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Wedge equilibrium in fold-and-thrust belts: prediction of out-of-sequence thrusting based on sandbox experiments and natural examples

Published online by Cambridge University Press:  01 April 2016

D.A. Nieuwland ,
J.H. Leutscher  and
J. Gast
D.A. Nieuwland*
Affiliation:
Shell International E & P, Research and Technical Services, Volmerlaan 6–8, 2288 GD, RIJSWIJK, the Netherlands
J.H. Leutscher*
Affiliation:
Geology Dept. Utrecht University, UTRECHT, the Netherlands
J. Gast*
Affiliation:
Geology Dept. Utrecht University, UTRECHT, the Netherlands
*
1corresponding author; present address: Vrije Universiteit, de Boelelaan 1085, 1081 HV AMSTERDAM, the Netherlands; e-mail: nied@geo.vu.nl
2 present address: Agip Norway, P.O. Box 101, N-4033 Forus, Norway
3 present address: Nederlandse Aardolie Maatschappij, VELZEN, the Netherlands
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Abstract

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Thrust tectonics are dealt with on the basis of primarily experiments focusing on the dynamics of a developing thrust belt and on understanding and predicting normal-sequence and out-of-sequence thrusting. Field examples are presented in addition to the examples of sandbox-model experiments. The results have improved the insight into thrust-belt-forming mechanisms; the validity of the conclusions is supported by natural examples.

The experimental program was aimed at examining the effect of changes in a selection of key parameters in thrust tectonics on the geometry and the successive phases in the development of thrust sheets. Sandbox experiments were used to analyse the effects of basal friction, detachment lithology, basement relief and syntectonic sedimentation. Multilayer experiments were performed to simulate the effects of ductile detachment lithologies.

It was found that a thrust belt’s cross-sectional geometry is formed in a dynamic process during which the wedge may develop from subcritical through critical to supercritical and back to critical again. The process is illustrated with sandbox experiments, analysed by time-lapse computed tomography scans and in-situ stress measurements. On the basis of the sandbox-model results and the natural examples, we conclude that a critical examination of the boundary conditions of a fold-and-thrust belt and of changes in these conditions during the deformation process enables predictions about the geometry and kinematics of the thrust belt.

Keywords

brittle behaviourcritical taperductile behaviourgeometrykinematicsthrust tectonics
Type
Research Article
Information
Netherlands Journal of Geosciences , Volume 79 , Issue 1 , March 2000 , pp. 81 - 91
Copyright
Copyright © Stichting Netherlands Journal of Geosciences 2000

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