扬子北缘中二叠统孤峰组不同岩性孔隙特征及其地质意义Pore Characteristics of Different Lithologies and Their Geological Significance from the Middle Permian Gufeng Formation in the North Margin of Yangtze
梁西文,吴勘,马强分,冯庆来,喻建新
摘要(Abstract):
孔隙是页岩层系是否具有生烃能力、储气能力和开采价值的主要标志。采用场发射扫描电镜对鄂西建始扬子北缘中二叠统孤峰组硅质页岩、泥质灰岩和碳质页岩3类岩石采取二次电子模式扫描,发现并分析了5大类9小类孔隙,即①絮凝作用孔隙;②有机质化石孔;③有机质碎片沥青孔;④黄铁矿粒间孔;⑤矿物颗粒晶间孔;⑥微型通道;⑦微裂缝;⑧钙质化石孔;⑨碎屑与围岩之间孔。研究表明,硅质页岩中发育较多的黄铁矿微球粒以及絮凝结构,有机质孔隙从纳米级至微米级;泥质灰岩中以矿物质孔隙为主,微裂缝比较发育,脆性矿物多;碳质页岩中存在大量蜂窝状孔洞和广泛分布的微裂缝,孔隙类型主要为有机质纳米孔。碳质页岩与传统储层孔隙特征具有很大差异,是页岩气勘探最为有利的岩层。
关键词(KeyWords): 孤峰组;页岩气;孔隙;空间分布;资源评价
基金项目(Foundation): 国家自然科学基金项目(41272024);; 中国地质调查局项目(1212011220796);; 生物地质与环境地质国家重点实验室自主研究课题项目(GBL11302)
作者(Author): 梁西文,吴勘,马强分,冯庆来,喻建新
参考文献(References):
- [1]叶良辅,李捷.安徽宣城泾县煤田地质[J].地质汇报,1924,6:25-50.
- [2]胡世忠.对孤峰组的新认识[J].火山地质与矿产,2000,21(1):63-68.
- [3]孔庆玉,龚玉觐.苏皖地区下二叠统放射虫硅质岩形成环境探讨[J].石油与天然气地质,1987(1):86-89.
- [4]朱同兴.安徽南部下二叠同结核状硅质岩和层状硅质岩的沉积学特征及其成因探讨[J].岩相古地理,1989,43(5):1-8.
- [5]冯庆来,钟长汀.层状硅质岩沉积环境研究的一种新方法(酸溶蚀法):兼论武昌地区孤峰组沉积环境[J].岩相古地理,1994,14(5):45-55.
- [6]He W,Wu S,Zhang K,et al.Classification of radiolarian fossil zones and environmental analysis of Gufeng Formation in Lower Yangtze region[J].Jiangsu Geology,1999,23:17-23.
- [7]Kametaka M,Takebe M,Nagai H,et al.Sedimentary environments of the Middle Permian phosphorite-chert complex from the northeastern Yangtze platform,China;the Gufeng Formation:A continental shelf radiolarian chert[J].Sedimentary Geology,2005,174(3/4):197-222.
- [8]吕炳全,瞿建忠.下扬子区早二叠世海进和上升流形成的缺氧环境沉积[J].科学通报,1989,22:1721-1724.
- [9]Canfield D E.Factors influencing organic carbon preservation in marine sediments[J].Chemical Geology,1994,114:315-329.
- [10]Tribovillard N,Algeo T J,Lyons T,et al.Trace metals as paleoredox and paleoproductivity proxies:An update[J].Chemical Geology,2006,232:12-32.
- [11]Loucks R G,Reed R M,Ruppel S C,et al.Morphology,genesis,and distribution of nanometer-scale pores in siliceous mudstones of the Mississippian Barnett Shale[J].Journal of Sedimentary Research,2009,79(12):848-861.
- [12]Jarvie D M,Hill R J,Ruble T E,et al.Unconventional shalegas systems:The Mississippian Barnett Shale of north-central Texas as one model for thermogenic shale-gas assessment[J].AAPG Bulletin,2007,91(4):475-499.
- [13]Chalmers G R L,Bustin R M.Lower Cretaceous gas shales in northeastern British Columbia,Part II:Evaluation of regional potential gas resources[J].Bulletin of Canadian Petroleum Geology,2008,56(1):22-61.
- [14]Mazzullo S J,Wilhite B W,Woolsey I W.Petroleum reservoirs within a spiculite-dominated depositional sequence:Cowley Formation(Mississippian-Lower Carboniferous),south-central Kansas[J].AAPG Bulletin,2009,93(12):1649-1689.
- [15]O′Brien N R.The effects of bioturbation on the fabric of shale[J].Journal of Sedimentary Research,1987,57(3):449-455.
- [16]Turner J T.Zooplankton fecal pellets,marine snow,and sinking phytoplankton blooms[J].Aquatic Microbial Ecology,2002,27:57-102.
- [17]李明诚.石油与天然气运移[M].北京:石油工业出版社,2004:50-103.
- [18]Ross D J K,Bustin R M.Shale gas potential of the Lower Jurassic Gordondale Member,northeastern British Columbia,Canada[J].Bulletin of Canadian Petroleum Geology,2007,55(3):51-75.
- [19]Curtis M E,Sondergergeld C H,Ambrose R J,et al.Microstructural investigation of gas shales in two and three dimensions using nanometer-scale resolution imaging[J].AAPG Bulletin,2012,96(4):665-677.
- [20]Slatt R M,Abousleiman Y.Merging sequence stratigraphy and geomechanics for unconventional gas shales[J].The Leading Edge,2011,30(3):274-282.
- [21]Jarvie D M.Shale plays:Making gas and oil from shale resource systems[R].Dalas:Geological Society,2010.
- [22]冯庆来.下扬子西部区块页岩特征及含气有利区带预测[R].武汉:中国地质大学,2012.
- [23]Julia F W G,Robert M R,Jon H.Natural fractures in the Barnett Shale and their importance for hydraulic fracture treatments[J].AAPG Bulletin,2007,91(4):603-622.