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    • 4. 发明申请
    • Subsurface Estimation of Level of Organic Maturity
    • 有机成熟度的地下估计
    • US20160139293A1
    • 2016-05-19
    • US14944312
    • 2015-11-18
    • Schlumberger Technology Corporation
    • Siddharth MisraJohn RasmusDean HomanCarlos Torres-Verdin
    • G01V3/38G01V11/00
    • G01V3/30G01F1/74
    • A method for determining a level of organic maturity of a shale gas formation includes inverting multifrequency complex conductivity data to estimate a volume fraction of graphite, turbostatic carbon nanostructures, and pyrite. The inversion is validated using estimates of the volume fraction of graphite, turbostatic carbon nanostructures, and pyrite. The volume fraction of graphite and turbostatic carbon nanostructures is correlated to a level of organic maturity log of the shale gas formation. The level of organic maturity log is validated using sulfur content obtained from pyrolysis or vitrinite reflectance. A variation of an electromagnetic response due to the volume fraction of graphite, turbostatic carbon nanostructures, and pyrite is quantified. The electromagnetic response is modified by removing the quantified variation to obtain resistivity and permittivity values.
    • 用于确定页岩气形成层的有机成熟度的方法包括反演多频复合电导率数据以估计石墨,涡旋型碳纳米结构和黄铁矿的体积分数。 使用石墨,涡轮增压碳纳米结构和黄铁矿体积分数的估计验证反演。 石墨和涡轮增压碳纳米结构的体积分数与页岩气形成的有机成熟度对数相关。 有机成熟度的水平通过从裂解或镜质体反射率获得的硫含量来验证。 量化了由石墨,涡旋型碳纳米结构和黄铁矿的体积分数引起的电磁响应的变化。 通过去除量化变化来获得电阻率和介电常数值来修改电磁响应。