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    • 4. 发明申请
    • Rock Physics Model For Simulating Seismic Response In Layered Fractured Rocks
    • 岩石物理模型,用于模拟分层岩石中的地震反应
    • US20100312534A1
    • 2010-12-09
    • US12863867
    • 2009-01-26
    • Shiyu XuGanglin Chen
    • Shiyu XuGanglin Chen
    • G06F7/60G06F17/10
    • G01V1/50G01V2210/626
    • 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.
    • 包含混合裂隙岩和其他地质体的地下区域各向异性弹性特征建模方法。 获得P波,快慢慢S波原子,并开发出地下地区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的岩石物理模型计算井和方向上的快速和慢速S波测井(22)。 将计算值与迭代模型更新过程中的测量值进行比较(23)。 通过使用能够处理至少斜方晶各向异性的升高理论(24)平均每层中的弹性特性来开发升高的ID模型。 ID模型可用于生成井架或AVO建模的合成地震反应(25)。 此外,公开了一种用于估计来自一个或多个偏斜井的P-和快/慢S波测井的各向异性参数的方法。
    • 5. 发明授权
    • Integrated anisotropic rock physics model
    • 综合各向异性岩石物理模型
    • US07676349B2
    • 2010-03-09
    • US11666374
    • 2005-10-27
    • Shiyu XuRebecca L. SaltzerRobert G. Keys
    • Shiyu XuRebecca L. SaltzerRobert G. Keys
    • G06F7/60G06F17/10
    • G01V99/00
    • Method for constructing an integrated rock physics model that simulates both shale anisotropy and stress-induced anisotropy of clastic rocks. In the model, the total pore volume is divided into three parts according to the estimated shale volume and effective stress: (1) clay-related pores, (2) sand-related pores, and (3) microcracks (mainly in the sand component). The pore space is then partitioned into the clay-related and sand-related pores using a scheme first disclosed by Xu and White in 1995. The model simulates shale anisotropy via the preferred orientation of clay-related pores and stress-induced anisotropy via the preferred orientation of microcracks, which is controlled by the differential stresses. Laboratory measurements or well logs are needed to establish a relationship between crack density and the effective stress.
    • 构建综合岩石物理模型的方法,该模型模拟碎屑岩的页岩各向异性和应力诱导各向异性。 在模型中,根据估计的页岩体积和有效应力,总孔容积分为三部分:(1)粘土相关孔,(2)砂相孔,(3)微裂纹(主要在砂组分 )。 然后使用徐和白在1995年首先公开的方案将孔隙分隔成粘土相关和砂相关孔。该模型通过优选的粘土相关孔取向和应力诱导各向异性模拟页岩各向异性 微裂纹的取向,由微分应力控制。 需要实验室测量或测井以确定裂纹密度与有效应力之间的关系。
    • 6. 发明授权
    • Rock physics model for simulating seismic response in layered fractured rocks
    • 用于模拟层状断裂岩石地震反应的岩石物理模型
    • US08184502B2
    • 2012-05-22
    • US12863867
    • 2009-01-26
    • Shiyu XuGanglin Chen
    • Shiyu XuGanglin Chen
    • G01V1/00G06F7/60G06F17/10
    • G01V1/50G01V2210/626
    • 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.
    • 包含混合裂隙岩和其他地质体的地下区域各向异性弹性特征建模方法。 获得P波,快慢慢S波原子,并开发出地下地区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的岩石物理模型计算井和方向上的快速和慢速S波测井(22)。 将计算值与迭代模型更新过程中的测量值进行比较(23)。 通过使用能够处理至少斜方晶各向异性的升高理论(24)平均每层中的弹性特性来开发升高的ID模型。 ID模型可用于生成井架或AVO建模的合成地震反应(25)。 此外,公开了一种用于估计来自一个或多个偏斜井的P-和快/慢S波测井的各向异性参数的方法。