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Civil-Comp Proceedings
ISSN 1759-3433 CCP: 105
PROCEEDINGS OF THE NINTH INTERNATIONAL CONFERENCE ON ENGINEERING COMPUTATIONAL TECHNOLOGY Edited by:
Paper 102
Simulation of Geological Fault Formation Mechanisms using the Discrete Element Method Y.A. Ferreira1,2, L.C.L.M. Vieira1 , V.C.L. Ramos1 and D.L. Ramos1
1Federal University of Alagoas, Maceió, Brazil
Y.A. Ferreira, L.C.L.M. Vieira , V.C.L. Ramos, D.L. Ramos, "Simulation of Geological Fault Formation Mechanisms using the Discrete Element Method", in , (Editors), "Proceedings of the Ninth International Conference on Engineering Computational Technology", Civil-Comp Press, Stirlingshire, UK, Paper 102, 2014. doi:10.4203/ccp.105.102
Keywords: geologic fault, discrete element method, sandbox.
Summary
The analysis of the geological fault formation mechanism is important in petroleum
exploration industries. Depending on the existing stresses and flow direction, the
faults can become preferential flow channels. Numerical and analogue modeling
methods represent two different techniques, which can be used to investigate the
evolution of geological structures. The experiment called sandbox has been used to
analyze the fault formation mechanism in sedimentary basins. In this paper the
analysis of the geologic faults formation mechanisms using the discrete element
method, through the numerical sandbox experiment, is reported. This numerical
model is composed of distinct particles that displace independently of one another,
and interact only at contacts or interfaces between the particles. The discrete element
program PetroDEM has been used to study the effect from the movement between
blocks with a two-dimensional model. The analysis is performed in a qualitative
mode. The simulations are carried out for cases with uniform and non-uniform grain
size, which in both cases are analyze the effect of the variation of the tangential
stiffness, the effect of parameters in a parametric study of the material properties is
investigated. The simulations produce a wide range of fundamental structures
similar to those observed in nature and in the analogue models.
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