4.5 Article

Thrust dip and thrust refraction in fault-bend folds: analogue models and theoretical predictions

期刊

JOURNAL OF STRUCTURAL GEOLOGY
卷 28, 期 1, 页码 36-49

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.jsg.2005.10.001

关键词

fault-bend fold; analogue modelling; minimum dissipation; thrust refraction; mechanics

向作者/读者索取更多资源

Analogue models made of two layers of loose sand separated by a thin layer of micro glass beads were shortened by a rigid emerging ramp dipping at either 30 degrees or 45 degrees and possessing a high, intermediate, or null surface friction. Shortening resulted in formation of closely spaced back thrusts in the sand layers. The dips of the back thrusts vary within a range of 30 degrees depending on the ramp friction, and 7 degrees depending on its dip. An increase in ramp friction, or, to a lesser extent, in ramp dip, decreases the thrust dips in the model. The second important observation is that, when friction is greater along the ramp than along the layer of glass beads, then the glass beads layer acts as a separate upper ramp above which the back thrusts steepen. The theory proposed to explain these observations predicts the thrust dips through a two-step procedure: first, global equilibrium of forces in the two layers is required to yield the mean forces at stake along the ramps and thrusts, second, the total dissipation is minimized with respect to the dips of the back thrusts. The relevant frictional properties of our analogue materials have been measured in stress conditions as close as possible to the experimental ones (below 1 kPa), and used with the theory to yield optimal back thrust dips that are all within 3 degrees of the measured dips. This is a surprisingly good fit when considering that we did not take into account geometric changes, strain-softening, and dilatancy or compaction, due to slip on the thrusts. We conclude that this general two-step theoretical procedure is validated in the context of analogue frictional materials. We also propose a possible mechanism for thrust refraction and top-to-the-foreland sense of shear observed in the hanging walls of lower-flat to ramp transition in sedimentary piles that is based on the triggering of secondary upper ramps. Finally, this mechanical approach can also be seen as complementary to the kinematic models of fold-thrust structures which, by definition, cannot grasp the strong effects of friction on the kinematics. (c) 2005 Elsevier Ltd. All rights reserved.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.5
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据