塔里木盆地西北缘震旦系沉积物源分析及对盆地属性的制约

陈汉林; 黄伟康; 李勇; 章凤奇; 吴鸿翔; 杨志林; 黄少英; 杨树锋

doi:10.11781/sysydz202005756

塔里木盆地西北缘震旦系沉积物源分析及对盆地属性的制约

doi: 10.11781/sysydz202005756

陈汉林^{1, 2,},
黄伟康^{1, 2},
李勇³,
章凤奇^{1, 2},
吴鸿翔^{1, 2},
杨志林³,
黄少英³,
杨树锋^{1, 2}

1.
浙江大学地球科学学院, 杭州 310027
2.
教育部含油气盆地构造研究中心, 杭州 310027
3.
中国石油塔里木油田公司勘探开发研究院, 新疆库尔勒 841000

基金项目:

国家重点研发计划 2016YFC0601004

国家科技重大专项 2017ZX05008001

国家科技重大专项 2016ZX05003001

详细信息

作者简介:
陈汉林(1964—)，男，博士，教授，从事造山带与盆地构造研究。E-mail: hlchen@zju.edu.cn

中图分类号: TE122.3
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- 文章访问数: 750
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- 被引次数: 0
出版历程
- 收稿日期: 2020-05-21
- 修回日期: 2020-07-28
- 刊出日期: 2020-09-28

Provenance analysis of Sinian sediments on the northwestern margin of Tarim Basin and its restriction on basin types

CHEN Hanlin^{1, 2
,},
HUANG Weikang^{1, 2},
LI Yong³,
ZHANG Fengqi^{1, 2},
WU Hongxiang^{1, 2},
YANG Zhilin³,
HUANG Shaoying³,
YANG Shufeng^{1, 2}

1.
School of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang 310027, China
2.
Research Center for Structures in Oil and Gas-bearing Basins, Ministry of Education, Hangzhou, Zhejiang 310027, China
3.
Institute of Exploration and Development, Tarim Oilfield Company, PetroChina, Kuerle, Xinjiang 841000, China

摘要

摘要: 新元古代是全球大地构造演化中一个十分重要的阶段，经历了罗迪尼亚（Rodinia）超大陆聚合和裂解的过程。作为我国三个最主要的克拉通盆地之一的塔里木盆地，其发育的新元古界南华系和震旦系沉积体系纪录了大量新元古代盆地构造属性和板块动力学信息，同时也是塔里木克拉通盆地深层油气勘探的重点层系。以塔里木盆地西北缘什艾日克剖面震旦系为对象，在野外调查和沉积学特征研究的基础上，开展碎屑锆石U-Pb定年和物源示踪研究。震旦系苏盖特布拉克组碎屑锆石存在约2 600，2 300，2 000~1 800，790~730和620 Ma等5个年龄峰值，其中2 600，2 300和2 000~1 800 Ma年龄峰值的碎屑锆石来自于塔里木克拉通内部新太古代—中元古代基底；790~730 Ma年龄峰值的碎屑锆石可能来源于塔里木盆地新元古代晚期的裂谷岩浆作用形成的岩浆岩；而620 Ma年龄峰值的锆石直接来自地层沉积时的岩浆作用，表明碎屑物质可能来源于塔里木盆地本身。结合地震剖面所具有断陷—坳陷的结构特征、南华系快速充填的浊积岩沉积建造、震旦系由碎屑岩建造转变为海相碳酸盐岩建造、震旦系苏盖特布拉克组沉积同期的岩浆作用，认为塔里木盆地西北缘震旦系经历了裂谷性盆地的断—坳转换阶段和坳陷阶段。
- 碎屑锆石年代学 /
- 物源分析 /
- 盆地属性 /
- 震旦纪 /
- 塔里木盆地
Abstract: The Neoproterozoic is a very important stage in the global tectonic evolution, which experienced the amalgamation and break-up of the Rodinia. The Nanhua and Sinian strata in the Tarim Basin, which is one of the three major craton basins, have recorded a great deal of information about the tectonic attributes and plate dynamics of the basin in the Neoproterozoic. These are also the key strata for deep oil and gas exploration in the Tarim Craton Basin. Based on field investigations and studies of sedimentary characteristics, this paper studies the U-Pb dating of detrital zircons and provenance of sediments from the Sinian strata outcropped on the northwestern margin of the Tarim Basin. The age distribution of detrital zircons from the Sugetebrak Formation have five peaks in age of about 2 600, 2 300, 2 000-1 800, 790-730 and 620 Ma. The detrital zircons with peak ages of 2 600, 2 300 and 2 000-1 800 Ma are from the Neoarchean-Mesoproterozoic basement within the Tarim Craton, the detrital zircons with peak ages of 790-730 Ma may be derived from magmatic rocks formed by rifting during the late Neoproterozoic in the Tarim Basin, and the zircons with a peak age of 620 Ma were directly derived from magmatism at the time of formation deposition. These results suggest that the clastic material may have originated in the Tarim Basin itself. In view of the fault depression to depression structure on seismic profile, the rapidly filled turbidite sedimentary construction in the Nanhua strata, the transformation of Sinian strata from a clastic rock sequence to a marine carbonate sequence, and the magmatism during the sedimentary period of the Sinian Sugetebrak Formation, it is concluded that the northwestern margin of the Tarim Basin experienced the transition from fault-depression to rift subsidence during the Sinian.
- detrital zircon chronology /
- sediment provenance /
- basin attributes /
- Sinian /
- Tarim Basin

HTML全文

图 1 塔里木克拉通及邻区构造格局(a)，塔西北阿克苏—乌什地区地质简图(b, c)

分别修改自文献[18]和[19]。

Figure 1. Tectonic pattern of the Tarim Craton and its adjacent areas (a) and simplified geological map of Aksu and Ush areas in northwestern Tarim (b, c)

下载: 全尺寸图片幻灯片

图 2 塔里木盆地西北缘什艾日克剖面震旦系苏盖特布拉克组野外照片

Figure 2. Field photos of Sinian Sugetebrak Formation in Shiaireke section, northwestern margin of Tarim Basin

下载: 全尺寸图片幻灯片

图 3 塔里木盆地西北缘什艾日克剖面震旦系综合柱状图

Figure 3. Stratigraphic histogram of Shiaireke section, northwestern margin of Tarim Basin

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图 4 塔里木盆地西北缘什艾日克剖面震旦系奇格布拉克组野外照片

Figure 4. Field photos of Sinian Qigebulake Formation in Shiaireke section, northwestern margin of Tarim Basin

下载: 全尺寸图片幻灯片

图 5 塔里木盆地西北缘什艾日克剖面震旦系苏盖特布拉克组沉积岩碎屑锆石U-Pb年龄谐和曲线

Figure 5. U-Pb concordia plots for detrital zircons of sedimentary rocks from Sinian Sugetebrak Formation in Shiaireke section, northwestern margin of Tarim Basin

下载: 全尺寸图片幻灯片

图 6 塔里木盆地西北缘什艾日克剖面震旦系苏盖特布拉克组沉积岩碎屑锆石U-Pb年龄谱图

Figure 6. U-Pb age spectrum for detrital zircons of sedimentary rocks from Sinian Sugetebrak Formation in Shiaireke section, northwestern margin of Tarim Basin

下载: 全尺寸图片幻灯片

图 7 塔里木盆地MX10-556地震测线剖面结构

Figure 7. Structure along seismic profile MX10-556 in Tarim Basin

下载: 全尺寸图片幻灯片

表 1 塔里木盆地西北缘什艾日克剖面震旦系苏盖特布拉克组碎屑锆石年龄谱峰值特征

Table 1. Peak age characteristics of detrital zircons from Sinian Sugetebrak Formation in Shiaireke section, northwestern margin of Tarim Basin Ma

样号	峰值5	峰值4	峰值3c	峰值3b	峰值3a	峰值2	峰值1
17SARK-01		~797			~1 964	~2 305	~2 603
17SARK-03	~621	~740		~1 840	~1 989	~2 305
17SARK-05	~616	~736	~1 781	~1 864	~2 019	~2 335

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