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

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.

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Bibliographic Details
Published in:Journal of structural geology 2014-09, Vol.66, p.58-74
Main Authors: Dempsey, E.D., Holdsworth, R.E., Imber, J., Bistacchi, A., Di Toro, G.
Format: Article
Language:English
Subjects:
Earthquake clusters
Faulting
Hydraulic fracturing
Stress inversions
Stress transfer
Zeolites
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Description
Summary: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.
ISSN:0191-8141
1873-1201
DOI:10.1016/j.jsg.2014.04.009