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首页> 外文期刊>Journal of structural geology >Kinematic interpretation of shearband boudins: New parameters and ratios useful in HT simple shear zones
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Kinematic interpretation of shearband boudins: New parameters and ratios useful in HT simple shear zones

机译:剪切带布丁的运动学解释:HT简单剪切带中有用的新参数和比率

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摘要

Shearband boudins (asymmetric boudins showing slip along the inter-boudin surface, which is synthetic with respect to the bulk shear sense) are ubiquitous and well exposed in HT simple shear zones. The present work aims to extend the methodology of analysis of shearband boudins developed by Goscombe and Passchier (2003). Such shearband boudins represent complex objects that require an adequate methodology for unambiguous kinematic interpretation. We propose new geometric parameters (Bbs, B-t, c', D′, d, ψ′) in order to describe and identify, with confidence, the kinematics of boudinage in this particular geological framework. The key-observation for kinematic interpretation in simple shear regimes is the boudin axis (Lb) that is commonly present, excluding the necessity to identify the regional stretching lineation (Lx) in the metasedimentary matrix. In monoclinic HT simple shear zones, this approach involves the use of a local displacement plane (Sx), which is always normal to the boudin axis (Lb).
机译:剪切带布丁(不对称布丁沿布丁间表面显示滑动,相对于整体剪切方向而言是合成的)无处不在,并且在HT简单剪切区域中充分暴露。本工作旨在扩展由Goscombe和Passchier(2003)开发的剪切带布丁分析方法。这样的剪切带布丁代表了复杂的物体,这些物体需要适当的方法来进行明确的运动学解释。我们提出了新的几何参数(Bbs,B-t,c',D',d,ψ'),以便自信地描述和识别在此特定地质框架中的后腿运动学。在简单剪切状态下进行运动学解释的关键观察是通常存在的布丁轴(Lb),而不必在变质沉积矩阵中识别区域性伸展线(Lx)。在单斜HT简单剪切带中,这种方法涉及使用局部位移平面(Sx),该平面始终垂直于Boudin轴(Lb)。

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