Diagenetic evolution and controlling factors of pyroclastic reservoirs of the Lower Cretaceous in Nanbeier Sag，Hailar-Tamtsag Basin
Zhang Liyuan1, Ji Youliang1, Liu Li2, Meng Qi′an3,Zhao Lei1, Yu Miao2, Zhou Bing2
1 State Key Laboratory of Petroleum Resource and Prospecting，China University of Petroleum(Beijing)，Beijing102249; 2 College of Earth Sciences，Jilin University，Changchun130061，Jilin; 3 Exploration and Development Research Institute，Daqing Oilfield Ltd Co.，Daqing163712，Heilongjiang
Through various measurements，such as analyses of normal thin-sections，cast thin-sections，scanning electron microscope and X-ray diffraction of clay minerals，this paper systematically studies the diagenetic evolution and controlling factors of pyroclastic reservoirs from the Tongbomiao and Nantun Formations of Lower Cretaceous in Nanbeier Sag of Hailar-Tamtsag Basin.It is considered that the diagenesis types of the reservoirs include weldition，compaction，devitrification，alteration，cementation and dissolution.The main diagenesis stage is the middle diagenetic stage A.The reservoirs undergo the evolution process from syngenesis diagenetic stage to middle diagenetic stage A，part of which experience the evolution process of epidiagenetic stage.Different diagenetic evolution stages have different characteristics.The syngenesis diagenetic stage is characterized by weldition and weak cementation.While the early diagenetic stage A is featured by strong compaction and weak cementation.The early diagenetic stage B has strong compaction，weak cementation and weak dissolution.When it comes to middle diagenetic stage A，compaction becomes moderate，on the other side，compaction and dissolution get stronger.The epidiagenetic stage differs from others by meteoric water leaching.The diagenetic evolution process is controled by diagenesis environment，tectonism and volcanic activities.The diagenetic environments undego the evolution process from weak alkali to weak acidic，then acidic to alkali environments.In the acidic diagenetic environment，dissolution takes place.While，in the alkali diagenetic environment，cementation dominates.Tectonism and volcanic activities influences the diagenetic evolution process by controlling the origin of pyroclastic components，the occurrence of fractures，thermal fluid activities and the evolution of epidiagenetic stage.
Corresponding Authors:
Ji Youliang，born in 1962，is a professor of China University of Petroleum(Beijing). Now he is mainly engaged in teaching and researches of petroleum geology，sedimentology and sequence stratigraphy.E-mail:jiyouliang @cup.edu.cn.
About author: Zhang Liyuan，born in 1985，got her master degree in 2010 from Jilin University.Now，she is a Ph.D.candidate in China University of Petroleum(Beijing) and mainly engaged in the study of sedimentology and reservoir geology.E-mail:zhangliyuan426@163.com.
Cite this article:
Zhang Liyuan,Ji Youliang,Liu Li et al. Diagenetic evolution and controlling factors of pyroclastic reservoirs of the Lower Cretaceous in Nanbeier Sag，Hailar-Tamtsag Basin[J]. JOURNAL OF PALAEOGEOGRAPHY, 2013, 15(2): 261-274.
Zhang Liyuan,Ji Youliang,Liu Li et al. Diagenetic evolution and controlling factors of pyroclastic reservoirs of the Lower Cretaceous in Nanbeier Sag，Hailar-Tamtsag Basin[J]. JOPC, 2013, 15(2): 261-274.
常丽华，曹林，高福红.2009.火成岩鉴定手册［M］.北京：地质出版社，95-113.程日辉，沈艳杰，颜景波，等.2010.海拉尔盆地火山碎屑岩的成岩作用［J］.岩石学报，26(1):47-54.戴启德，纪友亮.1996.油气储集层地质学［M］.山东东营：中国石油大学出版社，44-63.戴亚权，罗静兰，林潼，等.2007.松辽盆地北部升平气田营城组火山岩储集层特征与成岩演化［J］.中国地质，34(3):528-535.郝惠，漆家福，周建勋，等.2011.塔木查格盆地南贝尔凹陷构造特征［J］.科技导报，29(9):31-35.胡文婷，柳成志，赵辉，等.2011.徐家围子断陷火山岩成岩作用与储集层质量［J］.科学技术与工程，11(6):1176-1181.黄思静，武文慧，刘洁，等.2003.大气水在碎屑岩次生孔隙形成中的作用：以鄂尔多斯盆地三叠系延长组为例［J］.地球科学（中国地质大学学报），28(4):419-424.黄玉龙，王璞珺，邵锐.2010.火山碎屑岩的储集层物性：以松辽盆地营城组为例［J］.吉林大学学报（地球科学版），40(2):227-236.纪友亮，曹瑞成，蒙启安，等.2009.塔木察格盆地塔南凹陷下白垩统层序结构特征及控制因素分析［J］.地质学报，83(6):827-835.李春柏，张新涛，刘立，等.2006.布达特群热流体活动及其对火山碎屑岩的改造作用：以海拉尔盆地贝尔凹陷为例［J］.吉林大学学报（地球科学版），36(2):221-226.刘立，杨庆杰，于均民.1999.大气水—砂岩的相互作用［J］.世界地质，18(2):47-52.刘孟慧，赵澄林.1993.碎屑岩储集层成岩演化模式［M］.山东东营：中国石油大学出版社，8-30.蒙启安，刘立，曲希玉，等.2010.贝尔凹陷与塔南凹陷下白垩统铜钵庙组—南屯组油气储集层特征及孔隙度控制作用［J］.吉林大学学报（地球科学版），40(6):1232-1240.欧成华，董兆雄，魏学斌.2011.柴达木盆地干柴沟—咸水泉地区中—深层成岩演化及其对储集体性能的影响［J］.古地理学报，13(1):85-96.彭晓蕾，曾祥鹏，洪雪.2010.拉布达林盆地上库力组火山碎屑岩成岩作用特征［J］.吉林大学学报（地球科学版），40(4):961-970.邱隆伟，姜在兴.2006.陆源碎屑岩的碱性成岩作用［M］.北京：地质出版社，1-7.曲希玉，刘立，蒙启安，等.2012.大气水对火山碎屑岩改造作用的研究：以塔木查格盆地为例［J］.石油实验地质，34(3):285-290.单敬福，纪友亮，潘仁芳.2011.塔贝尔凹陷南屯组二段沉积体系平面展布特征［J］.海洋地质与第四纪地质，31(3):93-100.孙善平，刘永顺，钟蓉，等.2001.火山碎屑岩分类评述及火山沉积学研究展望［J］.岩石矿物学杂志，20(3):313-317.谭先锋，田景春，李祖兵，等.2010.碱性沉积环境下碎屑岩的成岩演化：以山东东营凹陷陡坡带沙河街组四段为例［J］.地质通报，29(4):535-543.王琪，史基安，薛莲花，等.1999.碎屑储集岩成岩演化过程中流体—岩石相互作用特征［J］.沉积学报，17(4):584-590.许建华，张世奇，纪友亮.2001.藏北羌塘盆地中上侏罗统碎屑岩储集层成岩演化特征［J］.石油大学学报（自然科学版），25(1):4-8.杨森楠，杨巍然.1985.中国区域大地构造学［M］.北京：地质出版社，1-341.应凤祥，罗平，何东博.2004.中国含油气盆地碎屑岩储集层成岩作用与成岩数值模拟［M］.北京：石油工业出版社，91-100.于振峰，程日辉，赵小青，等.2012.海拉尔盆地乌尔逊—贝尔凹陷下白垩统火山碎屑岩成岩作用类型及序列［J］.地球科学（中国地质大学学报），37(4):851-859.袁静，张善文，乔俊，等.2007.东营凹陷深层溶蚀孔隙的多重介质成因机理和动力机制［J］.沉积学报，25(6):840-846.曾溅辉.2000.东营凹陷热流体活动及其对水岩相互作用的影响［J］.地球科学（中国地质大学学报），25(2):138-142.张鼎，田作基，吴胜华，等.2008.川西须家河组储集层成岩演化［J］.岩石学报，24(9):2179-2184.张丽媛，纪友亮，刘立，等.2012.火山碎屑岩储集层异常高孔隙成因：以南贝尔凹陷东次凹北洼槽为例［J］.石油学报，33(5):814-821.张善文，袁静，隋风贵，等.2008.东营凹陷北部沙河街组四段深部储集层多重成岩环境及演化模式［J］.地球科学，43(3):576-587.周瑶琪，周振柱，陈勇，等.2011.东营凹陷民丰地区深部储集层成岩环境变化研究［J］.地学前缘，18(2):268-276.Atilla Aydin.2000.Fractures，faults，and hydrocarbon entrapment，migration and flow［J］.Marine and Petroleum Geology，17(7):797-814.Beard D C，Weyl P K.1973.Influence of texture on porosity and permeablility of unconsolidated sand［J］.AAPG Bulletin，57(2):349-369.Bloch S，Franks S G.1993.Preservation of shallow plagioclase dissolution porosity during burial implications for porosity prediction and aluminum mass balance［J］.AAPG Bulletin，77(9):1488-1501.Charlotte Vinchon，Denis Giot，Fabienne Orsag-Sperber， et al.1996.Changes in reservoir quality determined from the diagenetic evolution of Triassic and Lower Lias sedimentary successions(Balazuc borehole，Ardèche，France)［J］.Marine and Petroleum Geology，13(6):689-694.El-ghali M A K ，Tajori K G，Mansurbeg H， et al.2006.Origin and timing of siderite cementation in Upper Ordovician glaciogenic sandstones from the Murzuq basin，SW Libya［J］.Marine and Petroleum Geology，23(4):459-471.Emery D，Myers K J，Young R.1990.Ancient subaerial exposure and freshwater leaching in sandstones［J］.Geology(Boulder)，18(12):1178-1181.Giles M R.1987.Mass transfer and problems of secondary porosity creation in deeply buried hydrocarbon reservoirs［J］.Marine and Petroleum Geology，4(3):188-204.Knut B，Mogens R，Girish C S.1989.Sandstone diagenesis and porosity modification during basin evolution［J］.Geoiogische Rundschau，78(1):243-268.Lonstaffe F J.1984.The role of meteoric water in diagenesis of shallow sandstone: Stable isotope studies of the Milk River Aquifer and Gas Pool，Southeastern Albert［C］.In: McDonald D A，Surdam R C（eds）.Clastic Diagenesis.AAPG Memoirs，37: 81-98.Luiz Fernando De Ros.1998.Heterogeneous generation and evolution of diagenetic quartzarenites in the Silurian-Devonian Furnas Formation of the Paran Basin，southern Brazil［J］.Sedimentary Geology，116(1-2): 99-128.Shirley P Dutton，Robert G Loucks.2010.Diagenetic controls on evolution of porosity and permeability in lower Tertiary Wilcox sandstones from shallow to ultradeep(200-6700 m)burial，Gulf of Mexico Basin，U.S.A.［J］.Marine and Petroleum Geology，27(1):69-81.Wolela A.2010.Diagenetic evolution of the Ansian-Pliensbachian Adigrat Sandstone，Blue Nile Basin，Ethiopia［J］.Journal of African Earth Sciences，56(1):29-42.
