Tectonic setting and provenance of the Neoproterozoic Uinta Mountain and Big Cottonwood groups, northern Utah: constraints from geochemistry, Nd isotopes, and detrital modes-Reference-Cited by-同舟云学术

Tectonic setting and provenance of the Neoproterozoic Uinta Mountain and Big Cottonwood groups, northern Utah: constraints from geochemistry, Nd isotopes, and detrital modes

Published:2001-06 Issue: Volume:141-142 Page:443-464
ISSN:0037-0738
Container-title:Sedimentary Geology
language:en
Short-container-title:Sedimentary Geology

Author:

Condie Kent C,Lee Dennis,Farmer G.Lang

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference48 articles.

1. Infilling history of a Neoproterozoic intracratonic basin: Nd isotope provenance studies of the Uinta Mountain Group, western United States;Ball;Precambr. Res.,1998

2. Proterozoic crustal history of the western United States as determined by neodymium isotopic mapping;Bennett;Geol. Soc. Am. Bull.,1987

3. Oldest direct evidence of lunar–solar tidal forcing encoded in sedimentary rhythmites, Proterozoic Big Cottonwood Formation, central Utah;Chan;Geology,1994

4. Another look at REE in shales;Condie;Geochim. Cosmochim. Acta,1991

5. Proterozoic terranes and continental accretion in southwestern North America;Condie,1992

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