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| 松辽盆地北部泉三、四段异常高孔隙带预测 | |
| 引用本文： | 孟元林,丁桂霞,吴河勇,姜文亚,修洪文,李亚光,王又春,王正伟. 松辽盆地北部泉三、四段异常高孔隙带预测[J]. 中国石油大学学报(自然科学版), 2011, 35(4): 8-13. DOI: 10.3969/j.issn.1673-5005.2011.04.002 |
| 作者姓名： | 孟元林 丁桂霞 吴河勇 姜文亚 修洪文 李亚光 王又春 王正伟 |
| 作者单位： | 1. 东北石油大学地球科学学院,黑龙江大虎,163318 2. 中国石油大庆油田勘探开发研究院,黑龙江大庆,163712 3. 中国石油大港油田勘探开发研究院,天津,300280 4. 大庆油田第五采油厂,黑龙江大庆,163513 5. 大庆油田第八采油厂,黑龙江大庆,166400 |
| 摘 要： | 松辽盆地北部泉三、四段发育3个异常高孔隙带,主要由有机酸溶蚀储层形成。为预测次生孔隙发育带的横向展布,应用成岩作用数值模拟技术,对松辽盆地北部泉三、四段成岩阶段和成岩相的展布进行研究,探讨影响次生孔隙发育的地质因素并对异常高孔隙带进行预测。结果表明:次生孔隙发育的储层主要形成于曲流河、三角洲平原和三角洲前缘砂体,目前处于中成岩阶段A1亚期,发育中期溶蚀成岩相;从盆地边部到中心,早期压实相、早期胶结相、早期溶蚀相、中期溶蚀相、晚期溶蚀相和晚期胶结相呈环带状展布,在纵向上相邻的成岩相,在横向上也相邻,可称之为"成岩相律";泉三段Sq3异常高孔隙带主要分布在中央坳陷周围的边缘地区。 |
| 关 键 词： | 次生孔隙 成岩作用 成岩相 沉积相 扶杨油层 松辽盆地 |
Prediction of anomalously high porosity zones of K1 q3 and K1q4 in northern Songliao Basin |
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| MENG Yuan-lin,DING Gui-xia,WU He-yong,JIANG Wen-ya,XIU Hong-wen,LI Ya-guang,WANG You-chun,WANG Zheng-wei. Prediction of anomalously high porosity zones of K1 q3 and K1q4 in northern Songliao Basin[J]. Journal of China University of Petroleum (Edition of Natural Sciences), 2011, 35(4): 8-13. DOI: 10.3969/j.issn.1673-5005.2011.04.002 | |
| Authors: | MENG Yuan-lin DING Gui-xia WU He-yong JIANG Wen-ya XIU Hong-wen LI Ya-guang WANG You-chun WANG Zheng-wei |
| Affiliation: | MENG Yuan-lin1,DING Gui-xia1,WU He-yong2,JIANG Wen-ya3,XIU Hong-wen2,LI Ya-guang2,WANG You-chun4,WANG Zheng-wei5 (1.Earth Science Department,Northeast Petroleum University,Daqing 163318,China,2.Exploration & Development Research Institute of Daqing Oilfield,PetroChina,Daqing 163712,3.Exploration & Development Research Institute of Dagang Oilfield,Tianjin 300280,4.5th Oil Production Plant of Daqing Oilfield,Daqing 163513,5.8th Oil Production Plant of Daqing Oilfield,Daqing 1... |
| Abstract: | There exist three anomalously high porosity zones vertically in the K1q3 and K1q4 of northern Songliao Basin.The anomalously high porosity zones were formed mainly by dissolution.In order to predict the lateral distribution of secondary porosity zones,the distributions of diagenetic stages and diagenetic facies were studied by numerical modeling,the geofactors affecting the secondary porosity developing were discussed and the anomalously high porosity zones were predicted.The results show that the anomalous... |
| Keywords: | secondary porosity diagenesis diagenetic facies sedimentary facies Fuyang oil layer Songliao Basin |
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