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华北克拉通西南缘中元古代构造地层格架新认识(PDF)

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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:: 第47卷
期数:: 2025年第02期

页码:: 158-175

栏目:: 基础地质与矿床地质

出版日期:: 2025-03-15

文章信息/Info

Title:: New Insight into the Mesoproterozoic Stratigraphic Tectonic Framework in the Southwestern Margin of North China Craton

文章编号:: 1672-6561(2025)02-0158-18

作者:: 周义军^1*; 李振宏²; 3; 白海峰⁴; 余小雷¹; 董晓朋²; 3; 寇琳琳²; 3; (1. 中国石油集团东方地球物理公司研究院,河北涿州 072750; 2. 中国地质科学院地质力学研究所,北京 100081; 3. 自然资源部活动构造与地质安全重点实验室,北京 100081; 4. 中国石油长庆油田公司勘探开发研究院,陕西西安 710018)

Author(s):: ZHOU Yi-jun^1*; LI Zhen-hong²; 3; BAI Hai-feng⁴; YU Xiao-lei¹; DONG Xiao-peng²; 3; KOU Lin-lin²; 3; (1. Geophysical Research Institute, BGP Inc., CNPC, Zhuozhou 072750, Hebei, China; 2. Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China; 3. Key Laboratory of Active Tectonics and Geological Safety, Ministry of Natural Resources, Beijing 100081, China; 4. Research Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi'an 710018, Shaanxi, China)

关键词:: 中元古代; 长城系; 熊耳群; 玄武安山岩; 地球化学; 裂谷体系; 华北克拉通

Keywords:: Mesoproterozoic; Changcheng System; Xiong'er Group; basaltic andesite; geochemistry; rift system; North China Craton

分类号:: P534.3; P548

DOI:: 10.19814/j.jese.2024.10004

文献标志码:: A

摘要:: 华北克拉通中新元古代发育南部熊耳裂谷、东北部燕辽裂谷和北部渣尔泰—白云鄂博裂谷,但由于缺乏大规模火山岩喷发的直接证据,西南缘是否有固原裂谷一直存在争议。利用最新钻探的蟠探1井岩芯岩屑资料,结合区域地震剖面,采用锆石U-Pb定年及元素地球化学分析,厘定了中元古界长城系火山岩的喷发时限及构造属性,系统建立了华北克拉通西南缘中元古代的沉积-火山岩序列以及与熊耳裂谷中条山地区长城纪地层的对比关系,揭示了华北克拉通西南缘中元古代的地质结构。结果表明:蟠探1井在中元古界长城系钻遇一套厚层玄武安山岩,玄武安山岩具间隐结构、玻基斑状结构,主要为玻璃质和基性斜长石,含丰富磁铁矿,火山岩主体喷发时限分别为(1 768.51±0.39)Ma和(1 778.7±8.0)Ma,在喷发时限上相当于华北克拉通南缘中条山地区熊耳裂谷的马家河组火山岩序列; 玄武安山岩元素地球化学特征显示轻稀土元素富集,重稀土元素亏损,Eu负异常,微量元素相对富集大离子亲石元素Rb和Th,Zr和Hf明显正异常,Sr、P、Ba、Ti、Nb明显负异常,总体具有区域拉张的构造背景; 在地震剖面上,玄武安山岩与上覆砂岩声波速度差异明显,可形成强波谷反射界面,有利于玄武安山岩体的精确标定与追踪,地震与钻井相互约束,有效圈定中元古代火山岩相的主体范围大致位于华北克拉通西缘的固原与银川之间。

Abstract:: The three rift systems of Xiong'er rift in the southern margin, Yanliao rift in the northeastern margin and Zha'ertai-Baiyun'ebo rift in the northern margin of North China Craton have been recognized by the geoscience community. However, whether there is a Guyuan rift in the southwestern margin has been questioned due to the lack of direct evidence of large-scale volcanic eruption. Based on the latest drilling core cuttings data of well Pantan1, combined with regional seismic profiles, zircon U-Pb dating and element geochemical analysis, the eruption time and tectonic attributes of the Mesoproterozoic Changcheng System volcanic rocks were determined; the Mesoproterozoic sedimentary-volcanic rock sequence in the southwestern margin of North China Craton and its correlation with Changcheng System in Zhongtiaoshan area of Xiong'er rift were systematically established, and the geological structure of the Mesoproterozoic in the southwestern margin of North China Craton was revealed. The results show that a set of thick basaltic andesite is drilled in well Pantan1 in the Mesoproterozoic Changcheng System; the basaltic andesite has inter-cryptic structure and glass-based porphyritic structure, mainly glassy and basic plagioclase, containing abundant magnetite; the main eruption time of volcanic rock is(1 768.51±0.39)Ma and(1 778.7±8.0)Ma, respectively, which is equivalent to the volcanic rock sequence of Majiahe Formation in Xiong'er rift in Zhongtiaoshan area, the southern margin of North China Craton; the element geochemical characteristics of the basaltic andesite show LREE enrichment, HREE loss, Eu negative anomaly, trace elements are relatively enriched in large ion lithophile elements Rb and Th, Zr and Hf obvious positive anomalies, Sr, P, Ba, Ti, Nb obvious negative anomalies, with a regional extensional tectonic background; on the seismic profile, the difference of wave velocity between the basaltic andesite and the overlying sandstone is obvious, which can form a strong trough reflection interface and is conducive to the accurate calibration and tracking of the basaltic andesite; the seismic and drilling are mutually constrained, and the main range of the Mesoproterozoic volcanic facies is effectively delineated; it is roughly located between Guyuan and Yinchuan on the western margin of North China Craton.

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备注/Memo:: 收稿日期:2024-10-08; 修回日期:2025-01-11
基金项目:国家自然科学基金项目(U2244220); 中国地质调查局地质调查项目(DD20221644)
*通信作者:周义军(1975-),男,湖北黄冈人,高级工程师,工学博士,E-mail:zyj202410@126.com。
通信作者:李振宏(1973-),男,山西运城人,中国地质科学院地质力学研究所研究员,理学博士,E-mail:lizhennhong@126.com。

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