吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (2): 454-464.doi: 10.13278/j.cnki.jjuese.20190266

• 沉积盆地分析 • 上一篇    下一篇

四川盆地广安地区中二叠统栖霞组岩石特征与沉积环境

易海永1, 崔宝琛2, 王瑶琳3, 邱玉超1, 徐胜林3, 李乾3   

  1. 1. 中国石油西南油气田分公司, 成都 610056;
    2. 中国石油天然气股份有限公司对外合作经理部, 北京 100011;
    3. 成都理工大学沉积地质研究院, 成都 610059
  • 收稿日期:2019-12-10 出版日期:2020-03-26 发布日期:2020-03-31
  • 作者简介:易海永(1970-),男,高级工程师,主要从事石油天然气勘探方面的研究工作,E-mail:85821702@qq.com
  • 基金资助:
    中国石油天然气股份有限公司重大科技专项(2016E-0603)

Petrological Characteristics and Sedimentary Environment of Qixia Formation in Guang’an Area, Sichuan Basin

Yi Haiyong1, Cui Baochen2, Wang Yaolin3, Qiu Yuchao1, Xu Shenglin3, Li Qian3   

  1. 1. Southwest Oil&Gas Filed Company, PetroChina, Chengdu 610056, China;
    2. PetroChina Foreign Cooperation Administration Department, Beijing 100011, China;
    3. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
  • Received:2019-12-10 Online:2020-03-26 Published:2020-03-31
  • Supported by:
    Supported by Project of Major Science and Technology Projects of China National Petroleum Corporation (2016E-0603)

摘要: 四川盆地中二叠统栖霞组勘探发现系列油气,资源潜力巨大。但广安地区中二叠统栖霞组的岩石学特征及沉积环境研究薄弱。在野外地质调查的基础上,结合室内岩石学、岩相学等综合分析,对广安地区栖霞组碳酸盐岩岩石特征、沉积相类型及其古地理展布特征进行了系统研究。结果表明:广安地区栖霞组主要发育亮晶颗粒灰岩、亮晶生物碎屑灰岩、微晶生物碎屑灰岩、微晶颗粒灰岩、生物碎屑微晶灰岩、含生物碎屑微晶灰岩和泥晶灰岩7种岩石类型;碳酸盐岩颗粒主要以生物碎屑为主,部分层位发育球粒;古生物化石以三叶虫、腕足和有孔虫为主,同时可见棘皮类和藻类;栖霞组沉积期主要为碳酸盐岩台地沉积环境,其中栖霞组晚期(栖二段)台缘滩和台内滩较为发育,为该区油气成藏提供了有利条件。

关键词: 岩石类型, 沉积环境, 栖霞组, 广安地区, 四川盆地

Abstract: A series of petroleum exploration discoveries have been made in Qixia Formation of Middle Permian in Sichuan basin, which has great resource potential. However, the previous research on the petrological characteristics and sedimentary environment of Middle Permian Qixia Formation in Guang'an area is weak. On the basis of geological survey, combined with petrology and petrography, the authors studied the carbonate rock characteristics, sedimentary facies types,and paleo-geographical distribution characteristics of Qixia Formation. The result shows that there are seven rock types developed in Qixia Formation in Guang'an area, including sparry bioclastic limestone, sparry granular limestone, microcrystalline bioclastic limestone, microcrystalline granular limestone, biofragmentary microcrystalline limestone, biofragmentary microcrystalline limestone containing biofragmentary microcrystalline limestone, and micritic limestone. The carbonate grains are mainly bioclastic, and spherules in some layers. Paleontological fossils are mainly trilobites, brachiopods, foraminifera, as well as echinoderms and algae. In the deposition period of Qixia Formation, the depositional environment was mainly a carbonate platform; in the later stage of Qixia Formation (Member 2), the marginal-platform shoals and intra-platform shoals were well developed, which provides favorable conditions for hydrocarbon accumulation in this area.

Key words: rock types, sedimentary environment, Qixia Formation, Guang'an area, Sichuan basin

中图分类号: 

  • P588.2
[1] 宋文海. 四川盆地二叠系白云岩的分布及天然气勘探[J]. 天然气工业, 1985, 5(4):22-23. Song Wenhai. Distribution of Permian Dolomite and Natural Gas Exploration in Sichuan Basin[J]. Natural Gas Industry, 1985, 5(4):22-23.
[2] 陈宗清. 论四川盆地中二叠统栖霞组天然气勘探[J]. 天然气地球科学, 2009, 20(3):325-334. Chen Zongqing. Discussion on Gas Exploration of Middle Permian Qixia Formation, Sichuan Basin[J]. Natural Gas Geoscience, 2009, 20(3):325-334.
[3] 舒晓辉, 张军涛, 李国蓉, 等. 四川盆地北部栖霞组-茅口组热液白云岩特征与成因[J]. 石油与天然气地质, 2012, 33(3):442-448. Shu Xiaohui, Zhang Juntao, Li Gourong, et al. Characteristics and Genesis of Hydrothermal Dolomites of Qixia and Maokou Formations in Northern Sichuan Basin[J]. Oil & Gas Geology, 2012, 33(3):442-448.
[4] 汪华, 沈浩, 黄东, 等. 四川盆地中二叠统热水白云岩成因及其分布[J]. 天然气工业, 2014, 34(9):25-32. Wang Hua, Shen Hao, Huang Dong, et al. Origin and Distribution of Hydrothermal Permian in the Sichuan Dolomites of the Middle Basin[J]. Natural Gas Industry, 2014, 34(9):25-32.
[5] 江青春, 胡素云, 汪泽成, 等. 四川盆地中二叠统中-粗晶白云岩成因[J]. 石油与天然气地质, 2014, 35(4):503-510. Jiang Qingchun, Hu Suyun, Wang Zecheng, et al.Genesis of Medium-Macro-Crystalline Dolomite in the Middle Permian of Sichuan Basin[J]. Oil & Gas Geology, 2014, 35(4):503-510.
[6] 胡明毅, 魏国齐, 胡忠贵, 等. 四川盆地中二叠统栖霞组层序-岩相古地理[J]. 古地理学报, 2010, 12(5):515-526. Hu Mingyi, Wei Guoqi, Hu Zhonggui, et al. Sequence-Lithofacies Palaeogeography of the Middle Permian Qixia Formation in Sichuan Basin[J]. Jouanal of Palaeography, 2010, 12(5):515-526.
[7] 李凤杰, 刘琪, 刘殿鹤, 等. 四川盆地东北部二叠系层序发育的动力学分析[J]. 地层学杂志, 2010(1):35-42. Li Fengjie, Liu Qi, Liu Dianhe, et al.Sequence Dynamics of the Permian System in Northeastern Sichuan Basin[J]. Journal of Stratigraphy, 2010(1):35-42.
[8] 赵宗举, 周慧, 陈轩, 等. 四川盆地及邻区二叠纪层序岩相古地理及有利勘探区带[J]. 石油学报, 2012, 33(增刊2):35-51. Zhao Zongju, Zhou Hui, Chen Xuan, et al. Sequence Lithofacies Paleogeography and Favorable Exploration Zones of the Permian in Sichuan Basin and Adjacent Areas, China[J]. Acta Petrolei Sinica, 2012, 33(Sup. 2):35-51.
[9] 刘雁婷, 张文军, 熊治富, 等. 四川盆地东北部中二叠统层序地层特征[J]. 沉积与特提斯地质, 2014, 34(2):47-53. Liu Yanting, Zhang Wenjun, Xiong Zhifu, et al. Sequence Stratigraphy of the Middle Permian Strata in Northeastern Sichuan Basin[J]. Sedimentary Geology and Tethyan Geology, 2014, 34(2):47-53.
[10] 郑超, 王宇峰, 汤兴宇, 等. 双鱼石地区栖霞组层序地层划分及沉积相分析[J]. 特种油气藏, 2018, 25(4):39. Zheng Chao, Wang Yufeng, Tang Xingyu, et al. Sequence Stratigraphic Division and Sedimentary Facies Analysis of Qixia Formation in the Shuangyushi Block[J]. Special Oil & Gas Reservoirs, 2018, 25(4):39.
[11] 单长安, 王胜涛, 陈越, 等. 华蓥溪口剖面中二叠统栖霞组沉积相分析[J]. 海洋石油, 2012, 32(3):45-51. Shan Chang'an, Wang Shengtao, Chen Yue, et al. Analysis on Sedimentary Facies in the Qixia Formation, Middle Permian at Huaying Xikou Section[J]. Offshore Oil, 2012, 32(3):45-51.
[12] 钟怡江, 侯梅生, 夏杰, 等. 重庆石柱中二叠统栖霞组和茅口组沉积微相[J]. 成都理工大学学报(自然科学版), 2014, 41(4):458-467. Zhong Yijiang, Hou Meisheng, Xia Jie, et al.Microfacies of Qixia Formation and Maokou Formation in Shizhu, Chongqing, China[J]. Journal of Chengdu University of Technology (Science & Technology Edition), 2014, 41(4):458-467.
[13] 张运周, 徐胜林, 陈洪德, 等. 川东北旺苍地区栖霞组地球化学特征及其古环境意义[J]. 石油实验地质, 2018, 40(2):210-217. Zhang Yunzhou, Xu Shenglin, Chen Hongde, et al. Geochemical Characteristics and Paleo-Environmental Implications of Middle Permian Qixia Formation in Wangcan, Northern Sichuan[J]. Petrolum Geology & Experiment, 2018, 40(2):210-217.
[14] 石新, 王兴志, 张帆, 等. 川西北地区栖霞组白云岩储集层研究[J]. 西南石油学院学报, 2005, 27(2):13-16. Shi Xin, Wang Xingzhi, Zhang Fan, et al.The Study of the Dolomite Reservoir of Qixia Formation in the Northwest Sichuan Region[J]. Joumal of Southwest Petroleun Institute, 2005, 27(2):13-16.
[15] 许国明, 谢刚平, 隆轲, 等. 四川盆地西南部中二叠统沉积特征与勘探目标[J]. 天然气工业, 2015, 35(7):27-33. Xu Guoming, Xie Gangping, Long Ke, et al. Sedimentary Features and in the Exploration Targets of Middle Permian Reservoirs Southwestern Sichuan Basin[J]. Natural Gas Industry, 2015, 35(7):27-33.
[16] 黄先平, 杨天泉, 张红梅. 四川盆地下二叠统沉积相及其勘探潜力区研究[J]. 天然气工业, 2004, 24(1):10-12. Huang Xianping, Yang Tianquan, Zhang Hongmei. Research on the Sedimentary Facies and Exploration Potential Areas of Lower Permian in Sichuan Basin[J]. Natural Gas Industry, 2004, 24(1):10-12.
[17] 魏国齐, 杨威, 朱永刚, 等. 川西地区中二叠统栖霞组沉积体系[J]. 石油与天然气地质, 2010, 31(4):442-448. Wei Guoqi, Yang Wei, Zhu Yonggang, et al. Depositional System of the Middle Permian Qixia Formation in the Western Sichuan Basin[J]. Oil & Gas Geology, 2010, 31(4):442-448.
[18] 周进高, 姚根顺, 杨光, 等. 四川盆地栖霞组-茅口组岩相古地理与天然气有利勘探区带[J]. 天然气工业, 2016, 36(4):8-15. Zhou Jingao, Yao Genshun, Yang Guang, et al. Lithofacies Palaeogeography and Favorable Gas Exploration Zones of Qixia and Maokou Fms in the Sichuan Basin[J]. Natural Gas Industry, 2016, 36(4):8-15.
[19] 厚刚福, 周进高, 谷明峰, 等. 四川盆地中二叠统栖霞组、茅口组岩相古地理及勘探方向[J]. 海相油气地质, 2017, 22(1):25-31. Hou Gangfu, Zhou Jingao, Gu Mingfeng,et al. Lithofacies Paleogeography and Exploration Realms of Middle Permian Qixia Formation and Maokou Formation, Sichuan Basin[J]. Marine Origin Petroleum Geology, 2017, 22(1):25-31.
[20] 黎荣, 胡明毅, 杨威, 等.四川盆地中二叠统沉积相模式及有利储集体分布[J]. 石油与天然气地质, 2019, 40(2):369-379. Li Rong, Hu Mingyi, Yang Wei, et al.Sedimentary Facies Model and Favorable Reservoir Distribution of the Middle Permian in Sichuan Basin[J]. Oil & Gas Geology, 2019, 40(2):369-379.
[21] 郝毅, 林良彪, 周进高, 等. 川西北中二叠统栖霞组豹斑灰岩特征与成因[J]. 成都理工大学学报(自然科学版), 2012, 39(6):651-656. Hao Yi, Lin Liangbiao, Zhou Jingao, et al. Characteristics and Genesis of Leopard Limestone in Middle Permian Qixia Formation, Northwest Sichuan, China[J]. Journal of Chengdu University of Technology (Sciences & Technology Edition), 2012, 39(6):651-656.
[22] 曾德铭, 石新, 王兴志, 等. 川西北地区下二叠统栖霞组滩相储层特征及其分布[J]. 天然气工业, 2010, 30(12):25-28. Zeng Deming, Shi Xin, Wang Xingzhi, et al. Features and Distribution of Shoal Facies Reservoirs in the Lower Permian Qixia Formation, Northwest Sichuan Basin[J]. Natural Gas Industry, 2010, 30(12):25-28.
[23] 姜德民, 田景春, 黄平辉, 等. 川西南部地区中二叠统栖霞组岩相古地理特征[J]. 西安石油大学学报(自然科学版), 2013, 28(1):41-46. Jiang Demin, Tian Jingchun, Huang Pinghui, et al. Lithofacies Palaeogeography of Qixia Formation in Southwest Sichuan Basin[J]. Journal of Xi'an Shiyou University (Natural Science Edition), 2013, 28(1):41-46.
[24] Wilson J L. Carbonate Facies in Geologic History[M]. New York:Springer Science & Business Media, 1975.
[25] Flügel E. Microfacies of Carbonate Rocks:Analysis, Interpretation and Application[M]. Heidelberg:Springer Science & Business Media, 2004.
[26] Flügel E. Microfacies Analysis of Limestones[M]. Heidelberg:Springer Science & Business Media, 1982.
[27] 徐胜林, 袁文俊, 侯明才, 等. 上扬子地台南缘早志留世埃隆期碳酸盐岩岩石学特征及沉积环境[J]. 岩石学报, 2017, 33(4):1357-1368. Xu Shenglin, Yuan Wenjun, Hou Mingcai, et al. Petrological Characteristics and Sedimentary Environment of Carbonate During Aeronlian Stake of Early Silurian in the Southern Marlin of Yangtze Craton[J]. Actor Petrologica Sinica, 2017, 33(4):1357-1368.
[28] 李美铮, 刘楚雄, 江大勇, 等. 贵州盘县新民地区关岭组中三叠世盘县动物群产出层段碳酸盐岩微相分析和古环境恢复[J]. 地学前缘(中国地质大学(北京);北京大学), 2011, 18(6):329-340. Li Meizheng, Liu Chuxiong,Jiang Dayong, et al. The Analysis of Microfacies and Paleaoenvironment Reconstruction of Panxian Fauna from the Guanling Formation (Middle Triassic) of Xinmin, Panxian County, Guizhou[J]. Earth Science Frontiers (China University of Geosciences(Beijing); Peking University),2011, 18(6):329-340.
[29] 周新平, 郑可, 何幼斌, 等. 四川宣汉立石河剖面二叠系岩石特征及沉积环境分析[J]. 地质科技情报, 2017, 36(6):164-173. Zhou Xinping, Zheng Ke, He Youbin, et al. Petrological Characteristics and Sedimentary Environment of the Permian of Lishihe Section in Xuanhan, Sichuan[J]. Geological Science and Technology Information, 2017, 36(6):164-173.
[30] 胡凯迪, 陈洪德, 徐胜林, 等. 重庆綦江藻渡中二叠统沉积微相[J]. 成都理工大学学报(自然科学版), 2019, 46(3):334-340. Hu Kaidi, Chen Hongde,Xu Shenglin, et al. Study of Sedimentary Microfacies of the Middle Permian at Zaodu Section, Qijiang County, Chongqing, China[J]. Journal of Chengdu University of Technology (Sciences & Technology Edition), 2019, 46(3):334-340.
[31] 鄢伟, 张光学, 樊太亮, 等.塔里木盆地塔中-顺托果勒地区奥陶系良里塔格组碳酸盐岩颗粒滩沉积特征[J].吉林大学学报(地球科学版), 2019, 49(3):621-636. Yan Wei, Zhang Guangxue, Fan Tailiang,et al.Sedimentary Characteristics of Carbonate Shoals of Ordovician Lianglitage Formation in Tazhong and Shuntuoguole Area, Tarim Basin[J]. Journal of Jilin University (Earth Science Edition), 2019, 49(3):621-636.
[32] 陈洪德, 覃建雄, 王成善, 等.中国南方二叠纪层序岩相古地理特征及演化[J].沉积学报, 1999, 17(4):510-521. Chen Hongde, Tan Jianxiong, Wang Chengshan, et al. Sequence-Based Lithofacies and Paleogeographic Characteristics and Evolution of Permian in South China[J]. Acta Sedimentologica Sinica, 1999, 17(4):510-521.
[33] 曾允孚,夏文杰. 沉积岩石学[M]. 北京:地质出版社,1986. Zeng Yunfu, Xia Wenjie. Sedimentary Petrology[M]. Beijing:Geological Publish House, 1986.
[34] 胡明毅, 胡忠贵, 魏国齐, 等. 四川盆地茅口组层序岩相古地理特征及储集层预测[J]. 石油勘探与开发, 2012, 49(1):45-54. Hu Mingyi, Hu Zhonggui, Wei Guoqi,et al. Sequence Lithofacies Paleogeography and Reservoir Prediction of the Maokou Formation in Sichuan Basin[J]. Petroleum Exploration and Development, 2012,49(1):45-54.
[35] 李大军, 陈洪德, 侯明才, 等. 四川盆地中二叠世栖霞期-茅口期岩相古地理特征及其地球动力学机制探讨[J]. 地质科学, 2019, 54(4):1114-1134. Li Dajun, Chen Hongde, Hou Mingcai, et al. Lithofacies and Paleogeographic Characteristics of Middle Permian Qixi and Maokou Periods in Sichuan Basin and the Geodynamic Mecheanism[J]. Chinese Journal of Geology, 2019, 54(4):1114-1134.
[1] 王嗣敏, 臧东升, 王熙琼, 李杰, 韩嵩, 李建中. 辽西建昌盆地油页岩发育特征及沉积环境[J]. 吉林大学学报(地球科学版), 2020, 50(2): 326-340.
[2] 孟庆涛, 李金国, 刘招君, 胡菲, 徐川. 茂名盆地羊角含矿区始新统油柑窝组油页岩有机地球化学特征及沉积环境[J]. 吉林大学学报(地球科学版), 2020, 50(2): 356-367.
[3] 董清水, 何春生, 楼仁兴, 任锡钢, 张超, 张渝金, 许圣传. 大兴安岭南段阿鲁科尔沁旗地区林西组沉积环境特征及其时限的地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(2): 425-441.
[4] 张健, 张海华, 陈树旺, 郑月娟, 张德军, 苏飞, 黄欣. 松辽盆地北部上二叠统林西组地球化学特征及地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(2): 518-530.
[5] 曾文人, 孟庆涛, 刘招君, 徐银波, 孙平昌, 王克兵. 柴北缘团鱼山地区中侏罗统石门沟组油页岩有机地球化学特征及古湖泊条件[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1270-1284.
[6] 陈庆松, 杨润柏, 刘德民, 陶兰初. 滇东北会泽灯影组硅质岩成因及沉积环境——来自岩石学和地球化学证据[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1327-1337.
[7] 罗腾, 冯晅, 郭智奇, 刘财, 刘喜武. 基于模拟退火粒子群优化算法的裂缝型储层各向异性参数地震反演[J]. 吉林大学学报(地球科学版), 2019, 49(5): 1466-1476.
[8] 王璐, 杨胜来, 彭先, 刘义成, 徐伟, 邓惠. 缝洞型碳酸盐岩气藏多类型储集层孔隙结构特征及储渗能力——以四川盆地高石梯-磨溪地区灯四段为例[J]. 吉林大学学报(地球科学版), 2019, 49(4): 947-958.
[9] 曾忠诚, 边小卫, 张若愚, 孔文年, 陈宁, 赵端昌, 赵江林. 西昆仑塔什库尔干下-中侏罗统龙山组沉积构造背景分析[J]. 吉林大学学报(地球科学版), 2019, 49(4): 1039-1052.
[10] 高小惠, 张训华, 蔡来星, 郭兴伟, 李文强. 南黄海盆地中部隆起CSDP-2井志留系-石炭系岩石学特征及其沉积相[J]. 吉林大学学报(地球科学版), 2019, 49(1): 53-64.
[11] 史冀忠, 卢进才, 魏建设, 牛亚卓, 韩小锋, 张宇轩. 内蒙古阿拉善右旗雅干地区二叠系埋汗哈达组硅质岩成因及其沉积环境[J]. 吉林大学学报(地球科学版), 2018, 48(6): 1711-1724.
[12] 方晶, 王福, 方雨婷, 潘隆, 李杨, 胡克, 齐乌云, 王中良. 钻孔岩心黏土混浊水电导率、黄铁矿、pH相关性分析及其在古沉积环境复原的应用:以渤海湾西岸平原DC01孔为例[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1154-1164.
[13] 张冰, 郭智奇, 徐聪, 刘财, 刘喜武, 刘宇巍. 基于岩石物理模型的页岩储层裂缝属性及各向异性参数反演[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1244-1252.
[14] 刘忠宝, 杜伟, 高波, 胡宗全, 张钰莹, 吴靖, 冯动军. 层序格架中富有机质页岩发育模式及差异分布:以上扬子下寒武统为例[J]. 吉林大学学报(地球科学版), 2018, 48(1): 1-14.
[15] 刘丽红, 杜小弟, 徐守礼, 文华国. 四川盆地中南部寒武系白云岩特征及形成机制[J]. 吉林大学学报(地球科学版), 2017, 47(3): 775-784.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!