浊沸石溶蚀过程的热力学计算与次生孔隙发育带预测——以徐家围子断陷深层为例  

Thermodynamic Calculations of the Laumontite Dissolution and Prediction of Secondary Porosity Zones: A case study of horizon of Xujiaweizi Fault Depression

作　　者：孟元林[1] 梁洪涛[1] 魏巍[1] 修洪文[2] 李亚光[2] 邵红梅[2] 胡安文[1] 张磊[1] 

机构地区：[1]东北石油大学地球科学学院,黑龙江大庆163318 [2]中国石油大庆油田有限责任公司勘探开发研究院,黑龙江大庆163712

出　　处：《沉积学报》2013年第3期509-515,共7页Acta Sedimentologica Sinica

基　　金：国家自然科学基金项目(批准号:U1262106);黑龙江省研究生创新科研项目(YJSCX2011-118HLJ;YJSCX2012-064HLJ);全国油气资源战略选区调查与评价国家专项(2009GYXQ13)资助

摘　　要：浊沸石是徐家围子断陷深层砂砾岩中广泛分布的一种胶结物,被有机酸溶蚀后,形成大量次生孔隙,为油气的聚集提供了储集空间。为了预测深层次生孔隙发育带的分布,本研究应用热力学计算方法,定量讨论了徐家围子断陷深层营城组砂砾岩中浊沸石的溶解—沉淀过程和次生孔隙的形成机理,并提出了溶解—沉淀指数DPI的计算模型,定量表征溶蚀作用的强度。通过叠合DPI等值线图和沉积相图,预测了浊沸石溶蚀形成次生孔隙发育带的分布。结果表明,次生孔隙发育带主要分布于DPI>2.5的扇三角洲前缘和辫状河三角洲前缘砂砾岩体中。Laumontites are important and widespread cements formed in middle-late diagenetic stage in the deep-bur- ied glutenites of Xujiaweizi Fault Depression, Songliao Basin. They are later dissolved by organic acids released from kerogens during hydrocarbon generation and expulsion, forming secondary porosities. The secondary porosities within deeply buried glutenites are the main reservoir space of hydrocarbons in the deep formation of Xujiaweizi Fault Depres- sion. In order to predict the distribution of secondary porosity zones, the dissolve-precipitation states of the laumontites and the forming mechanism of secondary porosities in the reservoirs of Yingcheng Formation were studied by using thermodynamic method. Dissolution-precipitation index DPI was proposed to quantify the dissolution and precipitation of laumontites. The distributions of the secondary porosity zones were predicted by overlapping the DPI contour map o- ver the sedimentary facies map. As the result shows, the secondary porosity zones mainly distributed in the fan delta front or braided fluvial river delta front glutenites,where DPI is greater than 2.5.

关 键 词：致密砂砾岩 非常规储层 浊沸石 深层 次生孔隙 徐家围子断陷 松辽盆地 

分 类 号：P618.130.2[天文地球—矿床学]