Ultra-thick Triassic dolomites control the rupture behavior of the central Apennine seismicity: Evidence from magnetic modeling of the L'Aquila fault zone-Reference-Cited by-同舟云学术

Ultra-thick Triassic dolomites control the rupture behavior of the central Apennine seismicity: Evidence from magnetic modeling of the L'Aquila fault zone

Published:2014-09 Issue:9 Volume:119 Page:6756-6770
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Speranza Fabio¹,Minelli Liliana¹

Affiliation:

1. Istituto Nazionale di Geofisica e Vulcanologia; Roma Italy

Funder

FIRB Project

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014JB011199/fullpdf

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3. AGIP SpA Italia 1981 Carta Magnetica-Anomalie del Campo magnetico residuo

4. Coseismic deformation of the destructive April 6, 2009 L'Aquila earthquake (central Italy) from GPS data;Anzidei;Geophys. Res. Lett.,2009

5. Possible record of a Triassic ocean in the Southern Apennines;Argnani;Boll. Soc. Geol. Ital.,2005

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