吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (5): 1405-1415.doi: 10.13278/j.cnki.jjuese.20170119

• 地质与资源 • 上一篇    下一篇

塔里木盆地麦盖提斜坡皮山北新1井白云质角砾岩地层时代厘定

罗少辉1, 李九梅2,3, 王辉1   

  1. 1. 中国石化西北油田分公司勘探开发研究院, 乌鲁木齐 830011;
    2. 河北工程大学河北省资源勘测研究重点实验室, 河北 邯郸 056038;
    3. 中国石油大学(北京)油气资源与探测国家重点实验室, 北京 102249
  • 收稿日期:2017-12-27 发布日期:2018-11-20
  • 作者简介:罗少辉(1979-),男,工程师,主要从事油气勘探工作,E-mail:luoshaohui1@163.com
  • 基金资助:
    国家科技重大专项（2011ZX05049-001-002）

Age Determination of Dolomite Breccia in Well PSBX1 of Markit Slope in Tarim Basin

Luo Shaohui1, Li Jiumei2,3, Wang Hui1   

  1. 1. Institute of Exploration and Development of Northwest Oil Branch, SINOPEC, Urumqi 830011, China;
    2. Key Laboratory of Resource Exploration Research of Hebei Province, Hebei University of Engineering, Handan 056038, Hebei, China;
    3. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China
  • Received:2017-12-27 Published:2018-11-20
  • Supported by:
    Supported by Major National R & D Projects (2011ZX05049-001-002)

PDF (PC)

206

摘要： 本文结合岩石薄片、古生物孢粉、同位素、铂族元素、野外露头剖面等资料，对塔里木盆地麦盖提斜坡皮山北新1井钻遇的一套白云质角砾岩地层时代进行了厘定。结果认为：6 884~7 068 m段归属古近系吐依洛克组，化石含量较少；7 068~7 150 m段归属白垩系依格孜牙组，孢粉化石丰富。该井古近纪与白垩纪地层界线深度7 068 m，该位置碳同位素的突变指示海洋环境的剧烈变化，这可以与全球K/E界线处对比。同时，铂族元素在该深度见到明显的异常，其含量明显增大，尤其以Rh、Ru、Ir、Os等最为明显。通过此次厘定，丰富了对麦盖提斜坡晚白垩世—古近纪早期沉积格局的认识。

关键词: 塔里木盆地, 麦盖提斜坡, 皮山北新1井, 白云质角砾岩, 地层时代厘定

Abstract: The dolomitic breccia strata is drilled in Well PSBX1, Maigaiti slope, Tarim basin. Its age is determinated based on the data of thin section, paleontology sporopollen, isotope, platinum group elements and outcrop profiles. The results show that the 6 884-7 068 m well interval belongs to the Paleogene Tuyiluoke Group, which has very few fossils, 7 068-7 150 m well interval belongs to the Upper Cretaceous Yigeziya Group, which has a lots of sporopollen fossils. The Paleogene-Cretaceous boundary of this well lies at 7 068 m with an abrupt difference in carbon isotope, indicating a dramatic change of marine environment, which can be compared with the global K/E boundary. At this depth, the platinum group elements has obvious anormalies, their contents increase significantly, especially Rh, Ru, Ir, Os and so on. Through this determination, we have enriched our uderstanding of the sedimentary pattern of the Markit slope during the Late Cretaceous to the Early Paleogene.

Key words: Tarim basin, Markit slope, Well PSBX1, carbonate rocks, stratigraphic age determination

中图分类号: 

  • P59
[1] 吕海涛,顾忆,丁勇,等. 塔里木盆地西南部皮山北新1井白垩系油气成因[J]. 石油实验地质,2016,38(1):84-90. Lü Haitao, Gu Yi, Ding Yong, et al. Cretaceous Petroleum Origin in Well PSBX1 in the Southwestern Tarim Basin[J]. Petroleum Geology & Experiment, 2016, 38(1):84-90.
[2] 张长建,刘少杰,罗少辉,等. 塔里木盆地皮山破火山口构造及其油气地质意义[J]. 新疆石油地质, 2016, 37(3):281-285. Zhang Changjian, Liu Shaojie, Luo Shaohui, et al. Structure and Geological Significance of Pishan Calderain Tarim Basin[J]. Xinjiang Petroleum Geology, 2016, 37(3):281-285.
[3] 汤良杰,邱海峻,云露,等. 塔里木盆地多期改造-晚期定型复合构造与油气战略选区[J]. 吉林大学学报(地球科学版), 2014, 44(1):1-14. Tang Liangjie, Qiu Haijun, Yun Lu, et al. Poly-Phase Reform-Late-Stage Finalization Composite Tectonics and Strategic Area Selection of Oil and Gas Resources in Tarim Basin, NW China[J]. Journal of Jilin University (Earth Science Edition), 2014, 44(1):1-14.
[4] 刘辰生,张琳婷,郭建华. 塔里木盆地白垩系层序地层学[J]. 中南大学学报(自然科学版), 2012, 43(7):2683-2690. Liu Chensheng, Zhang Linting, Guo Jianhua. Sequence of Cetaceous in Tarim Basin[J]. Journal of Central South University (Science and Technology), 2012, 43(7):2683-2690.
[5] 孟昌,孟庆泉,杜芳芳,等. 塔里木盆地西北缘海相白垩系-古近系界线沉积物环境指标研究[J]. 沉积学报, 2011, 29(2):245-254. Meng Chang, Meng Qingquan, Du Fangfang, et al. Study on Environmental Proxies of the Marine Cretaceous-Paleogene Boundary from Wuqia Area in the Northwestern Tarim Basin[J]. Acta Sedimentologica Sinica, 2011, 29(2):245-254.
[6] 郝诒纯,郭宪璞,叶留生,等. 塔里木盆地西南地区海相白垩系-第三系界线[M]. 北京:地质出版社, 2001:1-101. Hao Yichun, Guo Xianpu, Ye Liusheng, et al. Marine Cretaceous and Paleogene Boundary in Southwestern Tarim Basin[M]. Beijing:Geological Publishing House, 2001:1-101.
[7] 廖林,程晓敢,王步清. 塔里木盆地西南缘中生代沉积古环境恢复[J]. 地质学报,2010, 84(8):1195-1206. Liao Lin, Cheng Xiaogan, Wang Buqing. Reconstruction of Mesozoic Sedimentary Paleoenvironment in the Southwestern Tarim Basin, Northwestern China[J]. Acta Geologica Sinica, 2010, 84(8):1195-1206.
[8] 张华,刘成林,曹养同,等. 塔里木古海湾新生代海退时限及方式的初步探讨[J]. 地球学报, 2013, 34(5):577-584. Zhang Hua, Liu Chenglin, Cao Yangtong, et al. A Tentative Discussion on the Time and the Way of Marine Regression from Tarim Bay During the Cenozoic[J]. Acta Geoscientia Sinica, 2013, 34(5):577-584.
[9] 郭群英,李越,张亮,等. 塔里木盆地西南地区白垩系沉积相特征[J]. 古地理学报, 2014, 16(2):169-178. Guo Qunying, Li Yue, Zhang Liang, et al. Sedimentary Facies Characteristics of the Cretaceous in Southwestern Tarim Basin[J]. Journal of Palaeogeography, 2014, 16(2):169-178.
[10] 郭宪璞,王大宁,丁孝忠,等. 塔里木盆地北部早-中白垩世孢粉时代和生物地理区系研究新进展[J]. 地质评论, 2011, 57(6):870-880. Guo Xianpu, Wang Daning, Ding Xiaozhong, et al. Early-Middle Cretaceous Sporopollen Assemblages and New Progress on Biogeography in the Northern Part of Tarim Basin[J]. Geological Review, 2011, 57(6):870-880.
[11] 刘家铎,王峻,王易斌,等. 塔里木盆地喀什北地区白垩系层序岩相古地理特征[J]. 地球科学与环境学报, 2013, 35(1):1-14. Liu Jiaduo, Wang Jun, Wang Yibin, et al. Sequence-Lithology Palaeogeography Characteristic of Cretaceous in Northern Kashi Area of Tarim Basin[J]. Journal of Earth Sciences and Environmant, 2013, 35(1):1-14.
[12] 郭荣涛,赵习,刘红光,等. 兰州盆地下白垩统碎屑岩层序地层序列:祁连山早白垩世隆升的沉积学响应[J]. 吉林大学学报(地球科学版), 2016, 46(2):321-335. Guo Rongtao, Zhao Xi, Liu Hongguang, et al. Sequence Stratigraphic Succession of the Lower Cretaceous Clastic Rock System in Lanzhou Basin:Sedimentological Response to the Early Cretaceous Uplift of Qilian Mountains[J]. Journal of Jilin University (Earth Science Edition), 2016, 46(2):321-335.
[13] 许靖华,何起祥. 彗星冲击作用:白垩纪末期地球上发生灾变的原因[J]. 长春地质学院学报,1980, 10(2):1-8. Xu Jinghua, He Qixiang. Comet impact:The Cause of Catastrophe on the Earth at the End of the Cretaceous Period[J]. Journal of the Changchun College of Geology, 1980, 10(2):1-8.
[14] 田晓雪,雒昆利,谭见安,等. K/T界线的研究进展:兼论元素演化与恐龙灭绝的可能关系[J]. 中国科学院研究生院学报,2005, 22(6):667-675. Tian Xiaoxue, Luo Kunli, Tan Jian'an, et al. Progress on the K/T Boundary:The Relation Between Chemical Elements Abnormity and Dinosaurs Extinction[J]. Journal of the Graduate School of the Chinese Academy of Sciences, 2005, 22(6):667-675.
[1] 郭春涛, 李如一, 陈树民. 塔里木盆地古城地区鹰山组白云岩稀土元素地球化学特征及成因[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1121-1134.
[2] 李文强, 郭巍, 孙守亮, 杨绪海, 刘帅, 侯筱煜. 塔里木盆地巴楚—麦盖提地区古生界油气藏成藏期次[J]. 吉林大学学报(地球科学版), 2018, 48(3): 640-651.
[3] 李昂, 鞠林波, 张丽艳. 塔里木盆地古城低凸起古-中生界构造演化特征与油气成藏关系[J]. 吉林大学学报(地球科学版), 2018, 48(2): 545-555.
[4] 陈斐然, 张颖, 徐祖新, 谭程, 周肖肖. 全球前寒武—寒武系含油气盆地石油地质特征及成藏主控因素[J]. 吉林大学学报(地球科学版), 2017, 47(4): 974-989.
[5] 牛君, 黄文辉, 丁文龙, 蒋文龙, 张亚美, 漆立新, 云露, 吕海涛. 麦盖提斜坡奥陶系碳酸盐岩碳氧同位素特征及其意义[J]. 吉林大学学报(地球科学版), 2017, 47(1): 61-73.
[6] 杜治利, 曾昌民, 邱海峻, 杨有星, 张亮. 塔西南叶城凹陷二叠系两套烃源岩特征及柯东1井油源分析[J]. 吉林大学学报(地球科学版), 2016, 46(3): 651-660.
[7] 薛海涛, 田善思, 卢双舫, 刘敏, 王伟明, 王民. 分散可溶有机质的气源意义[J]. 吉林大学学报(地球科学版), 2015, 45(1): 52-60.
[8] 汤良杰，邱海峻，云露，杨勇，谢大庆，李萌，蒋华山. 塔里木盆地多期改造-晚期定型复合构造与油气战略选区[J]. 吉林大学学报(地球科学版), 2014, 44(1): 1-14.
[9] 王小敏，陈昭年，樊太亮，余腾孝，曹自成，何海. 巴麦地区晚石炭世碳酸盐岩台内滩储层综合评价[J]. 吉林大学学报(地球科学版), 2013, 43(2): 371-381.
[10] 周波，邱海峻， 段书府，李启明，邬光辉. 塔中Ⅰ号断裂坡折带上奥陶统碳酸盐岩储层微观孔隙成因[J]. 吉林大学学报(地球科学版), 2013, 43(2): 351-359.
[11] 高志前, 樊太亮, 杨伟红, 王鑫. 塔里木盆地下古生界碳酸盐岩台缘结构特征及其演化[J]. J4, 2012, 42(3): 657-665.
[12] 郭倩, 蒲仁海. 塔里木盆地巴麦地区石炭系低速异常碳酸盐岩的解释[J]. J4, 2011, 41(3): 689-696.
[13] 张运波, 赵宗举, 袁圣强, 郑民. 频谱分析法在识别米兰科维奇旋回及高频层序中的应用——以塔里木盆地塔中－巴楚地区下奥陶统鹰山组为例[J]. J4, 2011, 41(2): 400-410.
[14] 孙林华. 塔里木盆地瓦吉里塔格超镁铁岩地球化学反演[J]. J4, 2010, 40(6): 1301-1310.
[15] 王民, 卢双舫, 高松, 李吉君, 王乃军. 应用化学动力学法评价塔中地区志留系沥青生气潜力[J]. J4, 2010, 40(1): 15-20.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发