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青藏高原东北缘隆德观音店剖面碎屑锆石年龄序列及地质意义

寇琳琳 李振宏 董晓朋 崔加伟 李海龙

寇琳琳, 李振宏, 董晓朋, 等, 2021. 青藏高原东北缘隆德观音店剖面碎屑锆石年龄序列及地质意义. 地质力学学报, 27 (6): 1051-1064. DOI: 10.12090/j.issn.1006-6616.2021.27.06.085
引用本文: 寇琳琳, 李振宏, 董晓朋, 等, 2021. 青藏高原东北缘隆德观音店剖面碎屑锆石年龄序列及地质意义. 地质力学学报, 27 (6): 1051-1064. DOI: 10.12090/j.issn.1006-6616.2021.27.06.085
KOU Linlin, LI Zhenhong, DONG Xiaopeng, et al., 2021. The age sequence of the detrital zircons from the Guanyindian section in Longde, the northeastern margin of the Tibetan Plateau, and its geological significance. Journal of Geomechanics, 27 (6): 1051-1064. DOI: 10.12090/j.issn.1006-6616.2021.27.06.085
Citation: KOU Linlin, LI Zhenhong, DONG Xiaopeng, et al., 2021. The age sequence of the detrital zircons from the Guanyindian section in Longde, the northeastern margin of the Tibetan Plateau, and its geological significance. Journal of Geomechanics, 27 (6): 1051-1064. DOI: 10.12090/j.issn.1006-6616.2021.27.06.085

青藏高原东北缘隆德观音店剖面碎屑锆石年龄序列及地质意义

doi: 10.12090/j.issn.1006-6616.2021.27.06.085
基金项目: 

国家自然科学基金面上项目 41972119

中国地质调查局地质调查项目 DD20190018

详细信息
    作者简介:

    寇琳琳(1998-), 女, 在读硕士, 主要从事构造地质方面的研究工作。E-mail: 1976734800@qq.com

    通讯作者:

    李振宏(1973-), 男, 副研究员, 主要从事沉积地质与大地构造、石油地质综合研究、区域地质调查等方面的研究工作。E-mail: Lizhennhong@126.com

  • 中图分类号: P534.61

The age sequence of the detrital zircons from the Guanyindian section in Longde, the northeastern margin of the Tibetan Plateau, and its geological significance

Funds: 

the National Natural Science Foundation of China 41972119

the Geological Survey Project of China Geological Survey DD20190018

  • 摘要: 青藏高原东北缘古近纪—新近纪地层的精确时代和高原隆升扩展何时影响到东北缘地区一直是地质学家争论的焦点。此次以青藏高原东北缘隆德观音店剖面为研究对象,采用碎屑锆石U-Pb测年方法,结合区域古生物化石鉴定、古地磁测年结果,针对上述两个问题提出了新的认识。测试分析发现,青藏高原东北缘古近系清水营组上部碎屑锆石年龄序列中最年轻的峰值为17.8 Ma,研究得出如下两个认识:清水营组的沉积时代应归属于晚渐新世—早中新世,区域上具有穿时性;青藏高原隆升向东北方向的扩展推挤作用在早中新世时期就开始影响到了海原-六盘山断裂带以西地区,区域上构造-沉积-气候之间具有协同演化的耦合关系。这一研究成果为青藏高原隆升向东推挤扩展影响到东北缘地区的起始时限提供了新的时间标尺。

     

  • 图  1  研究区区域大地构造位置图

    Figure  1.  Regional tectonic map of the study area

    图  2  研究区区域地质图(据宁夏回族自治区地质调查院, 2017修改)

    a—研究区区域地质图; b—隆德观音店剖面

    Figure  2.  Regional geological map of the study area(modified after Geological Survey Institute of Ningxia Hui Autonomous Region, 2017)

    (a)Regional geological map of the study area; (b) Guanyindian setion

    图  3  隆德观音店剖面综合地层柱状图(据宁夏回族自治区地质调查院, 2017修改)

    Figure  3.  Comprehensive stratigraphic histogram of the Guanyindian section(modified after Geological Survey Institute of Ningxia Hui Autonomous Region, 2017)

    图  4  隆德观音店剖面样品显微照片

    a、c—单偏光; b、d—正交偏光
    Q—石英; Pl—斜长石

    Figure  4.  Micrographs of samples from the Guanyindian section

    (a and c) Under single polarizing glass; (b and d) Under crossed polarizing glass
    Q-quartz; Pl-plagioclase

    图  5  古近系碎屑锆石典型阴极发光照片

    Figure  5.  Typical cathodoluminescence photos of the Paleogene detrital zircons

    图  6  隆德观音店剖面碎屑锆石U-Pb年龄谐和图

    Figure  6.  U-Pb age concordia plots of the detrital zircons from the Guanyindian section

    图  7  隆德观音店剖面碎屑锆石U-Pb年龄序列

    Figure  7.  U-Pb age sequence of the detrital zircons from the Guanyindian section

    图  8  青藏高原东北缘古近系—新近系典型对比剖面(据王伟涛, 2012修改)

    Figure  8.  Comparison diagram of three typical Paleogene-Neogene sections in the northeastern margin of the Qinghai-Tibet Plateau(modified after Wang et al., 2012)

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  • 收稿日期:  2021-04-25
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