Cookies

We use cookies to ensure that we give you the best experience on our website. By continuing to browse this repository, you give consent for essential cookies to be used. You can read more about our Privacy and Cookie Policy.


Durham Research Online
You are in:

Lithological and structural control on fracture frequency distribution within a carbonate-hosted relay ramp.

Mercuri, Marco and Carminati, Eugenio and Tartarello, Maria Chiara and Brandano, Marco and Mazzanti, Paolo and Brunetti, Alessandro and McCaffrey, Ken J.W. and Collettini, Cristiano (2020) 'Lithological and structural control on fracture frequency distribution within a carbonate-hosted relay ramp.', Journal of structural geology., 137 . p. 104085.

Abstract

Understanding the factors controlling fracture frequency distribution can greatly improve the assessment of fluid circulation in fault damage zones, with evident implications for fault mechanics, hydrogeology and hydrocarbon exploration. This is particularly important for relay zones that are usually characterized by strong damage and structural complexity. We investigated the fracture frequency within an outcrop adjacent to the front fault segment of a relay ramp, hosted within peritidal carbonates that forms part of the Tre Monti fault (Central Italy). We analysed the distribution of fracture frequency in the outcrop through (1) scanlines measured in the field, (2) oriented rock samples, and (3) scan-areas performed on a virtual outcrop model. Fracture frequency increases with distance from the front segment of the relay ramp. Moreover, supratidal and intertidal carbonate facies exhibit higher fracture frequency than subtidal limestones. This trend of increased fracture frequency has two main explanations. (1) The number of subsidiary faults and their associated damage zones increases moving away from the front segment. (2) the supratidal and intertidal carbonate facies content increases toward the centre of the relay ramp. Our results indicate that the fracture frequency pattern is very complex in relay ramps hosted in shallow-water limestones and that its prediction necessitates a good control on structures and sedimentary facies distribution.

Item Type:Article
Full text:(AM) Accepted Manuscript
Available under License - Creative Commons Attribution Non-commercial No Derivatives.
Download PDF
(40221Kb)
Status:Peer-reviewed
Publisher Web site:https://doi.org/10.1016/j.jsg.2020.104085
Publisher statement:© 2020 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/
Date accepted:04 May 2020
Date deposited:19 May 2020
Date of first online publication:16 May 2020
Date first made open access:16 May 2021

Save or Share this output

Export:
Export
Look up in GoogleScholar