Refining the footwall cooling history of a rift flank uplift, Rio Grande rift, New Mexico

Author:

House M. A.,Kelley S. A.1,Roy M.2

Affiliation:

1. Department of Earth and Environmental Science; New Mexico Institute of Mining and Technology; Socorro; New Mexico; USA

2. Department of Earth and Planetary Sciences; University of New Mexico; Albuquerque; New Mexico; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference92 articles.

1. Paleogene synorogenic sedimentation in the Galisteo basin related to the Tijeras-Canoncito fault system;Abbott;Field Conf. Guideb. N. M. Geol. Soc.,1995

2. Bull. N. M. Bur. Mines Miner. Resour.;Abbott,2003

3. Thermal consequences of lithosphere extension over continental margins: The initial stretching phase;Alvarez;Geophys. J. R. Astron. Soc.,1984

4. New K-Ar dates and the late Pliocene to Holocene geomorphic history of the central Rio Grande region, New Mexico;Bachman;Geol. Soc. Am. Bull.,1978

5. A new map of the geographic extent of the Socorro mid-crustal magma body;Balch;Bull. Seismol. Soc. Am.,1997

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