Petrogenesis of late Cenozoic volcanic rocks from the Raton-Clayton volcanic field, northeastern New Mexico and southeastern Colorado
Late Cenozoic volcanism on the Great Plains in northeastern New Mexico was closely related to the tectonic and thermal deformation along the transitional zone between the Colorado Plateau and southern Basin and Range province, which produced a broadly synchronous volcanism along the Jemez lineament....
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Format: | Others |
Language: | English |
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2009
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Online Access: | http://hdl.handle.net/1911/16904 |