Articles | Volume 11, issue 4
https://doi.org/10.5194/se-11-1163-2020
https://doi.org/10.5194/se-11-1163-2020
Research article
 | 
05 Jul 2020
Research article |  | 05 Jul 2020

Diagenetic evolution of fault zones in Urgonian microporous carbonates, impact on reservoir properties (Provence – southeast France)

Irène Aubert, Philippe Léonide, Juliette Lamarche, and Roland Salardon

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Irène Aubert on behalf of the Authors (15 Jan 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (21 Jan 2020) by Kei Ogata
RR by Mattia Pizzati (18 Mar 2020)
ED: Reconsider after major revisions (19 Mar 2020) by Kei Ogata
AR by Irène Aubert on behalf of the Authors (08 Apr 2020)  Manuscript 
ED: Referee Nomination & Report Request started (22 Apr 2020) by Kei Ogata
RR by Mattia Pizzati (24 Apr 2020)
ED: Publish subject to technical corrections (28 Apr 2020) by Kei Ogata
ED: Publish subject to technical corrections (02 May 2020) by Elias Samankassou (Executive editor)
AR by Irène Aubert on behalf of the Authors (09 May 2020)  Author's response   Manuscript 
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Short summary
In carbonate rocks, fault zones influence the fluid flows and lead to important diagenetic processes modifying reservoir properties. The aim of this study is to identify the impact of two polyphase fault zones on fluid flows and reservoir properties during basin history. We determined petro-physic and diagenetic properties on 92 samples. This study highlights that fault zones acted as drains at their onset and induced fault zone cementation, which has strongly altered local reservoir properties.