Seismically enhanced hydrothermal plume advection through the process zone of the Compione extensional Fault, Northern Apennines, Italy-Reference-Cited by-同舟云学术

Seismically enhanced hydrothermal plume advection through the process zone of the Compione extensional Fault, Northern Apennines, Italy

Published:2018-11-14 Issue:3-4 Volume:131 Page:547-571
ISSN:0016-7606
Container-title:GSA Bulletin
language:en
Short-container-title:

Author:

Lucca Alessio¹,Storti Fabrizio¹,Molli Giancarlo¹²,Muchez Philippe³,Schito Andrea⁴,Artoni Andrea⁵,Balsamo Fabrizio¹,Corrado Sveva⁴,Mariani Emma Salvioli⁵

Affiliation:

1. Department of Chemistry, Life Sciences and Environmental Sustainability, Natural and Experimental Tectonics research group, University of Parma, I-43124 Parma, Italy

2. Department of Earth Sciences, University of Pisa, via S. Maria, 53, I-56126 Pisa, Italy

3. Department of Earth and Environmental Sciences, Katholieke Universiteit Leuven, Celestijnenlaan 200E, B-3001 Heverlee, Belgium

4. Department of Sciences, Geology Section, Roma Tre University, L.go S. Leonardo Murialdo 1, I-00146 Roma, Italy

5. Department of Chemistry, Life Sciences and Environmental Sustainability, University of Parma, I-43124 Parma, Italy

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/131/3-4/547/4650651/547.pdf

Reference200 articles.

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2. The Northern Apennines and the kinematics of Europe-Africa convergence;Argnani;Bollettino della Società Geologica Italiana,2002

3. Gravity tectonics driven by Quaternary uplift in the Northern Apennines: Insights from the La Spezia-Reggio Emilia geo-transect;Argnani;Quaternary International,2003

4. Variables controlling epidote composition in hydrothermal and low-pressure regional metamorphic rocks;Arnason;Abhandlungen der Geologischen Bundesanstalt,1993

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