Paleomagnetism and geochronology of sills of the Doherty Mountain area, southwestern Montana: Implications for the timing of fold-and-thrust belt deformation and vertical-axis rotations along the southern margin of the Helena salient-Reference-Cited by-同舟云学术

Paleomagnetism and geochronology of sills of the Doherty Mountain area, southwestern Montana: Implications for the timing of fold-and-thrust belt deformation and vertical-axis rotations along the southern margin of the Helena salient

Published:2008-09-01 Issue:9-10 Volume:120 Page:1091-1104
ISSN:0016-7606
Container-title:Geological Society of America Bulletin
language:en
Short-container-title:Geological Society of America Bulletin

Author:

Harlan S. S.,Geissman J. Wm.,Whisner S. C.,Schmidt C. J.

Publisher

Geological Society of America

Subject

Geology

Reference36 articles.

1. Late Paleogene extensional collapse of the Cordilleran foreland fold and thrust belt

2. Solubility of the buffer assemblage pyrite + pyrrhotite + magnetite in NaCl solutions from 200 to 350°C

3. Thrust timing, growth of structural culminations, and synorogenic sedimentation in the type Sevier orogenic belt, western United States

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