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- W139371305 abstract "Recent studies suggest that the Rio Grande rift in southern New Mexico is a zone of very high reduced flux (greater than or equal to 1.8HFU), which contrasts strongly with lower values (1.2-1.5HFU) in adjacent portions of the Basin and Range high heat flow province. A +30 mgal Bouguer gravity anomaly also occurs in this portion of the rift, and the Bouguer gravity relief to the east and west is small. The gravity high can be explained by an upwarping of high temperature and low density upper mantle and/or shallow sills and dikes of mafic rocks in the crust in the rift. Interpreted in terms of steady heat sources, the reduced heat flow anomaly implies massive amounts of melting in the lower crust. Transient heat flow interpretations imply less crustal anatexis than do steady-state models of the thermal anomaly. The transient models also refine interpretations from gravity by requiring that the combined heat flow and gravity highs be explained by high temperature and low density masses in the upper mantle. Related discussion focuses on the relations between geophysical interpretations and the late Cenozoic volcanism and regional geology in the rift." @default.
- W139371305 created "2016-06-24" @default.
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- W139371305 date "1977-01-01" @default.
- W139371305 modified "2023-09-24" @default.
- W139371305 title "Review of the significance of geothermal and gravity studies in the southern Rio Grande rift (Abstract)" @default.
- W139371305 hasPublicationYear "1977" @default.
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