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Development of interconnected talc networks and weakening of continental low-angle normal faults
Cristiano Collettini
Cristiano Collettini
1
Geologia Strutturale e Geofisica, Dipartimento di Scienze della Terra, Università degli Studi di Perugia, Perugia, Italy
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Cecilia Viti
Cecilia Viti
2
Dipartimento di Scienze della Terra, Università degli Studi di Siena, Siena, Italy
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Steven A.F. Smith
Steven A.F. Smith
3
Reactivation Research Group, Department of Earth Sciences, University of Durham, Durham DH13LE, UK *Current address: Istituto Nazionale di Geofisica e Vulcanologia (INGV), Via di Vigna Murata 605, 00143 Rome, Italy.
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Robert E. Holdsworth
Robert E. Holdsworth
3
Reactivation Research Group, Department of Earth Sciences, University of Durham, Durham DH13LE, UK
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Geology (2009) 37 (6): 567-570.
Published:
June 01, 2009
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Cristiano Collettini, Cecilia Viti, Steven A.F. Smith, Robert E. Holdsworth; Development of interconnected talc networks and weakening of continental low-angle normal faults. Geology ; 37 (6): 567–570. doi: https://doi.org/10.1130/G25645A.1
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Index Terms/Descriptors
- Apennines
- case studies
- continental crust
- crust
- crystal growth
- EDS spectra
- Elba
- Europe
- experimental studies
- faults
- foliation
- geophysical methods
- geophysical profiles
- geophysical surveys
- Italy
- low-angle faults
- mechanics
- normal faults
- Northern Apennines
- seismic methods
- seismic profiles
- SEM data
- sheet silicates
- silicates
- Southern Europe
- spectra
- strength
- surveys
- talc
- TEM data
- Tuscany Italy
- X-ray diffraction data
- X-ray spectra
- Zuccale Fault
- CROP Program
Latitude & Longitude
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