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  5. The effects of pre-existing discontinuities on the surface expression of normal faults: Insights from wet-clay analogue modeling
 
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The effects of pre-existing discontinuities on the surface expression of normal faults: Insights from wet-clay analogue modeling

Author(s)
Bonini, L.  
Dipartimento di Matematica e Geoscienze, Università di Trieste, Italy  
Basili, R.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Toscani, G.  
Dipartimento di Scienze della Terra e dell'Ambiente, Università di Pavia, Pavia, Italy  
Burrato, P.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Seno, S.  
Dipartimento di Scienze della Terra e dell'Ambiente, Università di Pavia, Pavia, Italy  
Valensise, G.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia  
Language
English
Obiettivo Specifico
2T. Tettonica attiva
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Tectonophysics  
Issue/vol(year)
/684 (2016)
ISSN
0040-1951
Electronic ISSN
1879-3266
Publisher
Elsevier Science Limited
Pages (printed)
157-175
Date Issued
January 29, 2016
DOI
10.1016/j.tecto.2015.12.015
Alternative Location
http://www.sciencedirect.com/science/article/pii/S0040195115006782
URI
https://www.earth-prints.org/handle/2122/10356
Subjects
04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology  
04. Solid Earth::04.04. Geology::04.04.09. Structural geology  
04. Solid Earth::04.04. Geology::04.04.11. Instruments and techniques  
Subjects

Fault growth

normal fault

pre-existing disconti...

wetclay analogue mode...

Abstract
We use wet-clay analogue models to investigate how pre-existing discontinuities (i.e. structures inherited from previous tectonic phases) affect the evolution of a normal fault at the Earth's surface. To this end we first perform a series of three reference experiments driven by a 45° dipping master fault unaffected by pre-existing discontinuities to generate a mechanically isotropic learning set of models. We then replicate the experiment six times introducing a 60°-dipping precut in the clay cake, each time with a different attitude and orientation with respect to an initially-blind, 45°-dipping, master normal fault. In all experiments the precut intersects the vertical projection of the master fault halfway between the center and the right-hand lateral tip. All other conditions are identical for all seven models. By comparing the results obtained from the mechanically isotropic experiments with results from experiments with precuts we find that the surface evolution of the normal fault varies depending on the precut orientation. In most cases the parameters of newly-forming faults are strongly influenced. The largest influence is exerted by synthetic and antithetic discontinuities trending respectively at 30° and 45° from the strike of the master fault, whereas a synthetic discontinuity at 60° and an antithetic discontinuity at 30° show moderate influence. Little influence is exerted by a synthetic discontinuity at 45° and an antithetic discontinuity at 60° from the strike of the master fault. We provide a ranking chart to assess fault-to-discontinuity interactions with respect to essential surface fault descriptors, such as segmentation, vertical-displacement profile, maximum displacement, and length, often used as proxies to infer fault properties at depth. Considering a single descriptor, the amount of deviation induced by different precuts varies from case to case in a rather unpredictable fashion. Multiple observables should be taken into consideration when analyzing normal faults evolving next to pre-existing discontinuities.
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