Pliocene–Holocene deformation in the southern Rio Grande rift as inferred from topography and uplifted terraces of the Franklin Mountains, southern New Mexico and western Texas-Reference-Cited by-同舟云学术

Pliocene–Holocene deformation in the southern Rio Grande rift as inferred from topography and uplifted terraces of the Franklin Mountains, southern New Mexico and western Texas

Published:2018-05-17 Issue:4 Volume:14 Page:1677-1689
ISSN:1553-040X
Container-title:Geosphere
language:en
Short-container-title:

Author:

Armour L.K.¹,Langford Richard P.¹,Ricketts Jason W.¹

Affiliation:

1. Department of Geological Sciences, The University of Texas at El Paso, 500 West University Avenue, El Paso, Texas 79968, USA

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Link

https://pubs.geoscienceworld.org/gsa/geosphere/article-pdf/14/4/1677/4265540/1677.pdf

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3. Using geophysical techniques to trace active faults in the urbanized northern Hueco Bolson, West Texas, USA, and northern Chihuahua, Mexico;Avila,2015

4. Displacement geometry in the volume containing a single normal fault;Barnett;Bulletin of the American Association of Petroleum Geologists,1987

5. Distributed deformation across the Rio Grande rift, Great Plains, and Colorado Plateau;Berglund;Geology,2012

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