Tectonic subsidence, geoid analysis, and the Miocene-Pliocene unconformity in the Rio Grande rift, southwestern United States: Implications for mantle upwelling as a driving force for rift opening-Reference-Cited by-同舟云学术

Tectonic subsidence, geoid analysis, and the Miocene-Pliocene unconformity in the Rio Grande rift, southwestern United States: Implications for mantle upwelling as a driving force for rift opening

Published:2018-02-25 Issue:2 Volume:14 Page:684-709
ISSN:1553-040X
Container-title:Geosphere
language:en
Short-container-title:

Author:

van Wijk Jolante¹,Koning Daniel²,Axen Gary¹,Coblentz David³,Gragg Evan¹,Sion Brad¹

Affiliation:

1. Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, New Mexico 87801, USA

2. New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, New Mexico 87801, USA

3. Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Link

https://pubs.geoscienceworld.org/gsa/geosphere/article-pdf/14/2/684/4102034/684.pdf

Reference209 articles.

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3. 40Ar/39Ar Geochronology and Volcanic Evolution of the Taos Plateau Volcanic Field, Northern New Mexico and Southern Colorado [M.S. thesis];Appelt,1998

4. The western margin of the Rio Grande rift in northern New Mexico: An aborted boundary?;Baldridge;Geological Society of America Bulletin,1994

5. The Rio Grande rift;Baldridge,1995

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