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鄂尔多斯盆地南部上三叠统延长组物源分析及热演化

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孙宁亮, 钟建华, 倪良田, 郝兵, 罗可, 曲俊利, 刘闯, 杨冠群, 曹梦春. 2019. 鄂尔多斯盆地南部上三叠统延长组物源分析及热演化[J]. 中国地质, 46(3): 537-556. doi: 10.12029/gc20190307
引用本文: 孙宁亮, 钟建华, 倪良田, 郝兵, 罗可, 曲俊利, 刘闯, 杨冠群, 曹梦春. 2019. 鄂尔多斯盆地南部上三叠统延长组物源分析及热演化[J]. 中国地质, 46(3): 537-556. doi: 10.12029/gc20190307
shu
SUN Ningliang, ZHONG Jianhua, NI Liangtian, HAO Bing, LUO Ke, QU Junli, LIU Chuang, YANG Guanqun, CAO Mengchun. 2019. Provenance analysis and thermal evolution of Upper Triassic Yanchang Formation in the Southern Ordos Basin[J]. Geology in China, 46(3): 537-556. doi: 10.12029/gc20190307
Citation: SUN Ningliang, ZHONG Jianhua, NI Liangtian, HAO Bing, LUO Ke, QU Junli, LIU Chuang, YANG Guanqun, CAO Mengchun. 2019. Provenance analysis and thermal evolution of Upper Triassic Yanchang Formation in the Southern Ordos Basin[J]. Geology in China, 46(3): 537-556. doi: 10.12029/gc20190307
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鄂尔多斯盆地南部上三叠统延长组物源分析及热演化

  • 1.

    中国石油大学(华东)地球科学与技术学院, 山东 青岛 266580

  • 2.

    自然资源部油气资源战略研究中心, 北京 100034

  • 3.

    中国地质大学(北京)能源学院, 北京 10083

  • 基金项目:
    国家自然科学基金（41272088）及中央高校基本科研业务专项资金（15CX06002A）联合资助
详细信息
    作者简介: 孙宁亮, 男, 1987年生, 博士生, 主要从事构造和沉积方面的研究; E-mail:sunningliangll@163.com

  • 中图分类号: P597

Provenance analysis and thermal evolution of Upper Triassic Yanchang Formation in the Southern Ordos Basin

  • 1.

    School of Geosciences, China University of Petroleum, Qingdao 266580, Shandong, China

  • 2.

    Research Center of Oil & Gas Resources, Ministry of Natural Resources, Beijing 100034, China

  • 3.

    School of Energy Resources, China University of Geosciences(Beijing), Beijing 100083, China

  • Fund Project: Supported by National Natural Science Foundation (No. 41272088), Fundamental Research Funds for the Central Universities (No. 15CX06002A)
More Information
    Author Bio: SUN Ningliang, male, born in 1987, doctor candidate, engages in the study of tectonics and sedimentology; E-mail:sunningliangll@163.com .

    摘要

  • 本文以鄂尔多斯盆地南部旬邑地区上三叠统延长组为例系统研究了其物源区属性及热演化。采用碎屑锆石LA-ICP-MS定年的方法, 通过分析砂岩样品中碎屑锆石U-Pb的年龄结构及组成, 明确了其物源区属性。研究表明：长7碎屑锆石存在225~264 Ma、276~408 Ma、413~458 Ma、727~851 Ma、1249~1749 Ma和1868~2469 Ma 6个年龄区间, 分别对应于印支期、海西期、加里东晚期、Rodinia超大陆裂解、晋宁运动早中期和古元古代的构造热事件, 研究区物源复杂, 主要来自于北秦岭西段、秦祁造山带、西秦岭、祁连造山带东段及天山-兴蒙造山带, 阿拉善地块和盆地北部山区也可能为本区提供物源, 古水流分析表明研究区的物源方向为近南部。通过磷灰石裂变径迹年龄分析及热史模拟, 明确了研究区在100 Ma左右的早白垩世经历了重要的构造热事件, 是油气藏形成的重要时期。自此以后, 又经历了4次比较明显的热演化, 100~43 Ma为缓慢抬升阶段, 进入部分退火, 冷却速率大概在0.44℃/Ma, 43~36 Ma为一快速抬升阶段, 冷却速率达到4.3℃/Ma, 36~24 Ma为又一期的缓慢抬升, 冷却速率在0.52℃/Ma左右, 从24~17 Ma样品又经历了一次快速的抬升过程, 冷却速率在1.5℃/Ma左右。研究区43 Ma以来的抬升剥蚀明显受到印度板块与亚欧板块碰撞的影响。

    The sedimentary sources and thermal evolution of Upper Triassic of Yanchang Formation in Xunyi area of Southern Ordos Basin were studied in this paper. With the method of LA-ICP-MS, the detrital zircons ages and compositions of sandstone samples from the study area were analyzed so as to investigate the sedimentary sources. The results show that there exist six age stages of the Chang 7 detrital zircons, i.e., 225-264 Ma, 276-408 Ma, 413-458 Ma, 727-851 Ma, 1249-1749 Ma and 1868-2469 Ma, corresponding to the tectonic movements of Indo-Chinese, Hercynin, late Caledonian, Rodinia break-up, early-middle Jinning movement and Paleoproterozoic periods. Sedimentary sources are complex in the study area, and they mainly came from the western section of northern Qinling, Qin-Qi orogenic belt, West Qinling, eastern section of Qilian orogenic belt, and Tianshan-Xingmeng orogenic belt. Alxa block and northern area of the basin might have been the sedimentary sources of the study area. Paleo-current statistics indicate that the source direction was close to the southern part of the study area. Apatite fission track analysis and thermal history reconstruction were carried out, and the results confirm that the study area experienced an essential tectonic thermal event at 100 Ma in the early Cretaceous period of Late Mesozoic, which was an important period of oil and gas formation. There existed four relatively evident thermal evolution periods after that:100 to 43 Ma was a slow uplift stage and experienced partially annealing with a cooling rate of around 0.44℃/Ma; 45 to 36 Ma was a rapid uplift stage and the cooling rate came to 4.3℃/Ma; 36 to 24 Ma was another slow uplift stage with the cooling rate about 0.52℃/Ma; 24 to 17 Ma was a rapid uplift stage and the cooling rate came to 1.5℃/Ma. However, the India-Asia collision has influenced the uplift and erosion in the study area since 43 Ma.

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  • 图 1  鄂尔多斯盆地南部及邻区区域地质简图（据1: 500万中国地质图绘制）

    Figure 1. 

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    图 2  鄂尔多斯盆地南部延长组岩心及显微镜下照片

    Figure 2. 

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    图 3  鄂尔多斯盆地南部旬邑地区延长组长7砂岩中代表性锆石的阴极发光图像

    Figure 3. 

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    图 4  鄂尔多斯盆地南部旬邑地区延长组长7碎屑锆石年龄与Th/U关系

    Figure 4. 

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    图 5  鄂尔多斯盆地南部旬邑地区延长组长7碎屑锆石U-Pb年龄谐和图和年龄分布直方图

    Figure 5. 

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    图 6  鄂尔多斯盆地南部地区延长组磷灰石裂变径迹年龄放射图和裂变径迹长度分布图

    Figure 6. 

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    图 7  鄂尔多斯盆地南部延长组露头剖面古水流方向玫瑰花图

    Figure 7. 

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    图 8  鄂尔多斯盆地南部地区延长组热演化史模拟结果

    Figure 8. 

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    表 1  鄂尔多斯盆地南部旬邑地区延长组长7砂岩中的碎屑锆石LA-ICP-MS U-Pb测年结果

    Table 1.  Detrital zircon LA-ICP-MS U-Pb dating results in Chang7 Member of Yanchang Formation in Xunyi area of South Ordos Basin

    下载: 导出CSV

    表 2  鄂尔多斯盆地南部延长组磷灰石裂变径迹分析数据

    Table 2.  Apatite fission-track data of Yanchang Formation in the South Ordos Basin

    下载: 导出CSV

    表 3  鄂尔多斯盆地南缘周缘代表性地质体年龄值统计

    Table 3.  The dating results of representative geological bodies around the Southern Ordos Basin

    下载: 导出CSV

    表 4  鄂尔多斯盆地南部延长组古流向统计表

    Table 4.  The paleo-current statistics of Yanchang Formation in the South Ordos Basin

    下载: 导出CSV
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收稿日期:  2017-04-10
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