[an error occurred while processing this directive] 世界地质 2018, 37(4) 1177-1186 DOI:   10.3969/j.issn.1004-5589.2018.04.017  ISSN: 1004-5589 CN: 22-1111/P

本期目录 | 下期目录 | 过刊浏览 | 高级检索                                                            [打印本页]   [关闭]
油气地质
扩展功能
本文信息
Supporting info
PDF(815KB)
[HTML全文]
参考文献[PDF]
参考文献
服务与反馈
把本文推荐给朋友
加入我的书架
加入引用管理器
引用本文
Email Alert
文章反馈
浏览反馈信息
本文关键词相关文章
延长组长9段
浊积岩
沉积特征
有机质富集
本文作者相关文章
韩佳兵
柳蓉
刘招君
张坤
PubMed
Article by Han J
Article by Liu R
Article by Liu Z
Article by Zhang K
鄂尔多斯盆地南缘铜川地区三叠系延长组长9段浊积岩特征及对有机质富集的影响
韩佳兵1,2, 柳蓉1,2,3, 刘招君1,2,3, 张坤1,2
1. 吉林大学地球科学学院, 长春 130061;
2. 吉林省油页岩及共生能源矿产重点实验室, 长春 130061;
3. 油页岩地下原位转化与钻采技术国家地方联合工程实验室, 长春 130021
摘要: 通过岩芯观察、岩石薄片粒度分析,在鄂尔多斯盆地南缘铜川地区三叠系延长组9段识别出了浊积岩,并揭示了其垂向上典型鲍马序列组合及沉积特征。同时,对鄂尔多斯盆地延长组长9段的油页岩、富有机质泥岩等样本进行TOC、热解测试,分析了该段浊积岩特征及对有机质富集的特征及影响。结果表明:半深湖-深湖区油页岩、泥岩干酪根类型以Ⅱ1型为主,浊积岩上下层位的泥岩、泥页岩、粉砂质泥岩等干酪根类型主要为Ⅲ型和Ⅱ2型。长9段浊积岩对含油页岩段的有机质富集具有一定影响,浊积岩AB及ABC序列对底部沉积的泥岩、泥页岩有机质含量影响最大,其有机碳含量相对较低;浊积岩DE序列对底部沉积的泥岩、泥页岩有机质含量影响相对较小,有机质含量相对较高。
关键词 延长组长9段   浊积岩   沉积特征   有机质富集  
Characteristics of turbidite and its influence on organic matter accumulation in Chang 9 Member of Triassic Yanchang Formation in Tongchuan area, southern Ordos Basin
HAN Jia-bing1,2, LIU Rong1,2,3, LIU Zhao-jun1,2,3, ZHANG Kun1,2
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. Key-Lab for Oil Shale and Coexistent Energy Minerals of Jilin Province, Changchun 130061, China;
3. National-Local Joint Engineering Laboratory of In-situ Conversion, Drilling and Exploitation Technology for Oil Shale, Changchun 130021, China
Abstract: Based on core observation and grain size analysis of thin sections, turbidites were identified in Chang 9 Member of Triassic Yanchang Formation in the southern margin of Ordos Basin, and the vertical sedimentary characteristics of the typical Bouma sequence were revealed. Meanwhile,TOC and pyrolysis were tested for the samples of oil shale and organic rich shale in Chang 9 Member of Yanchang Formation in Ordos Basin. The authors analyzed the characteristics of turbidites and their influences on the enrichment of organic matter. The results showed that the kerogen of oil shale and mudstone in the semi-deep lake-deep lake area was mainly type Ⅱ1,and the kerogen of mudstone,shale and silty mudstone overlying and underlying the turbidite were mainly type Ⅲ and type Ⅱ2. The Chang 9 turbidites had some influences on the organic matter accumulation in the oil shale section. The AB and ABC sequences of turbidites had the greatest influence on the organic matter content in the underlying mudstone and shale deposited,and the organic carbon content was relatively low. The DE sequence of turbidite had relatively less influence on the content of organic matter in the underlying mudstone and shale,and the content of organic matter was relatively high.
Keywords: Chang 9 Member of Yanchang Formation   turbidite   sedimentary characteristics   organic matter enrichment  
收稿日期 2018-05-01 修回日期 2018-06-25 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2018.04.017
基金项目:

国家自然科学基金(41302097).

通讯作者: 柳蓉(1976-),女,教授,博士,主要从事沉积学、层序地层学、石油地质学及油页岩成矿理论研究.E-mail:liurong@jlu.edu.cn
作者简介:
作者Email: liurong@jlu.edu.cn

参考文献:
[1] 何家雄,施小斌,夏斌,等. 南海北部边缘盆地油气勘探现状与深水油气资源前景[J].地球科学进展,2007,22(3):261-270. HE Jia-xiong,SHI Xiao-bin,XIA Bin,et al. The satus of the petroleum exploration in the northern South China Sea and the resource potential in the deep water areas[J]. Advances in Earth Science. 2007,22(3):261-270.
[2] 袁珍,李文厚,范萌萌,等. 深水块状砂岩沉积特征及其成因机制探讨:以鄂尔多斯盆地东南缘上三叠统长6油层组为例[J]. 地质利技情报,2011,30(4):43-49. YUAN Zhen,LI Wen-hou,FAN Meng-meng,et al. Genetic mechanism and sedimentary features of deep water massive sandstone:a case study of the Upper Triassic sandstones of Chang 6 Formation in the southeast of Ordos Basin[J]. Geological Science and Technology Information,2011,30(4):43-49.
[3] 国吉安,庞军刚,王桂成,等. 鄂尔多斯盆地晚三叠世延长组湖盆演化及石油聚集规律[J]. 世界地质,2010,29(2):277-291. GUO Ji-an,PANG Jun-gang,WANG Gui-cheng,et al. Lake basin evolution and petroleum accumulation of Late Triassic Yanchang Formation in Ordos Basin[J]. Global Geology,2010,29(2):277-291.
[4] 李文厚,邵磊,魏红红,等. 西北地区湖相浊流沉积[J]. 西北大学学报(自然科学版),2001,31(1):57-62. LI Wen-hou,SHAO Li,WEI Hong-hong,et al. Turbidity current deposits of lake fades in northwestern China[J]. Journal of North West University(Natural Science Edition),2001,31(1):57-62.
[5] 朱静,朱亚军,辛红刚,等. 鄂尔多斯盆地延长组长9油层组沉积特征[J]. 西北大学学报(自然科学版),2013,43(1):94-100. ZHU Jing,ZHU Ya-jun,XIN Hong-gang,et al. The sedimentation during Chang 9 oil formation in Yanchang Formation in Ordos Basin[J]. Journal of Northwest University (Natural Science Edition),2013,43(1):94-100.
[6] 傅强,吕苗苗,刘永斗. 鄂尔多斯盆地晚三叠世湖盆浊积岩发育特征及地质意义[J]. 沉积学报,2008,26(2):186-192. FU Qiang,LYU Miao-miao,LIU Yong-dou. Developmental characteristics of turbidite and its implication on petroleum geology in Late Triassic Ordos Basin[J]. Acta Sedimentologica Sinica,2008,26(2):186-192.
[7] 杨仁超,何治亮,邱桂强,等. 鄂尔多斯盆地南部晚三叠世重力流沉积体系[J]. 石油勘探与开发. 2014,41(6):661-670. YANG Ren-chao,HE Zhi-liang,QIU Gui-qiang,et al. Late Triassic gravity flow depositional systems in the southern Ordos Basin[J]. Petroleum Exploration and Development, 2014,41(6):661-670.
[8] 陈全红,李文厚,郭艳琴,等. 鄂尔多斯盆地南部延长组浊积岩体系及油气勘探意义[J]. 地质学报,2006,80(5):656-663. CHEN Quan-hong,LI Wen-hou,GUO Yan-qin,et al. Turbidite systems and the significance of petroleum exploration of Yanchang Formation in the southern Ordos Basin[J]. Journal of Geology,2006,80(5):656-663.
[9] 李祥辉,王成善,金玮. 深海沉积理论发展及其在油气勘探中的意义[J]. 沉积学报,2009,27(1):77-84. LI Xiang-hui,WANG Cheng-shan, JIN Wei. A review on deep-sea sedimentation theory:significances to oil-gas exploration[J]. Acta Sedimentologica Sinica,2009,27(1):77-84.
[10] 刘芬,朱筱敏,李洋,等. 鄂尔多斯盆地西南部延长组重力流沉积特征及相模式[J]. 石油勘探与开发,2015,42(5):577-588. LIU Fen,ZHU Xiao-min,LI Yang,et al. Sedimentary characteristics and fades model of gravity flow deposits of Late Triassic Yanchang Formation in southwestern Ordos Basin,NW China[J]. Petroleum Exploration and Development, 2015,42(5):577-588.
[11] 何自新. 鄂尔多斯盆地演化与油气[M]. 北京石油工业出版社,2003:95-105. HE Zi-xin. Evolution and petroleum of Ordos Basin[M]. Beijing:Petroleum Industry Press,2003:95-105.
[12] 姜在兴,沉积学[M]. 北京:石油工业出版社,2003:357-374. JIANG Zai-xing. Sedimentology[M]. Beijing:Petroleum Industry Press,2003:357-374.
[13] 刘招君. 湖泊水下扇沉积特征及影响因素:以伊通盆地莫里青断陷双阳组为例[J]. 沉积学报,2003,21(1):148-154. LIU Zhao-jun. Acus subaqueous fan sedinentary characteristics and influence factors-a case study of Shuangyang Formation in Moliqing fault subsidence of Yitong Basin[J]. Acta Sedimentologica Sinica,2003,21(1):148-154.
[14] 赵俊兴,李风杰,申晓莉,等. 鄂尔多斯盆地南部长6和长7油层浊流事件的沉积特征及发育模式[J]. 石油学报,2008,29(3):389-394. ZHAO Jun-xing,LI Feng-jie,SHEN Xiao-li,et al. Sedimentary characteristics Chang 6 and Chang 7 and development pattern of turbidity event of oil reservoirs in the southern Ordos Basin[J]. Acta Petrolei Sinica,2008,29(3):389-394.
[15] 冯娟萍,李文厚,欧阳征健. 鄂尔多斯盆地黄陵地区上三叠统延长组长7、长6油层组浊积岩沉积特征及地质意义[J]. 古地理学报,2012,14(3):295-302. FENG Juan-ping,LI Wen-hou,OUYANG Zheng-jian. Sedimentary characters and geological implication of turbidite of the Chang 6 and Chang 7 intervals of Upper Triassic Yanchang Formation in Huangling area,Ordos Basin[J]. Journal of Palaeogeography,2012,14(3):295-302.
[16] 郝松立,李兆雨,李文厚. 鄂尔多斯盆地西南部延长组长7段浊积岩沉积特征[J]. 地质通报. 2016,35(2/3):424-432. HAO Song-li,LI Zhao-yu,LI Wen-hou. Sedimentary characteristics of turbidite of Chang 7 Member in southwestern Ordos Basin[J]. Geological Bulletin of China,2016,35(2/3):424-432.
[17] 时保宏,姚径利,张艳,等. 鄂尔多斯盆地延长组长9油层组成藏地质条件[J]. 石油与天然气地质,2013,34(3):294-300. SHI Bao-hong,YAO Jing-li,ZHANG Yan,et al. Geologic conditions for hydrocarbon accumulation in Change oil reservoir of the Yanchang Formation,Ordos Basin[J]. Oil & Geology,2013,34(3):294-300.
[18] 葛云锦,贺永红,焦健,等. 鄂尔多斯盆地周长地区长9油层组浊积岩及致密油勘探意义[J]. 中国石油勘探,2015,20(4):30-36. GE Yun-jin,HE Yong-hong,JIAO Jian,et al. Tight oil exploration of Chang 9 turbidity in Zhouchang area of Ordos Basin[J]. China Petroleum Exploration, 2015,20(4):30-36.
[19] 岳会雯,周瑶琪,梁文栋. 深水浊积岩有机质富集规律研究进展[J]. 地质科技情报,2016,35(6):112-120. YUE Hui-wen,ZHOU Yao-qi,LIANG Wen-dong. Progress in accumulation of organic matter in deepwater turbidite[J]. Geological Science and Technology Information,2016,35(6):112-120.
[20] 何玉平,刘招君,董清水,等. 依舒地堑汤原断陷古近系湖底扇沉积与层序特征[J]. 世界地质,2006,25(1):23-28. HE Yu-ping,LIU Zhao-jun,DONG Qing-shui,et al. Sedimentary and sequence characteristics of Paleogene sublacustrine fan of Tangyuan fault depression in Yishu Graben[J]. Global Geology,2006,25(1):23-28.
[21] 付金华,郭正权,邓秀芹. 鄂尔多斯盆地西南地区上三叠统延长组沉积相及石油地质意义[J]. 古地理学报,2005,7(1):34-43. FU Jin-hua,GUO Zheng-quan,DENG Xiu-qin. Sedimentary facies of the Yanchang Formation of Upper Triassic and petroleum geological implication in southwestern Ordos Basin[J]. Journal of Palaeogeography,2005,7(1):34-43.
[22] 张亚楠,梁俊红,李小东,等. 辽西义县组尖山沟层沉积环境粒度分析[J]. 世界地质,2006,25(4):373-389. ZHANG Ya-nan,LIANG Jun-hong,LI Xiao-dong,et al. Grain size analysis of sedimentary environment from Jianshangou bed of Yixian Formation in western Liaoning, China[J]. Global Geology,2006,25(4):373-389.
[23] Stow D A V,Huc A Y,Bertrand P. Depositional processes of black shales in deep water[J]. Marine and Petroleum Geology,2001,18(4):491-498.
[24] Deniau I,Disnar J R,Baudin F,et al. Characterization of organic matter in the Oligocene(Chattian) turbiditic fine grained deposits,offshore Angola[J].Organic Ueochemistry,2010,41(2):135-145.
[25] 郝芳,陈建渝,孙永传,等. 有机相研究及其在盆地分析中的应用[J]. 沉积学报,1994,12(4):77-86. HAO Fang,CHEN Jian-yu,SUN Yong-chuan, et al. Organic facies studies and their use in sedimentary basin analysis[J]. Acta Sedimentologica Sinica,1994,12(4):77-86.
[26] 孙平昌,刘招君,孟庆涛,等. 桦甸盆地古近纪充填特征及对油页岩成矿的影响[J]. 煤炭学报,2011,36(7):1110-1116. SUN Ping-chang,LIU Zhao-jun,MENG Qing-tao,et al. Effect of the basin-fill features on oil shale formation in Paleogene,Huadian Basin[J]. Journal of China Coal Society,2011,36(7):1110-1116.
[27] 刘招君,杨虎林,董清水,等. 中国油页岩[M].北京:石油工业出版社,2009:38-116. LIU Zhao-jun,YANG Hu-lin,DONE Qing-shui, et al. Chinese oil shale[M].Beijing:Petroleum Industry Press, 2009:38-116.
[28] 杨明慧,刘池洋. 鄂尔多斯中生代陆相盆地层序地层格架及多种能源矿产聚集[J].石油与天然气地质,2006,27(4):563-570. YANG Ming-hui,LIU Chi-yang. Sequence stratigraphic framework and its control on accumulation of various energy resources in the Mesozoic continental basins in Ordos[J]. Oi1& Gas Geology,2006,27(4):563-570.
本刊中的类似文章
1.侯艳平, 任延广, 孙丽, 张海军, 吴海波, 彭威, 李敬生.海拉尔盆地东明凹陷明D2井白垩系沉积特征及沉积环境分析[J]. 世界地质, 2020,39(2): 332-343
2.武昕普, 柳蓉, 张坤, 赵康安, 韩佳兵.银额盆地下白垩统巴音戈壁组含油页岩岩系地球化学特征及有机质富集条件[J]. 世界地质, 2019,38(4): 1021-1031
3.徐盛侠, 董清水, 楼仁兴, 李世臻, 王丹丹, 张文浩.吉林柳河盆地沉积特征与油气勘探前景[J]. 世界地质, 2019,38(1): 215-224
4.何奕言, 程日辉, 宋立斌.通化盆地亨通山组沉积特征及储层发育规律[J]. 世界地质, 2018,37(3): 861-872
5.郭强, 秦明宽, 何中波, 刘章月, 宋继叶, 许强, 贾翠, 谭思远.准噶尔盆地中新生代砂岩型铀矿地层沉积特征与产铀远景预测[J]. 世界地质, 2018,37(2): 447-457
6.王甘露, 赵万飞, 苏杭, 卞华鹏, 张峰玮, 李青枫.黔东南与黔西南浊积岩中两种不同类型金矿的比较[J]. 世界地质, 2014,33(3): 572-580
7.王建鹏,刘招君,苗长盛,方石,陈永成.蒙古塔木察格盆地塔南凹陷下白垩统南屯组三角洲沉积及储层特征[J]. 世界地质, 2011,30(3): 415-428

Copyright by 世界地质