Progressive opening of the northern Rio Grande rift based on fault structure and kinematics of the Tusas-Abiquiu segment in north-central New Mexico, U.S.

Author:

Liu Yiduo A.,Murphy Michael A.,van Wijk Jolante,Koning Daniel J.,Smith Tyson,Andrea Ross A.

Funder

AAPG Foundation

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference162 articles.

1. Recent mapping of the Oligo-Miocene Los Pinos Formation and associated units in the Tusas Mountains, New Mexico;Aby,2011

2. Geologic map of the El Vado 7.5-minute quadrangle, Rio Arriba County, New Mexico;Aby,2016

3. Evolution, pattern, and partitioning of deformation during oblique continental rifting: Inferences from lithospheric-scale centrifuge models;Agostini;Geochem. Geophys. Geosyst.,2009

4. Fault architecture in the Main Ethiopian Rift and comparison with experimental models: implications for rift evolution and Nubia–Somalia kinematics;Agostini;Earth Planet. Sci. Lett.,2011

5. Stress history and tectonic development of the Rio Grande rift, New Mexico;Aldrich;J. Geophys. Res. Solid Earth,1986

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