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  5. The role of shale content and pore-water saturation on frictional properties of simulated carbonate faults
 
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The role of shale content and pore-water saturation on frictional properties of simulated carbonate faults

Author(s)
Ruggieri, Roberta  
Università La Sapienza, Roma  
Scuderi, Marco Maria  
Università La Sapienza, Roma  
Trippetta, Fabio  
Università La Sapienza, Roma  
Tinti, Elisa  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia  
Brignoli, M  
Reservoir & Petroleum Engineering Dpt, Eni SpA, 20097 San Donato Mianese, Italy  
Mantica, S  
Reservoir & Petroleum Engineering Dpt, Eni SpA, 20097 San Donato Mianese, Italy  
Petroselli, S  
Reservoir & Petroleum Engineering Dpt, Eni SpA, 20097 San Donato Mianese, Italy  
Osculati, L  
Reservoir & Petroleum Engineering Dpt, Eni SpA, 20097 San Donato Mianese, Italy  
Volontè, G  
Upstream R&D Dpt., Eni SpA, 20097 San Donato Mianese, Italy  
Collettini, Cristiano  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia  
Language
English
Obiettivo Specifico
1T. Struttura della Terra
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Tectonophysics  
Issue/vol(year)
/807 (2021)
ISSN
0040-1951
Publisher
Elsevier
Pages (printed)
228811
Date Issued
2021
DOI
10.1016/j.tecto.2021.228811
Alternative Location
https://www.sciencedirect.com/science/article/pii/S0040195121000950#!
URI
https://www.earth-prints.org/handle/2122/15581
Subjects
04.02. Exploration geophysics  
Subjects

Carbonate faults

Fault slip behavior

Abstract
The presence of weak phyllosilicates in mature carbonate fault zones has been invoked to explain weak faults. However, the relation between frictional strength, fault stability, mineralogical composition, and fabric of fault gouge, composed of strong and weak minerals, is poorly constrained. We used a biaxial apparatus to systematically shear different mixtures of shale (68% clay, 23% quartz and 4% plagioclase) and calcite, as powdered gouge, at room temperature, under constant normal stresses of 30, 50, 100 MPa and under room-dry and pore fluid-saturated conditions, i.e. CaCO3-equilibrated water. We performed 30 friction experiments during which velocity-stepping and slide-hold-slide tests were employed to assess frictional stability and to measure frictional healing, respectively. Our frictional data indicate that the mineralogical composition of fault gouges significantly affects frictional strength, stability, and healing as well as the presence of CaCO3-equilibrated water. Under room-dry condition, the increasing shale content determines a reduction in frictional strength, from μ = 0.71 to μ = 0.43, a lowering of the healing rates and a transition from velocity-weakening to velocity-strengthening behavior. Under wet condition, with increasing shale content we observe a more significant reduction in frictional strength (μ = 0.65–0.37), a near-zero healing and a velocity strengthening behavior. Microstructural investigations evidence a transition from localized deformation promoted by grain size reduction, in calcite-rich samples, to a more distributed deformation with frictional sliding along clay-enriched shear planes in samples with shale content greater than 50%. For faults cutting across sedimentary sequences composed of carbonates and clay-rich sediments, our results suggest that clay concentration and its ability to form foliated and interconnected networks promotes important heterogeneities in fault strength and slip behavior.
Type
article
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32_2021_Ruggieri et al.Tectonophysics.pdf

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18 MB

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Checksum (MD5)

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