Progress and present research on volcanic-hydrothermal related fine-grained sedimentary rocks
Li Zhe-Xuan1, Liu Yi-Qun1, Jiao Xin1, Zhou Ding-Wu2, Yang Yi-Yao1, You Ji-Yuan1
1 State Key Laboratory of Continental Dynamics, Department of Geology,Northwest University,Xi’an 710069,China; 2 College of Earth Science and Engineering, Shandong University of Science and Technology,Qingdao 266510,China
Abstract：Continental fine-grained sedimentary rocks are important source rocks and tight oil-bearing rocks in continental petroliferous basins of China. In recent years,lots of significant progress and promising front research have been conducted due to continuous working on source rock,tight oil and gas. This paper reviewed the domestic and overseas existing research of fine-grained sedimentary rocks,and then discussed their evolution of basic concepts,petrological, mineralogical characteristics, forming mechanisms and classification approachs. According to recent literatures and reports,there distributes abundant volcanic-hydrothermal material in fine-grained sedimentary rocks which develop in intracontinental rift environment. Thus,studying the source of deep-derived clastics and hydrothermal fluids under intracontinental extensional environment,as well as how do they influence depositional process seems to be extremely necessary. This paper considered volcanic and hydrothermal exhalative material not only took a part in deposition and diagenesis processes,but also involved with hydrocarbon generation in terrestrial dark fine-grained rocks. Further studying on terrestrial fine-grained sedimentary rocks will benefit completing and enriching theories of sedimentation and petroleum generation in continental petroliferous basins. Consequently,tight oil and shale oil-gas exploration and development can be better instructed.
Li Zhe-Xuan,Liu Yi-Qun,Jiao Xin et al. Progress and present research on volcanic-hydrothermal related fine-grained sedimentary rocks[J]. JOPC, 2019, 21(5): 727-742.
[1] 常海亮,郑荣才,郭春利,文华国. 2016. 准噶尔盆地西北缘风城组喷流岩稀土元素地球化学特征. 地质论评, 62(3): 550-568. [Chang H L,Zheng R C,Guo C L,Wen H G.2016. Characteristics of rare earth elements of exhalative rock in Fengcheng Fomation,northwestern margin of Jungger Basin. Geological Review, 62(3): 550-568] [2] 陈彬滔,潘树新,王天奇,张庆石,梁苏娟,刘彩燕. 2015. 松辽盆地齐家—古龙凹陷青山口组深水细粒沉积体系的微相类型及其页岩油气勘探意义. 中南大学学报(自然科学版), 46(9): 3338-3345. [Chen B T,Pan S X,Wang T Q,Zhang Q S,Liang S J,Liu C Y.2015. Sedimentary microfacies of deepwater fine-grained depositional system and its significance for shale oil and gas exploration in Qingshankou Formation,Qijia-Gulong depression,Songliao Basin,Northeast China. Journal of Central South University(Science and Technology), 46(9): 3338-3345] [3] 陈世悦,张顺,王永诗,谭明友. 2016. 渤海湾盆地东营凹陷古近系细粒沉积岩岩相类型及储集层特征. 石油勘探与开发, 43(2): 198-205. [Chen S Y,Zhang S,Wang Y S,Tan M Y.2016. Lithofacies types and reservoirs of Paleogene fine-grained sedimentary rocks in Dongying Sag,Bohai Bay Basin. Petroleum Exploration and Development, 43(2): 198-205] [4] 陈世悦,张顺,刘惠民,鄢继华. 2017. 湖相深水细粒物质的混合沉积作用探讨. 古地理学报, 19(2): 271-284. [Chen S Y,Zhang S,Liu H M,Yan J H.2017. Discussion on mixing of fine-grained sediments in lacustrine deep water. Journal of Palaeogeography(Chinese Edition), 19(2): 271-284] [5] 董桂玉,陈洪德,何幼斌,秦志勇,罗进雄,辛长静. 2007. 陆源碎屑与碳酸盐混合沉积研究中的几点思考. 地球科学进展, 22(9): 931-939. [Dong G Y,Chen H D,He Y B,Qin Z Y,Luo J X,Xin C J.2007. Some problems on the study of the mixed Silicilastic-Carbonate sediments. Advances in Earth Science, 22(9): 931-939] [6] 冯乔,柳益群,郝建荣. 2004. 三塘湖盆地芦草沟组烃源岩及其古环境. 沉积学报, 22(3): 513-517. [Feng Q,Liu Y Q,Hao J R.2004. The source rock and its palaeo-environment of Lucaogou Formation,Permian in Santanghu Basin. Acta Sedimentologica Sinica, 22(3): 513-517] [7] 高岗,梁浩,沈霞,焦立新,李华明. 2009. 三塘湖盆地二叠系火成岩分布及其对烃源岩热演化的影响. 石油实验地质, 31(5): 462-465. [Gao G,Liang H,Shen X,Jiao L X,Li M H.2009. Permian igneous rock distribution and its influence to the thermal evolution of source rock in Santanghu Basin. Petroleum Geology & Experiment, 31(5): 462-465] [8] 郭占谦,王先彬. 1994. 松辽盆地非生物成因气的探讨. 中国科学(B辑), 24(3): 303-309. [Guo Z Q,Wang X B.1994. Disscussion: Abiogenic hydrocarbon gases from the Songliao. Science in China(Series B), 24(3): 303-309] [9] 贺聪,吉利明,苏奥,刘颖,李剑锋,吴远东,张明震. 2017. 鄂尔多斯盆地南部延长组热水沉积作用与烃源岩发育的关系. 地学前缘, 24(6): 277-285. [He C,Ji L M,Su A,Liu Y,Li J F,Wu Y D,Zhang M Z.2017. Relationship between hydrothermal sedimentation process and source rock development in the Yanchang formation,south Ordos Basin. Earth Science Frontiers, 24(6): 277-285] [10] 侯增谦,韩发,夏林圻. 2003. 现代与古代海底热水成矿作用. 北京: 地质出版社,293-309. [Hou Z Q,Han F,Xia L X.2003. Modern and Ancient Seabed Hot Water Mineralization. Beijing: Geological Publishing House,293-309] [11] 贾承造,邹才能,杨智,朱如凯,陈竹新,张斌,姜林. 2018. 陆相石油地质理论在中国中西部盆地的重大进展. 石油勘探与开发, 45(4): 546-560. [Jia C Z,Zou C N,Yang Z,Zhu R K,Chen Z X,Zhang B,Jiang L.2018. Significant progress of continental petroleum geology theory in basins of Central and Western China. Petroleum Exploration and Development, 45(4): 546-560] [12] 贾智彬,侯读杰,孙德强,姜玉涵,赵喆,张自鸣,洪梅,畅哲,董立成. 2018. 热水沉积区黑色页岩稀土元素特征及其地质意义: 以贵州中部和东部地区下寒武统牛蹄塘组页岩为例. 天然气工业, 38(5): 45-49. [Jia Z B,Hou D J,Sun D Q,Jiang Y H,Zhao Z,Zhang Z M,Hong M,Chang Z,Dong L C.2018. Characteristics and geological implications of rare earth elements in black shale in hydrothermal sedimentation areas: A case study from the Low Cambrian Niutitang Fm shale in central and eastern Guizhou. Natural Gas Industry, 38(5): 45-49] [13] 姜在兴. 2010. 沉积学. 北京: 石油工业出版社,93-95. [Jiang Z X.2010. Sedimentology. Beijing: Petroleum Industry Press,93-95] [14] 姜在兴,梁超,吴靖,张建国,张文昭,王永诗,刘惠民,陈祥. 2013. 含油气细粒沉积岩研究的几个问题. 石油学报, 34(6): 1031-1039. [Jiang Z X,Liang C,Wu J,Zhang J G,Zhang W Z,Wang Y S,Liu H M,Chen X.2013. Several issues in sedimentological studies on hydrocarbon-bearing fine-grained sedimentary rocks. Acta Petrolei Sinica, 34(6): 1031-1039] [15] 蒋宜勤,柳益群,杨召,南云,王睿,周鹏,杨焱钧,寇均益,周宁超. 2015. 准噶尔盆地吉木萨尔凹陷凝灰岩型致密油特征与成因. 石油勘探与开发, 42(6): 741-749. [Jiang Y Q,Liu Y Q,Yang Z,Nan Y,Wang R,Zhou P,Yang Y J,Kou J Y,Zhou N C.2015. Characteristics and origin of tuff-type tight oil in Jimusar Depression,Junggar Basin,NW China. Petroleum Exploration and Development, 42(6): 741-749] [16] 焦鑫. 2012. 新疆三塘湖盆地二叠系热液喷流岩特征及其对油气的影响. 西北大学硕士学位论文: 15-30. [Jiao X.2012. Characteristics of exhalative hydrothermal rocks and its impaction on oil and gas,Permian,Santanghu Basin,Xinjiang. Master’s Dissertation of Northwest University :15-30] [17] 焦鑫. 2017. 新疆三塘湖盆地二叠系岩浆—热液喷流沉积岩特征与形成机理. 西北大学博士学位论文: 40-60. [Jiao X.2017. Features and forming mechanism of magmatic-hydrothermal exhalative sedimentary rocks in Permian Lucaogou Formation,Santanghu Basin,Xinjiang. Docter’s Dissertation of Northwest University: 40-60] [18] 焦鑫,柳益群,周鼎武,汪双双,南云,周宁超,杨焱钧. 2013. “白烟型”热液喷流岩研究进展. 地球科学进展, 28(2): 221-232. [Jiao X,Liu Y Q,Zhou D W,Wang S S,Nan Y,ZhouN C,Yang Y J.2013. Progress of Research on “White Smoke Type”Exhalative Hydrothermal Rocks. Advance in Earth Science, 28(2): 221-232] [19] 焦鑫,柳益群,杨晚,周鼎武. 2017a. 水下火山喷发沉积特征研究进展. 地球科学进展, 32(9): 926-936. [Jiao X,Liu Y Q,Yang W,Zhou D W.2017a. Progress on sedimentation of subaqueous volcanic eruption. Advances in Earth Science, 32(9): 926-936] [20] 焦鑫,柳益群,靳梦琪,周鼎武. 2017b. 新疆三塘湖薄层状岩浆—热液白云质喷流沉积岩. 沉积学报, 35(6): 2-10. [Jiao X,Liu Y Q,Jin M Q,Zhou D W.2017b. Thin bed magmatic-hydrothermal dolomitic exhalative sedimentary rocks in Santanghu Basin,Xinjiang. Acta Sedimentologica Sinica, 35(6): 26-29] [21] 焦鑫,柳益群,樊婷婷,周鼎武,杨焱钧,张旭. 2017c. 幔源纹层状岩浆—热液喷溢沉积岩. 西北大学学报: 自然科学版, 47(6): 887-895. [Jiao X,Liu Y Q,Fan T T,Zhou D W,Yang Y J,Zhang X.2017c. Mantle-derived laminated magmatic-hydrothermal effusive-eruptive sedimentary rocks. Journal of Northwest University(Natural Science Edition), 47(6): 887-895] [22] 金强,朱光有,王娟. 2008. 咸化湖盆优质烃源岩的形成与分布. 中国石油大学学报(自然科学版), 32(4): 19-23. [Jin Q,Zhu G Y,Wang J.2008. Deposition and distribution of high-potential source rocks in saline lacustrine environments. Journal of China University of Petroleum(Natural Edition), 32(4): 19-23] [23] 李哲萱,柳益群,周鼎武,焦鑫,南云. 2019. 三塘湖盆地二叠系芦草沟组喷爆岩岩石学、矿物学特征及相关问题探讨. 沉积学报, 37(3): 456-463. [Li Z X,Liu Y Q,Zhou D Wu,Jiao X,Nan Y.2019. Petrology and mineralogy features of magmatic-hydrothermal explosion rocks in Permian Lucaogou Formation of Santanghu Basin and its relative discussions. Acta Sedimentologica Sinica, 37(3): 456-463] [24] 柳益群,焦鑫,李红,袁明生,Yang Wan,周小虎,梁浩,周鼎武,郑朝阳,孙芹,汪双双. 2011. 新疆三塘湖跃进沟二叠系地幔热液喷流型原生白云岩. 中国科学: 地球科学, 41(12): 1862-1871. [Liu Y Q,Jiao X,Li H,Yuan M S,Yang W,Zhou X H,Liang H,Zhou D W,Zheng C Y,Sun Q,Wang S S.2011. Permian mantle hydrothermal exhalative primary dolomite in Yuejingou,Santanghu,Xinjiang. Science China: Earth Sciences, 41(12): 1862-1871] [25] 柳益群,周鼎武,焦鑫,南云,杨晚,李红,周小虎. 2013. 一类新型沉积岩: 地幔热液喷积岩: 中国新疆三塘湖地区为例. 沉积学报, 31(5): 773-781. [Liu Y Q,Zhou D W,Jiao X,Nan Y,Yang W,Li H,Zhou X H.2013. A new type of sedimentary rocks: Mantle-originated hydroclastites and hydrothermal exhalites Santanghu area,Xinjiang NW China. Acta Sedimentologica Sinica, 31(5): 773-781] [26] 柳益群,周鼎武,南云,焦鑫,李哲萱,李红,周小虎. 2018. 新疆北部地区二叠系幔源碳酸岩质喷爆岩研究. 古地理学报, 20(1): 49-63. [Liu Y Q,Zhou D W,Nan Y,Jiao X,Li Z X,Li H,Zhou X H.2018. Permian mantle-derived carbonatite originated exhalative sedimentary rocks in North Xinjiang. Journal of Palaeogeography(Chinese Edition), 20(1): 49-63] [27] 马克,侯加根,刘钰铭,史燕青,闫林,陈福利. 2017. 吉木萨尔凹陷二叠系芦草沟组咸化湖混合沉积模式. 石油学报, 38(6): 636-648. [Ma K,Hou J G,Liu Y M,Shi Y Q,Yan L,Chen F L.2017. The sedimentary model of saline lacustrine mixed sedimentation in Permain Lucaogou Formation,Jimsar Sag. Acta Petrolei Sinica, 38(6): 636-648] [28] 潘树新,陈彬滔,刘华清,李相博,赵占银,林铁峰,张庆石. 2014. 陆相湖盆深水底流改造砂: 沉积特征、成因及其非常规油气勘探意义. 天然气地球科学, 25(10): 1577-1585. [Pan S X,Chen B T,Liu H Q,Li X B,Zhao Z Y,Lin T F,Zhang Q S.2014. Deepwater bottom current rework sand(BCRS)in lacustrine basins: Sedimentary characteristics,identification criterion,formation mechanism and its significance for unconventional oil/gas exploration. Natural Gas Geoscience, 25(10): 1577-1585] [29] 庞军刚,李赛,杨友运,刘利军,朱杰,陈栋. 2014. 湖盆深水区细粒沉积成因研究进展: 以鄂尔多斯盆地延长组为例. 石油实验地质, 36(6): 706-711. [Pang J G,Li S,Yang Y Y,Liu L J,Zhu J,Chen D.2014. Study progress of origin of fine-grained sedimentary rocks in deep-water area of lacustrine basin: Taking Yangchang Formation in Ordos Basin as an example. Petroleum Geology & Experiment, 36(6): 706-711] [30] 沙庆安. 2001. 混合沉积和混积岩的讨论. 古地理学报,3(3),63-66. [Sha Q A.Discussion on mixing deposit and Hunji Rock. Journal of Palaeogeography(Chinese Edition), 3(3): 63-66] [31] 孙龙德,方朝亮,李峰,朱如凯,张云辉,袁选俊,贾爱林,高兴军,苏玲. 2015. 油气勘探开发中的沉积学创新与挑战. 石油勘探与开发, 42(2): 129-134. [Sun L D,Fang C L,Li F,Zhu R K,Zhang Y H,Yuan X J,Jia A L,Gao X J,Su L.2015. Innovations and challenges of sedimentology in oil and gas exploration and development. Petroleum Exploration and Development, 42(2): 129-134] [32] 童晓光,郭建宇,王兆明. 2014. 非常规油气地质理论与技术进展. 地学前缘, 21(1): 9-20. [Tong X G,Guo J Y,Wang Z M.2014. The progress of geological theory and technology for unconventional oil and gas. Earth Science Frontiers, 21(1): 9-20] [33] 万从礼,金强,翟庆龙. 2003. 东营凹陷滨南地区水下火山喷溢对烃源岩形成及生烃演化的作用. 中国石油大学学报(自然科学版), 27(3): 17-21. [Wan C L,Jin Q,Zhai Q L.2003. Effect of volcanic activity on generation and evolution of hydrocarbon source rocks in Binnan Area of Dongying Depression. Journal of China University of Petroleum(Edition of Natural Science), 27(3): 17-21] [34] 王书荣,宋到福,何登发. 2013. 三塘湖盆地火山灰对沉积有机质的富集效应及凝灰质烃源岩发育模式. 石油学报, 34(6): 1077-1087. [Wang S R,Song D F,He D F.2013. The enrichment effect of organic materials by volcanic ash in sediments of the Santanghu Basin and the evolutionary pattern of tuffaceous source rocks. Acta Petrolei Sinica, 34(6): 1077-1087] [35] 王先彬,郭占谦,妥进才,郭洪岩,李振西,卓胜广,蒋鸿亮,曾龙伟,张铭杰,王连生,柳春雪,闫宏,李立武,周晓峰,王永莉,杨辉,王广. 2009. 中国松辽盆地商业天然气的非生物成因烷烃气体. 中国科学: 地球科学, 39(5): 602-614. [Wang X B,Guo Z Q,Tuo J C,Guo H Y,Li Z X,Zuo S G, Jiang H L,Zeng L W,Zhang M J,Wang L S,Liu C L,Yan H,Li L W,Zhou X F,Wang Y L,Yang H,Wang G.2009. Abiogenic hydrocarbons in commercial gases from the Songliao,China. Science China-Earth Sciences, 52(2): 213-226] [36] 文华国. 2005. 酒西盆地青西凹陷下沟组湖相“白烟型”喷流岩研究. 成都理工大学硕士学位论文: 26-29. [Wen H G.2005. Study on the “White smoke stype”of lacustrine exhalative rock in the Xiagou formation of Qingxi Sag of Jiuxi Basin. Masteral Dissertation of Chengdu University of Technology: 26-29] [37] 吴靖,姜在兴,梁超. 2017. 东营凹陷沙河街组四段上亚段细粒沉积岩岩相特征及与沉积环境的关系. 石油学报, 38(10): 1110-1122. [Wu J,Jiang Z X,Liang C.2017. Lithofacies characteristics of fine-grained sedimentary rocks in the upper submember of Member 4 of Shahejie Formation,Dongying sag and their relationship with sedimentary environment. Acta Petrolei Sinaca, 38(10): 1110-1122] [38] 肖荣阁,张汉城,陈卉泉,张宗恒. 1994. 热水沉积岩及矿物岩石标志. 地学前缘, 8(4): 379-385. [Xiao R G,Zhang H C,Chen H Q,Zhang Z H.1994. Hydrothermal sedimentary rock and indicators of minerals and rocks. Earth Science Frontiers, 8(4): 379-385] [39] 熊寿生,卢培德. 1996. 火山喷溢—喷流活动与半无机成因天然气的形成和类型. 石油实验地质, 18(1): 13-35. [Xiong S S,Lu P D.1996. Volcanic eruption-effusion and their relationship with the formation and type of semi-inorganic gas. Experimental Petroleum Geology, 18(1): 13-35] [40] 杨朝青,沙庆安. 1990. 云南曲靖中泥盆统曲靖组的沉积环境一种陆源碎屑. 沉积学报, 8(2): 59-66. [Yang C Q,Sha Q A.1990. Sedimentary environment of the Middle Devonian Qujing Formation,Qujing,Yunnan Province: A kind of mixing sedimentation of terrigenous clastics and carbonate. Acta Sedimentologica Sinica, 8(2): 59-66] [41] 杨仁超,尹伟,樊爱萍,A.J.(Tom)van Loon.2017. 鄂尔多斯盆地南部三叠系延长组湖相重力流沉积细粒岩及其油气地质意义. 古地理学报, 19(5): 791-806. [Yang R C,Yin W,Fan A P,van Loon A J.2017. Fine-grained,lacustrine gravity-flow deposits and their hydrocarbon significance in the Triassic Yangchang Formation in southern Ordos Basin. Journal of Palaeogeography(Chinese Edition), 19(5): 791-806] [42] 杨智,侯连华,林森虎,罗霞,张丽君,吴松涛,崔景伟. 2018. 吉木萨尔凹陷芦草沟组致密油、页岩油地质特征与勘探潜力. 中国石油勘探, 23(4): 76-85. [Yang Z,Hou L H,Lin S H,Luo X,Zhang L J,Wu S T,Cui J W.2018. Geologic characteristics and exploration potential of tight oil and shale oil in Lucaogou Formation in Jimsar sag. China Petroleum Exploration, 23(4): 76-85] [43] 袁选俊,林森虎,刘群,姚泾利,王岚,郭浩,邓秀芹,成大伟. 2015. 湖盆细粒沉积特征与富有机质页岩分布模式: 以鄂尔多斯盆地延长组长7油层组为例. 石油勘探与开发, 42(1): 34-43. [Yuan X J,Lin S H,Liu Q,Yao J L,Wang L,Guo H,Deng X Q,Cheng D W.2015. Lacustrine fine-grained sedimentary features and organic-rich shale distribution pattern: A case study of Chang 7 Member of Triassic Yangchang Formation in Ordos Baion,NW China. Petroleum Exploration and Development, 42(1): 34-43] [44] 张景廉,李相博,刘化清. 2013. “石油无机成因说”的理论与实践. 西安石油大学学报(自然科学版), 28(1): 1-11. [Zhang J L,Li X B,Liu H Q.2013. Theory and practice of petroleum inorganic origin. Journal of Xi’an Shiyou University(Natural Science Edition), 28(1): 1-11] [45] 张少敏,操应长,朱如凯,王尉,涂建琪,毛治国,白斌. 2016. 雅布赖盆地小湖次凹细粒沉积岩岩相特征与沉积环境探讨. 天然气地球科学, 27(2): 309-319. [Zhang S M,Cao Y C,Zhu R K,Wang W,Tu J Q,Mao Z G,Bai B.2016. The lithofacies and depositional environment of fine-grained sedimentary rocks of Xiaohu subsag in Yabulai Basin. Natural Gas Geosciences, 27(2): 309-319] [46] 张顺,陈世悦,鄢继华,谭明友,张云银,龚文磊,王光增. 2015. 东营凹陷西部沙三下亚段—沙四上亚段泥页岩岩相及储层特征. 天然气地球科学, 26(2): 320-332. [Zhang S,Chen S Y,Yan J H,Tan M Y,Zhang Y Y,Gong W L,Wang G Z.2015. Characteristics of shale lithofacies and reservoir space in the 3rd and 4th Members of Shahejie Formation,the west of Dongying Sag. Natural Gas Geoscience, 26(2): 320-332] [47] 张文正,杨华,杨奕华,孔庆芬,吴凯. 2008. 鄂尔多斯盆地长7优质烃源岩的岩石学、元素地球化学特征及发育环境. 地球化学, 37(1): 59-64. [Zhang W Z,Yang H,Yang Y H,Kong Q F,Wu K.2008. Petrology and element geochemistry and development environment of Yanchang formation Chang-7 high quality source rocks in Ordos Basin. Geochimica, 37(1): 59-64] [48] 张文正,杨华,彭平安,杨奕华,张辉,石小虎. 2009. 晚三叠世火山活动对鄂尔多斯盆地长7优质烃源岩发育的影响. 地球化学, 38(6): 573-582. [Zhang W Z,Yang H,Peng P A,Yang Y H,Zhang H,Shi X H.2009. The influence of late Triassic volcanism on the development of Chang 7 high grade hydrocarbon source rock in Ordos Basin. Geochimica, 38(6): 573-582] [49] 张文正,杨华,解丽琴,杨奕华. 2010. 湖底热水活动及其对优质烃源岩发育的影响: 以鄂尔多斯盆地长7烃源岩为例. 石油勘探与开发, 37(4): 421-429. [Zhang W Z,Yang H,Xie L Q,Yang Y H.2010. Lake-bottom hydrothermal activities and their influences on the high-quality source rock development: A case from Chang 7 source rocks in Ordos Basin. Petroleum Exploration and Development, 37(4): 421-429] [50] 张文正,杨华,杨伟伟,吴凯,刘飞. 2015. 鄂尔多斯盆地延长组长7湖相页岩油地质特征评价. 地球化学, 44(5): 505-515. [Zhang W Z,Yang H,Yang W W,Wu K,Liu F.2015. Assessment of geological characteristics if lacustrine shale oil reservoir in Chang 7 Member of Yangchang Formation,Ordos Basin. Geochimica, 44(5): 505-515] [51] 张雄华. 2000. 混积岩的分类和成因. 地质科技情报,19(4):31-34. [Zhang X H.2000. Classification and origin of mixsedimentite. Geological Science and Technology Information,19(4):31-34] [52] 赵贤正,蒲秀刚,韩文中,周立宏,时战楠,陈世悦,肖敦清. 2017. 细粒沉积岩性识别新方法与储集层甜点分析: 以渤海湾盆地沧东凹陷孔店组二段为例. 石油勘探与开发, 44(4): 492-502. [Zhao X Z,Pu X G,Han W Z,Zhou L H,Shi Z N,Chen S Y,Xiao D Q.2017. A new method for lithology identification of fine grained deposits and reservoir sweet spot analysis: A case study of Kong 2 Member in Cangdong sag,Bohai Bay Basin,China. Petroleum Exploration and Development, 44(4): 492-502] [53] 郑荣才,王成善,朱利东,刘红军,方国玉,杜文博,王崇孝,汪满福. 2003. 酒西盆地首例湖相“白烟型”喷流岩─热水沉积白云岩的发现及其意义. 成都理工大学学报(自然科学版), 30(1): 1-8. [Zheng R C,Wang C S,Zhu L D,Liu H J,Fang G Y,Du W B,Wang C X,Wang M F.2003. Discovery of the first example of “white smoke type” of exhalative rock(hydrothermal sedimentary dolostone)in jiuxi basin and its significance. Journal of Chengdu University of Technology(Science & Technology Edition), 30(1): 1-8] [54] 郑荣才,文华国,李云,常海亮. 2018. 甘肃酒西盆地青西凹陷下白垩统下沟组湖相喷流岩物质组分与结构构造. 古地理学报, 20(1): 1-18. [Zheng R C,Wen H G,Li Y,Chang H L.2018. Compositions and texture of lacustrine rocks from the Lower Cretaceous Xiagou Formation in Qingxi sag of Jiuxi Basin,Gansu. Journal of Palaeogeography(Chinese Edition), 20(1): 1-18] [55] 钟大康,姜振昌,郭强,孙海涛,杨喆. 2015. 内蒙古二连盆地白音查干凹陷热水沉积白云岩的发现及其地质与矿产意义. 石油与天然气地质, 36(4): 587-595. [Zhong D K,Jiang Z C,Guo Q,Sun H T,Yang Z.2015. Discovery of hydrothermal dolostones in Baiyinchagan sag of Erlian Basin,Inner Mongolia,and its geologic and mineral significance. Oil & Gas Geology, 36(4): 587-595] [56] 钟大康,杨喆,孙海涛,张硕. 2018. 热水沉积岩岩石学特征: 以内蒙古二连盆地白音查干凹陷下白垩统腾格尔组为例. 古地理学报, 20(1): 19-32. [Zhong D K,Yang Z,Sun H T,Zhang S.2018. Petrological characteristics of hydrothermal-sedimentary rocks: A case study of the Lower Cretaceous Tengger Formation in the Baiyinchagan Sag of Erlian Basin,Inner Mongolia. Journal of Palaeogeography(Chinese Edition), 20(1): 19-32] [57] 周中毅,盛国英,闵育顺. 1989. 凝灰质岩生油岩的有机地球化学初步研究. 沉积学报, 7(3): 3-9. [Zhou Z Y,Sheng G Y,Min Y S.1989. A primary study of tuffaceous source rock by organic geochemistry. Acta Sedimentologica Sinica, 7(3): 3-9] [58] 朱国华,张杰,姚根顺,李玉文,王鑫,余朝丰. 2014. 沉火山尘凝灰岩: 一种赋存油气资源的重要岩类: 以新疆北部中二叠统芦草沟组为例. 海相油气地质, 19(1): 1-7. [Zhu G H,Zhang J,Yao G S,Li Y W,Wang X,Yu C F.2014. Sedimentary volcanic dust tuff,an important kind of rock storing hydrocarbon resources: Discussion on the lithology of middle Permian Lucaogou Oil-bearing rocks in the north of Xinjiang. Marine Origin Petroleum Geology, 19(1): 1-7] [59] 邹才能,董大忠,杨桦,王玉满,黄金亮,王淑芳,付成信. 2011. 中国页岩气形成条件及勘探实践. 天然气工业, 31(12): 26-39. [Zou C N,Dong D Z,Yang H,Wang Y M,Huang J L,Wang S F,Fu C X.2011. Formation conditions and exploration practice of shale gas in China. Natural Gas Industry, 31(12): 26-39] [60] Allison M A,Nittrouer C A.1998. Identifying accretionary mud shorefaces in the geologic record: Insights from the modern Amazon dispersal system. P S. mudstones & shales recent progress in shale research. Schweizerbart’sche Verlagsbuchhandlung: 29-38. [61] Aplin A C,Macquaker J S H.2011. Mudstone diversity: Implications for source,seal,and reservior properties in petroleum systems. AAPG Bulletin, 95(12): 2031-2059. [62] Brazelton W J,Schrenk M O,Kelley D S,Baross J A.2006. Methane-and Sulfur-Metabolizing microbial communities dominate the lost city hydrothermal field ecosystem. Applied and Environmental Microbiology, 72(9): 6257-6270. [63] Ghadeer S,Macquaker J H S.2011. Sediment transport processes in an ancient mud-dominated succession: A comparison of processes operating in marine offshore settings and anoxic basinal environments. Journal of the Geological Society, 168: 1121-1132. [64] Hackley P C,Zhang L X,Zhang T W.2017. Organic petrology of peak oil maturity Triassic Yanchang Formation lacustrine mudrocks,Ordos Basin,China. Interpretation, 5(2): 211-223. [65] Helena G D,Camron K M,Richard L.2013. Score: A mineralogy based classification scheme for organic mudstones. Proceeding-SPE Annual Technical Conference and Exhibition: 2465-2481. [66] Jiang S,Zhang J C,Jiang Z Q,Xu Z Y,Cai D S,Chen L,Wu Y,Zhou D S,Jiang Z L,Zhao X B,Bao S J.2015. Geology,resource potentials,and properties of emerging and potential China shale gas and shale oil plays. Interpretation, 3(2): 1-13. [67] Jiao X,Liu Y Q,Yang W,Zhou D W,Li H,Nan Y,Jin M Q.2018a. A magmatic-hydrothermal lacustrine exhalite from the Permian Lucaogou Formation,Santanghu Basin,NW China-The volcanogenic origin of fine-grained clastic sedimentary rocks. Journal of Asian Earth Sciences, 156(1): 11-25. [68] Jiao X,Liu Y Q,Yang W,Zhou D W,Wang S S,Jin M Q,Sun B,Fan T T.2018b. Mixed biogenic and hydrothermal quartz in Permian lacustrine shale of Santanghu Basin,NW China: Implications for penecontemporaneous transformation of silica minerals. International Journal of Earth Sciences, 107: 1989-2009. [69] Kelley D S,Karson J A,Blackman D K,Früh-Green G L,Butterfield D A,Lilley M D,Olson E J,Schrenk M O,Roe K R,Lebon G T,Rivizzigno P,the AT3-60Shipboard Party.2001. An off-axis hydrothermal vent field near the Mid-Atlantic Ridge at 30° N. Nature, 412: 145-149. [70] Krumbein W C.1933. The dispersion of fine-grained sediments for mechanical analysis. Journal of Sedimentary Research, 3(3): 121-135. [71] Krumbein W C.1947. Shales and their environmental significance. Journal of Sedimentary Research,17(3): 101-108. [72] Kuenen Ph H,Migliorini C I.1950. Turbidity currents as a cause of graded bedding. The Journal of Geology, 58(2): 97-127. [73] Liang C,Jiang Z X,Cao Y C,Wu J,Wang Y S,Hao F.2017. Sedimentary characteristics and origin of lacustrine organic rich shales in the salinized Eocene Dongying Depression. GSA Bulletin, 130(1): 154-174. [74] Lonsdale P,Southard J B.1974. Experimental erosion of North Pacific red clay. Marine Geology, 17(1): 51-60. [75] Macquaker J H S,Adams A E.2003. Maximizing information form fine-grained sedimentary rocks: An inclusive nomenclation form mudstones. Journal of Sedimentary Research, 73(5): 735-744. [76] Macquaker J H S,Bentley S J,Bohacs K M.2010. Wave-enhanced sediment-gravity flows and mud dispersal across continental shelves: Reappraising sediment transport processes operating in ancient mudstone successions. Geology, 38(10): 947-950. [77] Mulder T,Syvitski J P M.1995. Turbidity currents generated at river mouths during exceptional discharges to the world oceans. The Journal of Geology, 103(3): 285-299. [78] Picard M D.1971. Classification of fine-grained sedimentary rocks. Journal of Sedimentary Petrology, 41(1): 179-195. [79] Potter P E,Maynard B,Pryor W A.1980. Sedimentology of Shale. New York:Springer,4-50. [80] Rona P A,McGregor B A,Betzer P R,Bolger G W,Krause D C.1975. Anomalous water temperatures over Mid-Atlantic Ridgecrest at 26 °N latitude. Deep-Sea Research, 22(9): 611-618. [81] Schieber J,Zimmerle W.1998. The history and promise of shale research. Stuttgart: Schweizerbart’sche Verlagsbuchhandlung, 1-10. [82] Schieber J,Southard J B.2009. Bedload transport of mud by floccule ripples-Direct observation of ripple migration processes and their implications. Journal of Food Engineering, 37(6): 483-486. [83] Schieber J,Krinsley D,Riciputi L.2000. Diagenetic origin of quartz silt in mudstones and implications for silica cycling. Nature, 406: 981-985. [84] Schieber J,Southard J,Thaisen K.2007. Accretion of mudstone beds from migrating floccule ripples. Science, 318: 1760-1763. [85] Schieber J,Southard J B,Schimmelmann A.2010. Lenticular shale fabrics resulting from intermittent erosion of water-rich muds-interpreting the rock record in the light of recent flume experiments. Journal of Sedimentary Research, 80(1): 119-128. [86] Simoneit B R T,Lonsdale P F.1982. Hydrothermal petroleum in mineralized mounds at the seabed of Guaymas Basin. Nature, 295: 198-202. [87] Simoneit B R T,Lein A Y,Peresypkin V I.2004. Composition and origin of hydrothermal petroleum and associated lipids in the sulfide deposits of the Rainbow field(Mid-Atlantic Ridge at 36°N). Geochimica Et Cosmochimica Acta, 68(10): 2275-2294. [88] Slack J F.2012. Exhalites in volcanogenic massive sulfide occurrence model. U.S. Geological Survey Scientific Investigations Report,2010-5070-C,chap. 10: 6. [89] Smith J. V.2018. Susceptibility of lava domes to erosion and collapse by toppling on cooling joints. Journal of Volcanology and Geothermal Research, 349: 311-322. [90] Southard J B,Young R A,Hollister C D.1971. Experimental erosion of calcareous ooz. Journal of Geophysical Research, 76(24): 5903-5909. [91] Talling P J,Masson D G,Sumner E J,Malgesini G.2012. Subaqueous sediment density flows: Depositional processes and deposit types. Sedimentology, 59(7): 1937-2003. [92] Tang X,Zhang J C,Wang X Z,Yu B S,Ding W L,Xiong J Y,Yang Y,Wang L,Yang C.2015. Shale Characteristics in the southeastern Ordos Basin,China: Implications for hydrocarbon accumulation conditions and the potential of continental shales. International Journal of Coal Geology,128-129(3): 32-46. [93] Verolino A,White J D L,Zimanowski B.2018. Particle transport in subaqueous eruptions: An experimental investigation. Journal of Volcanology and Geothermal Research, 349: 298-310. [94] Wang G C,Carr T R.2012. Marcellus shale lithofacies prediction by multiclass neural network classification in the Appalachian Basin. Mathematical Geosciences, 44(8): 975-1004. [95] Wang P,Jiang Z,Yin L,Chen L,Li Z,Zhang C,Li T W,Huang P.2017. Lithofacies classification and its effect on pore structure of the Cambrian marine shale in the Upper Yangtze Platform,South China: Evidence from FE-SEM and gas adsorption analysis. Journal of Petroleum Science & Engineering, 156: 307-321. [96] White D E.1955. Thermal springs and epithermal ore deposits. Economic Geology(50th Anniversary Volume): 99-154. [97] White J D L.2000. Subaqueous eruption-fed density currents and their deposits. Precambrian Research, 101: 87-109. [98] White J D L,Houghton B F.2006. Primary volcaniclastic rocks. Geology, 34(8): 677-680. [99] Yang R,Jin Z J,van Loon A J(T),Han Z Z,Fan A.2017. Climatic and tectonic controls of lacustrine hyperpycnite origination in the Late Triassic Ordos Basin,central China: Implications for unconventional petroleum development. AAPG Bulletin, 101(1): 95-117. [100] Zou C N,Yang Z,Cui J W,Zhu R K,Hou L H,Tao S Z.2013. Formation mechanism,geological characteristics,and development strategy of nonmarine shale oil in China. Petroleum Exploration and Development, 40(1): 14-26. [101] Sundborg,Å.1956. The river Klarälven;A study of fluvial processes. Geografiska Annaler, 38: 127-316.
