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TECTONICALLY CONTROLLED, TIME-PREDICTABLE BASALTIC VOLCANISM FROM ALITHOSPHERIC MANTLE SOURCE (CENTRAL BASIN AND RANGE PROVINCE, USA) (2007)

This paper summarizes physical volcanological, geochemical, and time-volume characteristics of the Plio-Pleistocene part of the Southwestern Nevada Volcanic Field (SNVF) as an example of an extremely low volume-flux end member of basaltic fields.
Reference:
Earth and Planetary Science Letters 261 (2007) 201-216
Organization:
Earth and Environmental Sciences Division, Los Alamos National Laboratory
USA, Nevada
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