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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Bibliographic Details
Published in:Geosphere (Boulder, Colo.) Vol. 14; no. 2; pp. 684 - 709
Main Authors: van Wijk, Jolante, Koning, Daniel, Axen, Gary J, Coblentz, David, Gragg, Evan, Sion, Brad
Format: Journal Article Magazine Article
Language:English
Published: United States Geological Society of America 01-04-2018
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