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A geological explanation for intraplate earthquake clustering complexity: The zeolite-bearing fault/fracture networks in the Adamello Massif (Southern Italian Alps)

Dempsey, E. D.; Holdsworth, R. E.; Imber, J.; Bistacchi, A.; Di Toro, G.

Authors

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Dr Edward Dempsey E.Dempsey@hull.ac.uk
Lecturer in Structural Geology, Programme Director (Geology and GPG)

R. E. Holdsworth

J. Imber

A. Bistacchi

G. Di Toro

Abstract

Interconnected networks of faults and veins filled with hydrothermal minerals such as zeolite are widespread in many orogenic terrains. These fractures commonly form at relatively low temperatures (e.g.

Journal Article Type Article
Publication Date 2014-09
Journal Journal of Structural Geology
Print ISSN 0191-8141
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 66
Pages 58-74
Institution Citation Dempsey, E. D., Holdsworth, R. E., Imber, J., Bistacchi, A., & Di Toro, G. (2014). A geological explanation for intraplate earthquake clustering complexity: The zeolite-bearing fault/fracture networks in the Adamello Massif (Southern Italian Alps). Journal of Structural Geology, 66, 58-74. doi:10.1016/j.jsg.2014.04.009
DOI https://doi.org/10.1016/j.jsg.2014.04.009
Keywords Faulting; Earthquake clusters; Hydraulic fracturing; Stress inversions; Stress transfer; Zeolites
Publisher URL https://www.sciencedirect.com/science/article/pii/S0191814114000984?via%3Dihub
Additional Information This article is maintained by: Elsevier; Article Title: A geological explanation for intraplate earthquake clustering complexity: The zeolite-bearing fault/fracture networks in the Adamello Massif (Southern Italian Alps); Journal Title: Journal of Structural Geology; CrossRef DOI link to publisher maintained version: http://dx.doi.org/10.1016/j.jsg.2014.04.009; Content Type: article; Copyright: Copyright © 2014 Elsevier Ltd. All rights reserved.