Low Dissipation of Earthquake Energy Where a Fault Follows Pre‐Existing Weaknesses: Field and Microstructural Observations of Malawi’s Bilila‐Mtakataka Fault-Reference-Cited by-同舟云学术

Low Dissipation of Earthquake Energy Where a Fault Follows Pre‐Existing Weaknesses: Field and Microstructural Observations of Malawi’s Bilila‐Mtakataka Fault

Published:2022-04-14 Issue:8 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Williams Jack N.¹²³^ORCID,Fagereng Åke¹^ORCID,Wedmore Luke N. J.³^ORCID,Biggs Juliet³^ORCID,Mdala Hassan⁴,Mphepo Felix⁴,Hodge Michael¹^ORCID

Affiliation:

1. School of Earth and Environmental Sciences Cardiff University Cardiff UK

2. Now at the Department of Geology University of Otago Dunedin New Zealand

3. School of Earth Sciences University of Bristol Bristol UK

4. Geological Survey Department Mzuzu Regional Office Mzuzu Malawi

Funder

Engineering and Physical Sciences Research Council

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL095286

Reference77 articles.

1. Constraints on Rift Basin Structure and Border Fault Growth in the Northern Malawi Rift From 3‐D Seismic Refraction Imaging

2. A multi-kilometer pseudotachylyte system as an exhumed record of earthquake rupture geometry at hypocentral depths (Colorado, USA)

3. Microfracturing, paleostress and the growth of faults

4. A quantitative study of the influence of pre‐existing compositional and fabric heterogeneities upon fracture‐zone development during basement reactivation;Beacom L. E.,2001

5. Three-dimensional characterization of a crustal-scale fault zone: The Pusteria and Sprechenstein fault system (Eastern Alps)

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