Tectonic subsidence, geoid analysis, and the Miocene-Pliocene unconformity in the Rio Grande Rift, Southwestern United States; implications for mantle upwelling as a driving force for rift opening
We use tectonic subsidence patterns from wells and stratigraphic sections to describe the mid-Miocene to present tectonic subsidence history of the Rio Grande rift. Tectonic subsidence and therefore rift opening were quite fast until ca. 8 Ma, with net subsidence rates (∼25-65 mm/k.y.) comparable to...
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Published in: | Geosphere (Boulder, Colo.) Vol. 14; no. 2; pp. 684 - 709 |
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Main Authors: | , , , , , |
Format: | Journal Article Magazine Article |
Language: | English |
Published: |
United States
Geological Society of America
01-04-2018
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Subjects: | |
Online Access: | Get full text |
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