Normal Fault Foreshocks
Normal Fault Foreshocks is a seismological phenomenon characterized by a sequence of localized, low-magnitude earthquakes preceding a larger mainshock on a normal fault, distinguished by their specific occurrence in extensional tectonic regimes and their spatiotemp在玩家中 clustering in the preparatory phase of fault rupture.
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2017–2026
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Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
13 h-index
47 publications
3K citations

Sapienza University of Rome
Rome, Italy
4 h-index
9 publications
624 citations

University of Manchester
Manchester, United Kingdom
3 h-index
9 publications
1.2K citations
ETH Zurich
Zurich, Switzerland
3 h-index
3 publications
161 citations
GFZ Helmholtz Centre for Geosciences
Potsdam, Germany
3 h-index
5 publications
112 citations
Institute of Environmental Geology and Geoengineering
Monterotondo, Italy
3 h-index
8 publications
466 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
6 publications
234 citations

Chinese Academy of Geological Sciences
Beijing, China
2 h-index
7 publications
152 citations
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