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KINE3D: a New 3d Restoration Method Based on a Mixed Approach Linking Geometry and Geomechanics

机译:KINE3D:一种基于几何和地质力学的混合方法的3d恢复新方法

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We developed a new methodology for 3D restoration by coupling a geometric modelling software and a mechanical finite-element code. This method allows the geologist to impose the displacement on the main faults in order to get an adequate restored geometry and to compute the 3D strain and stress fields within the main blocks based on the unfolding with the mechanical approach. Complex meshing of the solid take into account heterogeneities due to the layering and facies variation. Results are discussed on compressive and extensional contexts, as well as in backward and forward approaches. The compressive case is illustrated by the restoration of a faulted anticline with massive sand and shaly beds. This case has been also restored with 2D surface unfolding processes and we will compare the information that geologists may get from the various methods. The second case concerns the deformation, in a gravity gliding context, of a sandy channel embedded into a shaly matrix. The mixed approach allows to quantify the reorientation of the stress field on the sand/shale boundary.
机译:通过结合几何建模软件和机械有限元代码,我们开发了3D还原的新方法。这种方法允许地质学家将位移施加在主要断层上,以便获得足够的恢复几何形状,并基于机械方法的展开来计算主要区块内的3D应变和应力场。实体的复杂网格划分考虑了由于分层和相变而引起的异质性。在压缩和扩展上下文以及后退和前进方法中讨论了结果。该受压情况以断层背斜的恢复为例,该背斜具有大量的沙子和页岩床。这种情况也已通过2D表面展开过程得以恢复,我们将比较地质学家可能从各种方法中获得的信息。第二种情况是在重力滑动的情况下,嵌入泥质基质中的沙质通道的变形。混合方法可以量化砂/页岩边界上应力场的重新定向。

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