F
Francesca Meneghini
Researcher at University of Pisa
Publications - 46
Citations - 1198
Francesca Meneghini is an academic researcher from University of Pisa. The author has contributed to research in topics: Subduction & Fault (geology). The author has an hindex of 16, co-authored 44 publications receiving 930 citations. Previous affiliations of Francesca Meneghini include University of California, Santa Cruz & Universidade Federal de Ouro Preto.
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Journal ArticleDOI
Large-scale pseudotachylytes and fluidized cataclasites from an ancient subduction thrust fault
TL;DR: In this article, the pseudotachylyte was found to be composed of glass, with vesicles, amygdules, microlites, and flow structures, indicating a frictional melt.
Journal ArticleDOI
Slow slip source characterized by lithological and geometric heterogeneity
Philip M. Barnes,Laura M. Wallace,Demian M. Saffer,Rebecca E. Bell,Michael B. Underwood,Ake Fagereng,Francesca Meneghini,Heather M. Savage,H. S. Rabinowitz,Julia K. Morgan,Hiroko Kitajima,Steffen Kutterolf,Yoshitaka Hashimoto,Christie Helouise Engelmann de Oliveira,Atsushi Noda,Martin P. Crundwell,Claire Shepherd,Adam Woodhouse,Robert N. Harris,Maomao Wang,Stuart Henrys,D. Barker,Katerina Petronotis,Sylvain Bourlange,Michael B. Clennell,Ann E. Cook,Brandon Dugan,Judith Elger,Patrick M. Fulton,Davide Gamboa,Annika Greve,S. Han,Andre Hüpers,Matt J. Ikari,Yoshihiro Ito,Gil Young Kim,Hiroaki Koge,Hikweon Lee,Xuesen Li,Min Luo,Pierre Malie,Gregory F. Moore,Joshu J. Mountjoy,David D. McNamara,M. Paganoni,Elizabeth J. Screaton,Uma Shankar,Srisharan Shreedharan,Evan A. Solomon,X. Wang,H.-Y. Wu,Ingo Pecher,Leah J. LeVay,Iodp Expedition Scientists +53 more
TL;DR: Observations suggest that SSEs and associated slow earthquake phenomena are promoted by lithological, mechanical, and frictional heterogeneity within the fault zone, enhanced by geometric complexity associated with subduction of rough crust.
Journal ArticleDOI
Deformation and hydrofracture in a subduction thrust at seismogenic depths: The Rodeo Cove thrust zone, Marin Headlands, California
TL;DR: The authors investigated the fabric and the deformational processes of an exhumed subduction zone thrust active at seismogenic depths in the Rodeo Cove thrust zone, which outcrops north of the Golden Gate Bridge of San Francisco, imbricates two basalt-chertsandstone sequences belonging to the Marin Headlands terrane.
Journal ArticleDOI
Anatomy of the Ligure-Piemontese subduction system: evidence from Late Cretaceous-middle Eocene convergent margin deposits in the Northern Apennines, Italy
TL;DR: In this paper, the authors present a brief history of geological research in the Northern Apennines during the last half of the twentieth century and then a comprehensive picture of the stratigraphy and tectonics of the Ligurian units.
Book ChapterDOI
How Accretionary Prisms Elucidate Seismogenesis in Subduction Zones
TL;DR: In this paper, thermal models suggest that the earthquakes on the plate-boundary thrusts initiate in a temperature range of 125 o C to about 350 o C. Because syndeformational diagenetic and metamorphic alterations recorded in accretionary prisms have specific temperature ranges, the alterations and the associated deformation can be correlated to the temperature range that accretionial prisms are seismogenic.