T41E:
Breaking Up Is Never Easy: Why Do Some Rifts Fail and Others Succeed?
Submit an Abstract to this Session
T41E:
Breaking Up Is Never Easy: Why Do Some Rifts Fail and Others Succeed?
Breaking Up Is Never Easy: Why Do Some Rifts Fail and Others Succeed?
Session ID#: 31235
Session Description:
The breakup of continents is a fundamental process of plate tectonics. However, we have not yet identified the crucial ingredients that permit complete rupture of strong continental lithosphere. Studies of continental breakup are biased towards success stories - rifts that evolve to oceanic spreading. Some extension episodes cease before this point, presumably in the absence of some fundamental process, initial condition(s), or forcing. Investigations of “failed rifts” may help isolate key processes or conditions that enable continental breakup, particularly when compared to successful examples. Outstanding questions include: Does rift success/failure depend on intrinsic or far-field properties? How do pre-existing structure, magma, and volatiles influence rift initiation, continuation, and extinction? Are failed rifts actually “paused rifts” that can later be reactivated? Do analogous mechanical controls apply to extinct seafloor spreading centers? We solicit contributions from diverse geoscience perspectives, including geodesy, geodynamics, geochemistry/petrology, volcanology, structural geology and seismology.
Primary Convener: Zachary Eilon, University of California Santa Barbara, Department of Earth Science, Santa Barbara, United States
Conveners: Natalie J Accardo, Columbia University of New York, Palisades, NY, United States, James D Muirhead, Syracuse University, Earth Sciences, Syracuse, NY, United States and Dr. D. Sarah Stamps, PhD
Chairs: Natalie J Accardo, Pennsylvania State University, Department of Geosciences, University Park, PA, United States and Zachary Eilon, Lamont-Doherty Earth Observatory, Department of Earth Science, Santa Barbara, United States
OSPA Liaison: James D Muirhead, Syracuse University, Earth Sciences, Syracuse, NY, United States
Cross-Listed:
- DI - Study of the Earth's Deep Interior
- G - Geodesy
- S - Seismology
- V - Volcanology, Geochemistry and Petrology
Index Terms:
1209 Tectonic deformation [GEODESY AND GRAVITY]
7230 Seismicity and tectonics [SEISMOLOGY]
8109 Continental tectonics: extensional [TECTONOPHYSICS]
8178 Tectonics and magmatism [TECTONOPHYSICS]
Abstracts Submitted to this Session:
Timing of mafic magmatism VS localization of the deformation: the Ivrea Zone (Italian Alps) (269230)
See more of: Tectonophysics
