RIFTING AND VOLCANISM IN THE NEW MEXICO SEGMENT OF THE BASIN AND RANGE PROVINCE, SOUTHWESTERN USA*
作者： Wolfgang E. Elston
DOI: 10.1007/978-94-009-9803-2_8
关键词: Paleontology 、 Volcanism 、 Tectonics 、 Basin and Range Province 、 Structural basin 、 Seismology 、 Geology 、 Orogeny 、 Rift 、 Volcanic arc 、 Intraplate earthquake
摘要: The Basin and Range province has been the site of extensional orogeny for past 40 m.y. Its complexities may be caused by superposition three tectonic regimes: (a) an Andean-type volcanic arc, which gradually gave way to (b) a spreading ensialic backarc basin was in turn succeeded (c) intraplate block faulting rifting. Total extension have exceeded 100 percent.
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