Origin and role of fluids involved in the seismic cycle of extensional faults in carbonate rocks

Autor: Smeraglia L.[1], Berra F.[2], Billi A.[3], Boschi C.[4], Carminati E.[1, Doglioni C.[1

Publikováno v: Earth and planetary science letters 450 (2016): 292–305. doi:10.1016/j.epsl.2016.06.042
info:cnr-pdr/source/autori:Smeraglia L.[1], Berra F.[2], Billi A.[3], Boschi C.[4], Carminati E.[1,3], Doglioni C.[1,3]/titolo:Origin and role of fluids involved in the seismic cycle of extensional faults in carbonate rocks./doi:10.1016%2Fj.epsl.2016.06.042/rivista:Earth and planetary science letters/anno:2016/pagina_da:292/pagina_a:305/intervallo_pagine:292–305/volume:450

We examine the potentially-seismic right-lateral transtensional-extensional Tre Monti Fault (central Apennines, Italy) with structural and geochemical methods and develop a conceptual evolutionary model of extensional faulting with fluid involvement

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::057a49f4c77dba13454b57610faee43d
https://doi.org/10.1016/j.epsl.2016.06.042