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Rock Physics Model For Simulating Seismic Response In Layered Fractured Rocks

机译:模拟层状破裂岩石地震响应的岩石物理模型

摘要

Method for modeling anisotropic elastic properties of a subsurface region comprising mixed fractured rocks and other geological bodies. P-wave and fast and slow S-wave logs are obtained, and an anisotropic rock physics model of the subsurface region is developed (21). P- and fast and slow S-wave logs at the well direction are calculated using a rock physics model capable of handling fractures and other geological factors (22). Calculated values are compared to measured values in an iterative model updating process (23). An upscaled ID model is developed by averaging elastic properties in each layer using an upscaling theory capable of handling at least orthorhombic anisotropy (24). The ID model may be used to generate synthetic seismic response for well ties or AVO modeling (25). Further, a method is disclosed for estimating anisotropy parameters from P- and fast/slow S-wave logs from one or more deviated wells.
机译:对包括混合裂隙岩和其他地质体的地下区域的各向异性弹性特性进行建模的方法。得到了纵波和纵波和慢波测井曲线,并建立了地下岩层的各向异性岩石物理模型( 21 )。使用能够处理裂缝和其他地质因素( 22 )的岩石物理模型计算井方向的P波和慢S波测井曲线。在迭代模型更新过程( 23 )中将计算值与测量值进行比较。通过使用至少能够处理正交各向异性( 24 )的放大理论,通过平均每一层的弹性特性,开发出一个放大的ID模型。 ID模型可用于为井带或AVO建模( 25 )生成合成地震响应。此外,公开了一种用于根据来自一个或多个偏斜井的P波和快/慢S波测井来估计各向异性参数的方法。

著录项

  • 公开/公告号US2010312534A1

    专利类型

  • 公开/公告日2010-12-09

    原文格式PDF

  • 申请/专利权人 SHIYU XU;GANGLIN CHEN;

    申请/专利号US20090863867

  • 发明设计人 SHIYU XU;GANGLIN CHEN;

    申请日2009-01-26

  • 分类号G06F7/60;G06F17/10;

  • 国家 US

  • 入库时间 2022-08-21 18:10:00

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