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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.

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


Authors

E.D. Dempsey

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. < 200°C) late in the tectonic history and represent significant phases of fluid flow and mineralisation during exhumation. Zeolite-bearing fractures spatially associated with the Gole Larghe Fault Zone in the Southern Italian Alps are preserved along an interconnected network of variably orientated pre-existing structures. They show evidence of repeated episodes of hydraulic tensile fracturing and small magnitude (total offsets <5m) shear displacements. We use geological observations and Coulomb stress modelling to propose that repeated seismogenic rupturing of larger offset faults led to local stress transfer and reactivation of widely distributed smaller pre-existing structures in the wall rocks. The differing orientations of the pre-existing features within what is assumed to have been a single regional stress field led to the simultaneous development of reverse, strike-slip and extensional faults. The kinematic diversity and cyclic nature of the hydraulically-assisted deformation suggest that the mineralised fracture systems represent a geological manifestation of intraplate micro-earthquake clusters associated with fluid migration episodes in the upper crust. Our observations highlight the role of crustal fluids and structural reactivation during earthquakes.

Citation

Dempsey, E., Holdsworth, R., 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. https://doi.org/10.1016/j.jsg.2014.04.009

Journal Article Type Article
Acceptance Date Apr 28, 2014
Online Publication Date May 22, 2014
Publication Date Sep 1, 2014
Deposit Date May 22, 2014
Publicly Available Date May 22, 2014
Journal Journal of Structural Geology
Print ISSN 0191-8141
Electronic ISSN 1873-1201
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 66
Pages 58-74
DOI https://doi.org/10.1016/j.jsg.2014.04.009
Keywords Faulting, Earthquake Clusters, Hydraulic fracturing, Stress Inversions, Stress transfer, Zeolites.
Public URL https://durham-repository.worktribe.com/output/1464180

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Copyright Statement
NOTICE: this is the author’s version of a work that was accepted for publication in Journal of structural geology. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Journal of structural geology, 66, 2014, 10.1016/j.jsg.2014.04.009





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