Difference of mound-bank complex reservoir under different palaeogeographic environment of the Sinian Dengying Formation in Sichuan Basin
Xu Zhe-Hang1,2, Lan Cai-Jun1,2, Hao Fang3, Chen Hao-Ru4, Yang Wei-Qiang1,2, Ma Xiao-Lin2,5, Zou Hua-Yao1,2
1 State Key Laboratory of Petroleum Resources and Prospecting,China University of Petroleum(Beijing),Beijing 102249,China; 2 College of Geosciences,China University of Petroleum(Beijing),Beijing 102249,China; 3 School of Geosciences,China University of Petroleum(East China),Qingdao 266580,China; 4 Faculty of Earth Resources,China University of Geosciences(Wuhan),Wuhan 430074,China; 5 CNOOC Nanhai East Petroleum Bureau,Shenzhen 518067,China
Abstract The mound-bank deposits of the Dengying Formation of the Sinian System are well developed in Sichuan Basin,with good reservoir value. Based on outcrop and core observation,thin section observation,porosity and permeability of samples test,we analyzed the reservoir quality of different mound-bank complexes. During the terminal of Sinian Period,development of the Mianyang-Changning rift affected distribution of sedimentary facies of the 2nd and the 4th Members of Dengying Formation,forming different palaeogeographic units. The high-energy environment,transition environment and low-energy environment of the mound-bank complex rock types are identified,and their reservoir quality is different. The keep-up platform margin mound-bank complex,which is represented by Hujiaba section in the 4th Member of the Dengying Formation mainly deposited high-energy zone rock types. The catch-up platform margin mound-bank complex,which is represented by Yangba section in the 2nd Member of the Dengying Formation,mainly deposited transform zone rock types. The give-up platform interior mound-bank complex,which is represented by Fucheng section in the 4th Member of the Dengying Formation mainly deposited low-energy zone rock types. By comparing reservoir characteristics of three types of mound-bank complex,it is found that the keep-up platform margin mound-bank complex is the‘Sweet spots’ of the Dengying Formation in the Sichuan Basin. The above studies are conducive to find the‘Sweet spots’ of the Sinian Dengying Formation in the Sichuan Basin.
Fund:Co-funded by the Strategic Priority Research Program of the Chinese Academy of Sciences(No. XDA14010306),the National Natural Science Foundation of China(No. U1663210)and the National Science and Technology Major Project(No.2017ZX05005-003-003)
Corresponding Authors:
Zou Hua-Yao,born in 1963,professor,is mainly engaged in petroleum generation and accumulation. E-mail: huayaozou@cup.edu.cn.
About author: Xu Zhe-Hang,born in 1993,Ph.D. candidate,is mainly engaged in carbonate reservoir in the Sichuan Basin. E-mail: xuzhehang93@outlook.com.
Cite this article:
Xu Zhe-Hang,Lan Cai-Jun,Hao Fang et al. Difference of mound-bank complex reservoir under different palaeogeographic environment of the Sinian Dengying Formation in Sichuan Basin[J]. JOPC, 2020, 22(2): 235-250.
Xu Zhe-Hang,Lan Cai-Jun,Hao Fang et al. Difference of mound-bank complex reservoir under different palaeogeographic environment of the Sinian Dengying Formation in Sichuan Basin[J]. JOPC, 2020, 22(2): 235-250.
[1] 陈娅娜,沈安江,潘立银,张杰,王小芳. 2017. 微生物白云岩储集层特征、成因和分布: 以四川盆地震旦系灯影组四段为例. 石油勘探与开发, 44(5): 704-715. [Chen Y N,Shen A J,Pan L Y,Zhang J,Wang X F.2017. Features,origin and distribution of microbial dolomite reservoirs: A case study of 4th Member of Sinian Dengying Formation in Sichuan Basin,SW China. Petroleum Exploration and Development, 44(5): 704-715] [2] 邓胜徽,樊茹,李鑫,张师本,张宝民,卢远征. 2015. 四川盆地及周缘地区震旦(埃迪卡拉)系划分与对比. 地层学杂志, 39(3): 239-254. [Deng S H,Fan R,Li X,Zhang S B,Zhang B M,Lu Y Z.2015. Subdivision and correlation of the Sinian(Ediacaran)System in the Sichuan Basin and its adjacent area. Journal of Stratigraphy, 39(3): 239-254] [3] 杜金虎,汪泽成,邹才能,徐春春,魏国齐,张宝民,杨威,周进高,王铜山,邓胜徽. 2016a. 古老碳酸盐岩大气田地质理论与勘探实践. 北京: 石油工业出版社. [Du J H,Wang Z C,Zou C N,Xu C C,Wei G Q,Zhang B M,Yang W,Zhou J G,Wang T S,Deng S H.2016a. Geologic Theory and Exploration Practice of Ancient Large Carbonates Gas Field .Beijing: Petroleum Industry Press] [4] 杜金虎,汪泽成,邹才能,徐春春,沈平,张宝民,姜华,黄士鹏. 2016b. 上扬子克拉通内裂陷的发现及对安岳特大型气田形成的控制作用. 石油学报, 37(1): 1-16. [Du J H,Wang Z C,Zou C N,Xu C C,Shen P,Zhang B M,Jiang H,Huang S P.2016b. Discovery of intra-cratonic rift in the Upper Yangtze and its control effect on the formation of Anyue giant Gas Field. Acta Petrolei Sinica, 37(1): 1-16] [5] 段金宝,梅庆华,李毕松,梁子锐. 2019. 四川盆地震旦纪—早寒武世构造-沉积演化过程. 地球科学, 44(3): 738-755. [Duan J B,Mei Q H,Li B S,Liang Z R.2019. Sinian-Early Cambrian tectonic-sedimentary evolution in Sichuan Basin. Earth Science, 44(3): 738-755] [6] 范正秀,旷红伟,柳永清,彭楠,朱志才,王玉冲,夏晓旭,陈骁帅,郑行海. 2018. 扬子克拉通北缘中元古界神农架群乱石沟组叠层石类型及其沉积学意义. 古地理学报, 20(4): 545-561. [Fan Z X,Kuang H W,Liu Y Q,Peng N,Zhu Z C,Wang Y C,Xia X X,Chen X S,Zheng H H.2018. Types of stromatolites of the Mesoproterozoic Shennongjia Group in northern margin of Yangtze Craton and their sedimentary significance. Journal of Palaeogeography(Chinese Edition), 20(4): 545-561] [7] 郭旭升,胡东风,段金宝,吴浩,李毕松. 2018. 四川盆地北部宁强胡家坝灯影组四段岩石特征及沉积环境分析. 石油实验地质, 40(6): 749-756. [Guo X S,Hu D F,Duan J B,Wu H,Li B S.2018. Rock features and sedimentary environment of the Fourth Member of Dengying Formation in Hujiaba section of Ningqiang,northern Sichuan Basin. Petroleum Geology and Experiment, 40(6): 749-756] [8] 金民东,谭秀成,李毕松,朱祥,曾伟,连承波. 2019. 四川盆地震旦系灯影组白云岩成因. 沉积学报, 37(3): 443-454. [Jin M D,Tan X C,Li B S,Zhu X,Zeng W,Lian C B.2019. Genesis of dolomite in the Sinian Dengying Formation in the Sichuan Basin. Acta Sedimentologica Sinica, 37(3): 443-454] [9] 兰才俊,徐哲航,马肖琳,胡超,陈浩如,邹华耀. 2019. 四川盆地震旦系灯影组丘滩体发育分布及对储层的控制. 石油学报, 40(9): 1069-1084. [Lan C J,Xu Z H,Ma X L,Hu C,Chen H R,Zou H Y.2019. Development and distribution of mound-shoal complex in the Sinian Dengying Formation,Sichuan Basin and its control on reservoirs. Acta Petrolei Sinica, 40(9): 1069-1084] [10] 李凌,谭秀成,曾伟,周涛,杨雨,洪海涛,罗冰,边立曾. 2013. 四川盆地震旦系灯影组灰泥丘发育特征及储集意义. 石油勘探与开发, 40(6): 666-673. [Li L,Tan X C,Zeng W,Zhou T,Yang Y,Hong H T,Luo B,Bian L Z.2013. Development and reservoir significance of mud mounds in Sinian Dengying Formation,Sichuan Basin. Petroleum Exploration and Development, 40(6): 666-673] [11] 李双建,高平,黄博宇,王海军,沃玉进. 2018. 四川盆地绵阳—长宁凹槽构造演化的沉积约束. 石油与天然气地质, 39(5): 889-898. [Li S J,Gao P,Huang B Y,Wang H J,Wo Y J.2018. Sedimentary constraints on the tectonic evolution of Mianyang-Changning Trough in the Sichuan Basin. Oil & Gas Geology, 39(5): 889-898] [12] 李勇,王兴志,冯明友,曾德铭,谢圣阳,凡睿,王良军,曾韬,杨雪飞. 2019. 四川盆地北部及周缘地区震旦系灯影组二段、四段储集层特征及成因差异. 石油勘探与开发, 46(1): 52-64. [Li Y,Wang X Z,Feng M Y,Zeng D M,Xie S Y,Fan R,Wang L J,Zeng T,Yang X F.2019. Reservoir characteristics and genetic differences between the Second and Fourth Members of Sinian Dengying Formation in northern Sichuan Basin and its surrounding areas. Petroleum Exploration and Development, 46(1): 52-64] [13] 李智武,冉波,肖斌,宋金民,郑玲,李金玺,王瀚,肖斌,叶玥豪,蔡其新,刘树根. 2019. 四川盆地北缘震旦纪—早寒武世隆—坳格局及其油气勘探意义. 地学前缘, 26(1): 59-85. [Li Z W,Ran B,Xiao B,Song J M,Zheng L,Li J X,Wang H,Xiao B,Ye Y H,Cai Q X,Liu S G.2019. Sinian to Early Cambrian uplift-depression framework along the northern margin of the Sichuan Basin,central China and its implications for hydrocarbon exploration. Earth Science Frontiers, 26(1): 59-85] [14] 林孝先,彭军,闫建平,侯中健. 2015. 四川盆地震旦系灯影组葡萄状白云岩成因讨论. 古地理学报, 17(6): 755-770. [Lin X X,Peng J,Yan J P,Hou Z J.2015. A discussion about origin of botryoidal dolostone of the Sinian Dengying Formation in Sichuan Basin. Journal of Palaeogeography(Chinese Edition), 17(6): 755-770] [15] 林孝先,彭军,侯中健,韩浩东,李旭杰,马春疆. 2018. 四川汉源—峨边地区上震旦统灯影组藻白云岩特征及成因研究. 沉积学报, 36(1): 57-71. [Lin X X,Peng J,Hou Z J,Han H D,Li X J,Ma C J.2018. Study on characteristics and geneses of algal dolostone of the Upper Sinian Dengying Formation in the Hanyuan-Ebian area of Sichuan Province,China. Acta Sedimentologica Sinica, 36(1): 57-71] [16] 刘静江,李伟,张宝民,周慧,袁晓红,单秀琴,张静,邓胜徽,谷志东,樊茹,王拥军,李鑫. 2015. 上扬子地区震旦纪沉积古地理. 古地理学报, 17(6): 735-753. [Liu J J,Li W,Zhang B M,Zhou H,Yuan X H,Shan X Q,Zhang J,Deng S H,Gu Z D,Fan R,Wang Y J,Li X.2015. Sedimentary palaeogeography of the Sinian in Upper Yangtze region. Journal of Palaeogeography(Chinese Edition), 17(6): 735-753] [17] 刘静江,张宝民,周慧,单秀琴,王拥军,张静. 2016. 灰泥丘系统分类及石油地质特征. 北京: 石油工业出版社. [Liu J J,Zhang B M,Zhou H,Shan X Q,Wang Y J,Zhang J.2016. Mud Mound Systems Classificition and Petroleum Geological Features .Beijing: Petroleum Industry Press] [18] 刘树根,宋金民,罗平,Qing H,林彤,孙玮,李智武,王浩,彭瀚霖,余永强,龙翼,万元博. 2016. 四川盆地深层微生物碳酸盐岩储层特征及其油气勘探前景. 成都理工大学学报(自然科学版), 43(2): 129-152. [Liu S G,Song J M,Luo P,Qing H,Lin T,Sun W,Li Z W,Wang H,Peng H L,Yu Y Q,Long Y,Wan Y B.2016. Characteristics of microbial carbonate reservior and its hydrocarbon exploring outlook in the Sichuan Basin,China. Journal of Chengdu University of Technology(Science &Technology Edition), 43(2): 129-152] [19] 罗冰,杨跃明,罗文军,文龙,王文之,陈康. 2015. 川中古隆起灯影组储层发育控制因素及展布. 石油学报, 36(4): 416-426. [Luo B,Yang Y M,Luo W J,Wen L,Wang W Z,Chen K.2015. Controlling factors and distribution of reservoir development in Dengying Formation of paleo-uplift in central Sichuan Basin. Acta Petrolei Sinica, 36(4): 416-426] [20] 罗平,王石,李朋威,宋金民,金廷福,王果谦,杨式升. 2013. 微生物碳酸盐岩油气储层研究现状与展望. 沉积学报, 31(5): 807-823. [Luo P,Wang S,Li P W,Song J M,Jin T F,Wang G Q,Yang S S.2013. Review and prospectives of microbial carbonate reservoirs. Acta Sedimentologica Sinica, 31(5): 807-823] [21] 梅冥相,周鹏,张海,陈永红,聂瑞贞. 2006. 上扬子区震旦系层序地层格架及其形成的古地理背景. 古地理学报, 8(2): 219-231. [Mei M X,Zhou P,Zhang H,Chen Y H,Nie R Z.2006. Sequence stratigraphic framework and its palaeogeographical background for the Sinian of Upper Yangtze region. Journal of Palaeogeography(Chinese Edition), 8(2): 219-231] [22] 梅冥相,孟庆芬,刘智荣. 2007. 微生物形成的原生沉积构造研究进展综述. 古地理学报, 9(4): 353-367. [Mei M X,Meng Q F,Liu Z R.2007. Overview of advances in studies of primary sedimentary structures formed by microbes. Journal of Palaeogeography(Chinese Edition), 9(4): 353-367] [23] 梅冥相,Latif K,刘丽,孟庆芬. 2019. 光合作用生物膜建造的凝块: 来自于辽东半岛芙蓉统长山组凝块石生物丘中的一些证据. 古地理学报, 21(2): 254-277. [Mei M X,Latif K,Liu L,Meng Q F.2019. Clots built by photosynthetic biofilms: Evidences from thrombolite bieherms of the Changshan Formation of Cambrian Furongian in Liaodong Peninsula. Journal of Palaeogeography(Chinese Edition), 21(2): 254-277] [24] 彭瀚霖,刘树根,宋金民,孙玮,丁一,尹柯惟. 2014. 川北米仓山地区灯影组微生物碳酸盐岩发育特征. 成都理工大学学报(自然科学版), 41(2): 181-191. [Peng H L,Liu S G,Song J M,Sun W,Ding Y,Yin K W.2014. Characteristics of microbial carbonate rocks in Upper Sinian Dengying Formation of Micang Mountains,North Sichuan,China. Journal of Chengdu University of Technology(Science &Technology Edition), 41(2): 181-191] [25] 单秀琴,张静,张宝民,刘静江,周慧,王拥军,傅卓文. 2016. 四川盆地震旦系灯影组白云岩岩溶储层特征及溶蚀作用证据. 石油学报, 37(1): 17-29. [Shan X Q,Zhang J,Zhang B M,Liu J J,Zhou H,Wang Y J,Fu Z W.2016. Dolomite karst reservoir characteristics and dissolution evidences of Sinian Dengying Formation,Sichuan Basin. Acta Petrolei Sinica, 37(1): 17-29] [26] 沈骋,谭秀成,周博,李凌,曾伟,陈虹宇,苏成鹏,施开兰. 2016. 川北旺苍唐家河剖面仙女洞组灰泥丘沉积特征及造丘环境分析. 地质论评, 62(1): 202-214. [Shen C,Tan X C,Zhou B,Li L,Ceng W,Chen H Y,Su C P,Shi K L.2016. Construction of mud mounds and their forming models of Xiannüdong Formation in Tangjiahe section of Wangcang,North Sichuan. Geological Review, 62(1): 202-214] [27] 唐玄,刘树根,宋金民,李智武,余永强,龙翼,昝博文,赵聪. 2018. 四川盆地东北缘灯影组核形石特征及环境意义. 沉积学报, 36(2): 232-242. [Tang X,Liu S G,Song J M,Li Z W,Yu Y Q,Long Y,Zan B W,Zhao C.2018. Characteristics and environmental significance of the Sinian Dengying Formation oncoids in the northeastern Sichuan Basin. Acta Sedimentologica Sinica, 36(2): 232-242] [28] 王良军. 2019. 川北地区灯影组四段优质储层特征及控制因素. 岩性油气藏, 31(2): 35-45. [Wang L J.2019. Characteristics and controlling factors of high-quality reservoirs of the Fourth Member of Dengying Formation in Northern Sichuan Basin. Lithologic Reservoirs, 31(2): 35-45] [29] 王文之,杨跃明,文龙,罗冰,罗文军,夏茂龙,孙赛男. 2016. 微生物碳酸盐岩沉积特征研究:以四川盆地高磨地区灯影组为例. 中国地质, 43(1): 306-318. [Wang W Z,Yang Y M,Wen L,Luo B,Luo W J,Xia M L,Sun S N.2016. A study of sedimentary characteristics of microbial carbonate: A case study of the Sinian Dengying Formation in Gaomo area,Sichuan Basin. Geology in China, 43(1): 306-318] [30] 魏国齐,杨威,杜金虎,徐春春,邹才能,谢武仁,曾富英,武赛军. 2015. 四川盆地震旦纪—早寒武世克拉通内裂陷地质特征. 天然气工业, 35(1): 24-35. [Wei G Q,Yang W,Du J H,Xu C C,Zou C N,Xie W R,Ceng F Y,Wu S J.2015. Geological characteristics of the Sinian-Early Cambrian intracratonic rift,Sichuan Basin. Natural Gas Industry, 35(1): 24-35] [31] 吴亚生,姜红霞,虞功亮,刘丽静. 2018. 微生物岩的概念和重庆老龙洞剖面P-T界线地层微生物岩成因. 古地理学报, 20(5): 737-775. [Wu Y S,Jiang H X,Yu G L,Liu L J.2018. Conceptions of microbialites and origin of the Permian-Triassic boundary microbialites from Laolongdong,Chongqing,China. Journal of Palaeogeography(Chinese Edition), 20(5): 737-775] [32] 武赛军,魏国齐,杨威,谢武仁,曾富英. 2016. 四川盆地桐湾运动及其油气地质意义. 天然气地球科学, 27(1): 60-70. [Wu S J,Wei G Q,Yang W,Xie W R,Zeng F Y.2016. Tongwan movement and its geologic significances in Sichuan Basin. Natural Gas Geoscience, 27(1): 60-70] [33] 邢凤存,侯明才,林良彪,徐胜林,胡华蕊. 2015. 四川盆地晚震旦世—早寒武世构造运动记录及动力学成因讨论. 地学前缘, 22(1): 115-125. [Xing F C,Hou M C,Lin L B,Xu S L,Hu H R.2015. The records and its dynamic genesis discussion of tectonic movement during the Late Sinian and the Early Cambrian of Sichuan Basin. Earth Science Frontiers, 22(1): 115-125] [34] 邢凤存,陆永潮,郭彤楼,李思田,侯明才,胡华蕊,吴嗣跃. 2017. 碳酸盐岩台地边缘沉积结构差异及其油气勘探意义:以川东北早三叠世飞仙关期台地边缘带为例. 岩石学报, 33(4): 1305-1316. [Xing F C,Lu Y C,Guo T L,Li S T,Hou M C,Hu H R,Wu S Y.2017. Sedimentary texture diversity of different carbonate platform margins and its significance for petroleum exploration: A case study of carbonate platform margins in Feixianguan Period of the Early Triassic,NE Sichuan Basin,China. Acta Petrologica Sinica, 33(4): 1305-1316] [35] 徐哲航,兰才俊,杨伟强,诸丹诚,马肖琳,邹华耀. 2018. 四川盆地震旦系灯影组微生物丘沉积演化特征. 大庆石油地质与开发, 37(2): 15-25. [Xu Z H,Lan C J,Yang W Q,Zhu D C,Ma X L,Zou H Y.2018. Sedimentary characteristics of microbial mound in Sinian Dengying Formation,Sichuan Basin. Petroleum Geology & Oilfield Development in Daqing, 37(2): 15-25] [36] 徐哲航,兰才俊,马肖琳,胡超,陈浩如,李平平,邹华耀. 2019. 四川盆地震旦系灯影组丘滩体储层沉积模式与物性特征. 地球科学, DOI: 10.3799/dqkx.2019.138. [Xu Z H,Lan C J,Ma X L,Hu C,Chen H R,Li P P,Zou H Y.2019. Sedimentary models and physical properties of the mound-shoal complex reservoirs in Sinian Dengying Formation,Sichuan Basin. Earth Science,DOI: 10.3799/dqkx.2019.138] [37] 颜佳新,孟琦,王夏,刘志臣,黄恒,陈发垚,郭全鼎. 2019. 碳酸盐工厂与浅水碳酸盐岩台地: 研究进展与展望. 古地理学报, 21(2): 232-253. [Yan J X,Meng Q,Wang X,Liu Z C,Huang H,Chen F Y,Guo Q D.2019. Carbonate factory and carbonate platform: Progress and prospects. Journal of Palaeogeography(Chinese Edition), 21(2): 232-253] [38] 杨跃明,杨雨,杨光,宋家荣,文龙,邓传光,夏茂龙,冉崎,段国彬,罗冰,谢冰. 2019. 安岳气田震旦系、寒武系气藏成藏条件及勘探开发关键技术. 石油学报, 40(4): 493-508. [Yang Y M,Yang Y,Yang G,Song J R,Wen L,Deng C G,Xia M L,Ran Q,Duan G B,Luo B,Xie B.2019. Gas accumulation conditions and key exploration & development technologies of Sinian and Cambrian gas reservoirs in Anyue Gas Field. Acta Petrolei Sinica, 40(4): 493-508] [39] 姚根顺,郝毅,周进高,蒋伟雄,文龙,倪超,潘立银,张建勇. 2014. 四川盆地震旦系灯影组储层储集空间的形成与演化. 天然气工业, 34(3): 31-37. [Yao G S,Hao Y,Zhou J G,Jiang W X,Wen L,Ni C,Pan L Y,Zhang J Y.2014. Formation and evolution of reservoir spaces in the Sinian Dengying Fm of the Sichuan Basin. Natural Gas Industry, 34(3): 31-37] [40] 张杰,Jones B,潘立银,周进高,秦玉娟,郝毅,武明德. 2014. 四川盆地震旦系灯影组葡萄状白云岩成因. 古地理学报, 16(5): 715-725. [Zhang J,Jones B,Pan L Y,Zhou J G,Qin Y J,Hao Y,Wu M D.2014. Origin of botryoidal dolostone of the Sinian Dengying Formation in Sichuan Basin. Journal of Palaeogeography(Chinese Edition), 16(5): 715-725] [41] 张静,张宝民,单秀琴. 2014. 古气候与古海洋对碳酸盐岩储集层发育的控制. 石油勘探与开发, 41(1): 121-128. [Zhang J,Zhang B M,Shan X Q.2014. Controlling effects of paleo-climate and paleo-ocean on formation of carbonate reservoirs. Petroleum Exploration and Development, 41(1): 121-128] [42] 张荫本,唐泽尧,陈季高. 1996. 粘结岩分类及应用. 天然气勘探与开发, 19(4): 24-33. [Zhang Y B,Tang Z Y,Chen J G.1996. Bond rock classification and application. Natural Gas Exploration and Development, 19(4): 24-33] [43] 赵东方,胡广,张文济,王利超,李飞,谭秀成,连承波. 2018. 渝北巫溪鱼鳞剖面灯影组鲕粒沉积特征及其地质意义. 地质论评, 64(1): 191-202. [Zhao D F,Hu G,Zhang W J,Wang L C,Li F,Tan X C,Lian C B.2018. Sedimentary characteristics of ooids of Sinian(Ediacaran)Dengying Formation on the Yulin section in Wuxi,Chongqing,and geological implications. Geological Review, 64(1): 191-202] [44] 朱东亚,金之钧,张荣强,张殿伟,何治亮,李双建. 2014. 震旦系灯影组白云岩多级次岩溶储层叠合发育特征及机制. 地学前缘, 21(6): 335-345. [Zhu D Y,Jin Z J,Zhang R Q,Zhang D W,He Z L,Li S J.2014. Characteristics and developing mechanism of Sinian Dengying Formation dolomite reservoir with multi-stage karst. Earth Science Frontiers, 21(6): 335-345] [45] 曾富英,杨威,孙爱,金惠,谢武仁,马石玉,苏楠. 2017. 四川盆地川中地区震旦系灯影组台地边缘相带地震识别及其分段特征. 石油与天然气地质, 38(6): 1079-1086. [Zeng F Y,Yang W,Sun A,Jin H,Xie W R,Ma S Y,Su N.2017. Seismic recognition and zonation of the platform margin facies of the Sinian Dengying Formation in central Sichuan Basin. Oil & Gas Geology, 38(6): 1079-1086] [46] 邹才能,杜金虎,徐春春,汪泽成,张宝民,魏国齐,王铜山,姚根顺,邓胜徽,刘静江,周慧,徐安娜,杨智,姜华,谷志东. 2014. 四川盆地震旦系—寒武系特大型气田形成分布、资源潜力及勘探发现. 石油勘探与开发, 41(3): 278-293. [Zou C N,Du J H,Xu C C,Wang Z C,Zhang B M,Wei G Q,Wang T S,Yao G S,Deng S H,Liu J J,Zhou H,Xu A N,Yang Z,Jiang H,Gu Z D.2014. Formation,distribution,resource potential and discovery of the Sinian-Cambrian giant gas field,Sichuan Basin,SW China. Petroleum Exploration and Development, 41(3): 278-293] [47] Al-Siyabi H A.2005. Exploration history of the Ara intrasalt carbonate stringers in the South Oman Salt Basin. GeoArabia, 10(4): 39-72. [48] Andres M S,Pamela R R.2006. Growth morphologies of modern marine stromatolites: A case study from Highborne Cay,Bahamas. Sedimentary Geology, 185(3-4): 319-328. [49] Bosak T,Liang B,Sim M S,Petroff A P,Hoffman P F.2009. Morphological record of oxygenic photosynthesis in conical stromatolites. Proceedings of the National Academy of Sciences of the United States of America, 106(27): 10939-10943. [50] Ding Y,Chen D Z,Zhou X Q,Guo C,Huang T Y,Zhang G J.2019. Cavity-filling dolomite speleothems and submarine cements in the Ediacaran Dengying microbialites,South China: Responses to high-frequency sea-level fluctuations in an'Aragonite-Dolomite Sea'. Sedimentology, 66(6): 2511-2537. [51] Gomez F J,Kah L C,Bartley J K,Astini R A.2014. Microbialites in a high-altitude Andean Lake: Multiple controls on carbonate precipitation and lamina accretion. Palaios, 29(6): 233-249. [52] Grotzinger J,Al-Rawahi Z.2014. Depositional facies and platform architecture of microbialite-dominated carbonate reservoirs,Ediacaran-Cambrian Ara Group,Sultante of Om. AAPG Bulletin, 98(8): 1453-1494. [53] Grotzinger J P,Knoll A H.1999. Stromatolites in Precambrian carbonates: Evolutionary mileposts or environmental dipsticks?Annual Review of Earth and Planetary Sciences, 27(1): 313-358. [54] Harwood C L,Sumner D Y.2012. Origins of microbial microstructures in the Neoproterozoic Beck Spring dolomite: Variations in microbial community and timing of lithification. Journal of Sedimentary Research, 82(9): 709-722. [55] Hillgärtner H,Strasser A.2003. Quantification of high-frequency sea-level fluctuations in shallow-water carbonates: An example from the Berriasian-Valanginian(French Jura). Palaeogeography,Palaeoclimatology,Palaeoecology, 200(1-4): 43-63. [56] Hood A V S,Wallace M W.2018. Neoproterozoic marine carbonates and their paleoceanographic significance. Global and Planetary Change, 160: 28-45. [57] Hood A V S,Wallace M W,Reed C P,Hoffmann K H,Freyer E E.2015. Enigmatic carbonates of the Ombombo Subgroup,Otavi Fold Belt,Namibia: A prelude to extreme cryogenian anoxia?Sedimentary Geology, 324: 12-31. [58] Hu M Y,Gao D,Wei G Q,Yang W,Xie W R,Wang X.2019. Sequence stratigraphy and facies architecture of a mound-shoal-dominated dolomite reservoir in the Late Ediacaran Dengying Formation,central Sichuan Basin,SW China. Geological Journal, 54(3): 1653-1671. [59] Jahnert R J,Collins L B.2011. Significance of subtidal microbial deposits in Shark Bay,Australia. Marine Geology, 286(1-4): 106-111. [60] Jahnert R J,Collins L B.2012. Characteristics,distribution and morphogenesis of subtidal microbial systems in Shark Bay,Australia. Marine Geology, 303-306: 115-136. [61] Kennard J M,James N P.1986. Thrombolites and stromatolites: Two distinct types of microbial structures. Palaios, 1(5): 492-503. [62] Muniz M C,Bosence D W J. 2015. Pre-salt microbialites from the Campos Basin(offshore Brazil): Image log facies,facies model and cyclicity in lacustrine carbonates. In: Bosence D W J,Gibbons K A,LeHeron D P,Morgan W A,Pritchard T,Vining B A(eds). Microbial Carbonates in Space and Time: Implications for Global Exploration and Production. Geological Society,London,Special Publications: 221-242. [63] Riding R.2000. Microbial carbonates: The geological record of calcified bacterial-algal mats and biofilms. Sedimentology,47(s1): 179-214. [64] Riding R.2006. Cyanobacterial calcification,carbon dioxide concentrating mechanisms,and Proterozoic-Cambrian changes in atmospheric composition. Geobiology, 4(4): 299-316. [65] Su D C,Sun A P.2012. Typical earthquake-induced soft-sediment deformation structures in the Mesoproterozoic Wumishan Formation,Yongding River Valley,Beijing,China and interpreted earthquake frequency. Journal of Palaeogeography, 1(1): 71-89. [66] Smodej J,Reuning L,Becker S,Kukla A P.2019. Micro- and nano-pores in intrasalt,microbialite-dominated carbonate reservoirs,Ara Group,South-Oman salt basin. Marine and Petroleum Geology, 104: 389-403. [67] Wang G Z,Liu S G,Ma Y S,Xu G S,Cai X Y.2010. Characteristics of subaerial karstification and late reconstruction in the Dengying Formation,Sichuan Basin,southwestern China. Journal of Earth Science, 21(3): 290-302.
