Rheologic evolution of low-grade metasedimentary rocks and granite across a large strike-slip fault zone: A case study of the Kellyland fault zone, Maine, USA
Author:
Funder
Colby College Division of Natural Sciences
Publisher
Elsevier BV
Subject
Geology
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1. Superplastic deformation inside the knife-sharp shear bands in mid-crustal granites;Journal of Structural Geology;2023-12
2. A natural example of brittle-to-viscous strain localization under constant-stress conditions: a case study of the Kellyland fault zone, Maine, USA;Geological Magazine;2021-11-15
3. Distribution and magnitude of stress due to lateral variation of gravitational potential energy between Indian lowland and Tibetan plateau;Geophysical Journal International;2018-11-01
4. Seismic cycle feedbacks in a mid-crustal shear zone;Journal of Structural Geology;2018-07
5. Pulverized granite at the brittle-ductile transition: An example from the Kellyland fault zone, eastern Maine, U.S.A.;Journal of Structural Geology;2017-08
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