Structural properties of fractured and faulted Cretaceous platform carbonates, Murge Plateau (southern Italy)-Reference-Cited by-同舟云学术

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Structural properties of fractured and faulted Cretaceous platform carbonates, Murge Plateau (southern Italy)

Published:2014-11 Issue: Volume:57 Page:312-326
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Korneva I.^ORCID,Tondi E.,Agosta F.,Rustichelli A.,Spina V.,Bitonte R.,Di Cuia R.

Funder

PRIN 2009

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference83 articles.

1. Fluid conduits in carbonate-hosted seismogenic normal faults of Central Italy;Agosta;J. Geophys. Res.,2003

2. Architecture and deformation mechanism of a basin-bounding normal fault in Mesozoic platform carbonates, central Italy;Agosta;J. Struct. Geol.,2006

3. Geochemical traces of CO2-rich fluid flow along normal faults of central Italy;Agosta;Geophys. J. Int.,2008

4. Oblique normal faulting along the northern edge of the Majella Anticline, central Italy: inferences on hydrocarbon migration and accumulation;Agosta;J. Struct. Geol.,2009

5. From fractures to flow: a field-based quantitative analysis of an outcropping carbonate reservoir;Agosta;Tectonophysics,2010

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4. Depositional Setting, Diagenetic Processes, and Pressure Solution-Assisted Compaction of Mesozoic Platform Carbonates, Southern Apennines, Italy;Geosciences;2024-03-22

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