物探化探计算技术
物探化探計算技術
물탐화탐계산기술
COMPUTING TECHNIQUES FOR GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2015年
1期
83-88
,共6页
陈利%方中于%但志伟%杨平华%梁立锋
陳利%方中于%但誌偉%楊平華%樑立鋒
진리%방중우%단지위%양평화%량립봉
叠前同步反演%岩石物理分析%密度%储层预测
疊前同步反縯%巖石物理分析%密度%儲層預測
첩전동보반연%암석물리분석%밀도%저층예측
prestack synchronous inversion%petrophysics analysis%density%reservoir prediction
经前人研究结果表明,珠江口盆地M地区常规叠后波阻抗较难识别储层和反映储层物性。使用叠前同步反演方法,即利用叠前CRP道集和测井信息,采用Fatti方程的改进形式进行反演,可同时获得纵波阻抗、横波阻抗、密度等弹性参数。结果表明,密度属性能很好地区分储层,反映储层物性,目的层灰岩和砂岩储层的沿层密度属性很好地反映了储层横向变化规律。实钻结果表明,预测结果与井实测结果吻合度较高,表明利用叠前同步反演技术进行珠江口盆地M地区储层预测是可行的。
經前人研究結果錶明,珠江口盆地M地區常規疊後波阻抗較難識彆儲層和反映儲層物性。使用疊前同步反縯方法,即利用疊前CRP道集和測井信息,採用Fatti方程的改進形式進行反縯,可同時穫得縱波阻抗、橫波阻抗、密度等彈性參數。結果錶明,密度屬性能很好地區分儲層,反映儲層物性,目的層灰巖和砂巖儲層的沿層密度屬性很好地反映瞭儲層橫嚮變化規律。實鑽結果錶明,預測結果與井實測結果吻閤度較高,錶明利用疊前同步反縯技術進行珠江口盆地M地區儲層預測是可行的。
경전인연구결과표명,주강구분지M지구상규첩후파조항교난식별저층화반영저층물성。사용첩전동보반연방법,즉이용첩전CRP도집화측정신식,채용Fatti방정적개진형식진행반연,가동시획득종파조항、횡파조항、밀도등탄성삼수。결과표명,밀도속성능흔호지구분저층,반영저층물성,목적층회암화사암저층적연층밀도속성흔호지반영료저층횡향변화규률。실찬결과표명,예측결과여정실측결과문합도교고,표명이용첩전동보반연기술진행주강구분지M지구저층예측시가행적。
The previous research results showed that it was difficult to identify reservoir and to indicate reservoir porosity property by using routine post-stack impedance in M region of Zhuj iangkou basin.Using prestack synchronous inversion tech-nology,by using prestack CRP gathers and logging data by the improvement form of Fatti equation,could obtain impedance, shear impedance,density data and so on at the same time.The results show that the density attribute could clearly distinguish reservoir,and indicate reservoir porosity property,the density attribute along the goal layers of limestone and sandstone reser-voir could clearly indicate the reservoir lateral chang law.The drilling results showed that the coincide was high between the prediction results and the actual measurement results,so it was feasible to predict reservoir by using prestack synchronous in-version technology in M region of Zhuj iangkou basin.