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Parallel thrust and normal faulting in Peru and constraints on the state of stress
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“The major driving force is tectonic compression associated with the continued plate convergence, which is largely balanced by the gravitational buoyancy force arising from the isostatically supported elevation of the mountain ranges [Dalmayrac and Molnar, 1981; Molnar and Lyon-Caen, 1988].”
From Crustal shortening in the Andes: Why do GPS rates differ from geological rates? (2000) · cites this paper as Dalmayrac and Molnar, 1981
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Metadata
- Authors
- Dalmayrac, B., & Molnar, P.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 1981-11
- Volume
- 55
- Issue
- 3
- Pages
- 473-481
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2008739566
- Cited by
- 273
- References
- 37
- Citations by year
- 2026: 3 · 2025: 5 · 2024: 9 · 2023: 1 · 2022: 11 · 2021: 5 · 2020: 10 · 2019: 4 · 2018: 6 · 2017: 8 · 2016: 4 · 2015: 15 · 2014: 4 · 2013: 3 · 2012: 6
- FWCI
- 4.28
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Tectonic Studies in Latin America
- Physical Sciences › Earth and Planetary Sciences › Geophysics › earthquake and tectonic studies
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Keywords
- normal faulting, thrust faulting, Cordillera Blanca, crustal stress, buoyancy, crustal root, Peruvian Andes
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