Middle Miocene to Holocene tectonics, basin evolution, and paleogeography along the southern margin of the Snake River Plain in the Knoll Mountain–Ruby–East Humboldt Range region, northeastern Nevada and south-central Idaho-Reference-Cited by-同舟云学术

Middle Miocene to Holocene tectonics, basin evolution, and paleogeography along the southern margin of the Snake River Plain in the Knoll Mountain–Ruby–East Humboldt Range region, northeastern Nevada and south-central Idaho

Published:2017-09-25 Issue:6 Volume:13 Page:1901-1948
ISSN:1553-040X
Container-title:Geosphere
language:en
Short-container-title:

Author:

Camilleri Phyllis,Deibert Jack,Perkins Michael

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Link

http://pubs.geoscienceworld.org/geosphere/gsa/geosphere/article-pdf/13/6/1901/3994098/1901.pdf

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4. Miocene to Holocene landscape evolution of the western Snake River Plain region, Idaho: Using the SHRIMP detrital zircon provenance record to track eastward migration of the Yellowstone hotspot;Geological Society of America Bulletin,2006

5. Voluminous low δ18O magmas in the late Miocene Heise volcanic field, Idaho: Implications for the fate of Yellowstone hotspot calderas;Geology,2007

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