinct crust formation ages.

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