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METHOD FOR DERIVING RESERVOIR LITHOLOGY AND FLUID CONTENT FROM PRE-STACK INVERSION SEISMIC DATA

机译:叠前反演资料推导储层岩性和流体含量的方法

摘要

A METHOD FOR DERIVING RESERVOIR LITHOLOGY AND FLUID CONTENT FOR A TARGET LOCATION FROM PRE-STACK SEISMIC REFLECTION DATA. THE METHOD USES INVERSION OF PRE-STACK SEISMIC REFLECTION DATA (112) FOR BOTH THE TARGET LOCATION AND A CALIBRATION LOCATION (110) HAVING KNOWN SUBSURFACE LITHOLOGY AND FLUID CONTENT TO DERIVE THE SUBSURFACE LITHOLOGY AND FLUID CONTENT AT THE LOCATION. THE INVERSION PROCESS IN PREFERABLY A VISCOELASTIC INVERSION TO ACCOUNT FOR THE EFFECTS OF FRICTION ON SEISMIC WAVE PROPAGATION. THE RESULTS OF THE INVERSION PROCESS ARE A SET OF SUBSURFACE ELASTIC PARAMETERS FOR BOTH THE TARGET AND CALIBRATION LOCATIONS ( 110) .RELATIVE MAGNITUDES OF THESE SUBSURFACE ELASTIC PARAMETERS ARE COMPARED, TOGETHER WITH THE KNOWN SUBSURFACE ELASTIC PARAMETERS ARE COMPARED, TOGETHER WITH THE KNOWN SUBSURFACE LITHOLOGY AND FLUID CONTENT AT THE CALIBRATION LOCATION, TO DERIVE THE SUBSURFACE LITHOLOGY AND FLUID CONTENT AT THE TARGET LOCATION.(FIGURE 1)
机译:一种从叠前地震反射数据推导目标位置的储层岩性和流体含量的方法。该方法对目标位置和标定位置(110)都使用叠前地震反射数据(112)进行反演,这些位置具有已知的地下岩性和流体含量,可以推导该位置的地下岩性和流体含量。倒转过程最好是粘弹性倒转,以说明摩擦力对地震波传播的影响。转换过程的结果是针对目标位置和校准位置的一组亚表面弹性参数(110)。这些亚表面弹性参数的相对大小已比较,并且与已知的亚表面弹性参数相同校准位置的流体含量和流体含量,以推导目标位置的地下岩性和流体含量(图1)。

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