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    昌宁-孟连结合带中三叠世含放射虫硅质岩地层的古特提斯意义

    罗亮 谢韬 王冬兵 黄晓明 姜丽莉 李建忠 彭智敏

    罗亮, 谢韬, 王冬兵, 黄晓明, 姜丽莉, 李建忠, 彭智敏, 2020. 昌宁-孟连结合带中三叠世含放射虫硅质岩地层的古特提斯意义. 地球科学, 45(8): 3014-3027. doi: 10.3799/dqkx.2020.093
    引用本文: 罗亮, 谢韬, 王冬兵, 黄晓明, 姜丽莉, 李建忠, 彭智敏, 2020. 昌宁-孟连结合带中三叠世含放射虫硅质岩地层的古特提斯意义. 地球科学, 45(8): 3014-3027. doi: 10.3799/dqkx.2020.093
    Luo Liang, Xie Tao, Wang Dongbing, Huang Xiaoming, Jiang Lili, Li Jianzhong, Peng Zhimin, 2020. Radiolarian Chert Strata in Middle Triassic from Changning-Menglian Suture Zone and Implications for Paleo-Tethys. Earth Science, 45(8): 3014-3027. doi: 10.3799/dqkx.2020.093
    Citation: Luo Liang, Xie Tao, Wang Dongbing, Huang Xiaoming, Jiang Lili, Li Jianzhong, Peng Zhimin, 2020. Radiolarian Chert Strata in Middle Triassic from Changning-Menglian Suture Zone and Implications for Paleo-Tethys. Earth Science, 45(8): 3014-3027. doi: 10.3799/dqkx.2020.093

    昌宁-孟连结合带中三叠世含放射虫硅质岩地层的古特提斯意义

    doi: 10.3799/dqkx.2020.093
    基金项目: 

    中国地质调查局项目 DD20190053

    中国地质调查局项目 DD20160016

    国家自然科学基金项目 41802031

    第二次青藏高原综合科学考察研究项目 2019QZKK0702

    详细信息
      作者简介:

      罗亮(1987-), 男, 工程师, 主要从事地层学、沉积学与微体古生物学研究.ORCID:0000-0002-4963-1482.E-mail:lianglcgs@126.com

    • 中图分类号: P581

    Radiolarian Chert Strata in Middle Triassic from Changning-Menglian Suture Zone and Implications for Paleo-Tethys

    • 摘要: 昌宁-孟连结合带中三叠世地层记录了古特提斯洋晚期演化信息,为正确认识古特提斯构造古地理格局提供了重要的解剖窗口.云南省沧源县团结地区原划泥盆系曼信组岩性为硅质岩与泥岩互层夹砂岩层(透镜体),对其中长石砂岩和硅质岩分别开展锆石U-Pb测年和地球化学分析,在限定该地层时代的基础上探讨其古特提斯演化意义.长石砂岩夹层和透镜体碎屑锆石定年显示其时代分别不早于237.8±1.3 Ma和237.7±1.4 Ma,赋存地层区域上可与牡音河组对比.本次中三叠世放射虫硅质岩地层的发现,填补了本区残余盆地沉积记录.该地层中硅质岩的地球化学特征反映其形成于大陆边缘环境,结合其中陆源碎屑岩碎屑组分和副矿物特征,表明古特提斯残余洋盆规模有限.研究区三岔河组磨拉石沉积角度不整合于早期地层之上标志着残余洋盆最终闭合.

       

    • 图  1  西南三江南段构造简图(a)和团结地区地质图(b)

      图a据潘桂棠等(2013)修改;I.羌塘-三江造山系,I1.哀牢山结合带,I2.兰坪-思茅地块,I2-1.墨江-绿春陆缘弧,I2-2.兰坪-思茅盆地,I3.乌兰乌拉-澜沧江结合带,I3-1.临南澜沧江俯冲增生杂岩,I4.左贡-临沧地块,I4-1.临沧地块,II.昌宁-孟连对接带,II1.昌宁-孟连结合带,II2.双江-澜沧俯冲杂岩带,Ш.冈底斯-腾冲造山系,Ш1.保山-镇康地块,Ш2.腾冲-梁河岩浆弧.图b据云南省地质调查院, 2003, 1:25万临沧、滚龙幅(国内部分)区域地质报告. 1.早石炭世基性岩(平掌组);2.“泥盆纪硅质岩与泥岩互层夹砂岩(温泉组和曼信组)”;3.石炭-二叠纪灰岩(鱼塘寨组);4.中二叠世灰岩(大名山组);5.二叠纪浅变质碎屑岩(拉巴组);6.泥盆-石炭纪浅变质碎屑岩(南段组); 7.劈理产状;8.层理产状;9.整合接触接线;10.逆断层;11.不明性质断层;12.道路;13.锆石U-Pb采样点

      Fig.  1.  Tectonic map of southern Sanjiang in Southwest China (a) and geological map of the Tuanjie area (b)

      图  2  昌宁-孟连结合带原划泥盆系曼信组中放射虫硅质岩的野外(a、b)及显微结构照片(c、d)

      Fig.  2.  Field (a, b) and microstructure (c, d) photos of the radiolarian cherts from the original Devonian Manxin Formation in the Changning-Menglian suture zone

      图  3  昌宁-孟连结合带原划泥盆系曼信组中长石砂岩野外及显微结构照片

      a.PM101-7TW1野外照片;b.PM101-7TW1显微照片;c.PM101-18TW1野外照片;d.PM101-18TW1显微照片. Q.石英;Fsp.长石

      Fig.  3.  Field and microstructure photos of the arkose from the original Devonian Manxin Formation in the Changning-Menglian suture zone

      图  4  昌宁-孟连结合带中三叠世长石砂岩碎屑锆石U-Pb年龄

      a、d.谐和图;b、e.年龄相对频分布图;c、f.部分锆石CL图像

      Fig.  4.  Detrital zircon U-Pb ages of arkose from Middle Triassic in the Changning- Menglian suture zone

      图  5  昌宁-孟连结合带中三叠世硅质岩Al-Fe-Mn图解(a)和NASC(北美页岩)标准化稀土元素配分曲线(b)

      图a据Adachi et al.(1986);图b标准化数据据Gromet et al.(1984)

      Fig.  5.  Al-Fe-Mn diagram (a) and NASC-normalized REE patterns (b) of the radiolarian cherts from Middle Triassic in the Changning-Menglian suture zone

      图  6  昌宁-孟连结合带中三叠世硅质岩Fe2O3/TiO2-Al2O3/(Al2O3+Fe2O3)(a)和Fe2O3/(100-SiO2)-Al2O3/(100-SiO2)(b)图解

      据Murray(1994)

      Fig.  6.  Fe2O3/TiO2-Al2O3/(Al2O3+Fe2O3) (a) and Fe2O3/(100-SiO2)-Al2O3/(100-SiO2) (b) diagrams of the radiolarian cherts from Middle Triassic in the Changning-Menglian suture zone

      表  1  昌宁-孟连结合带中三叠世硅质岩与典型硅质岩稀土元素特征对比

      Table  1.   Comparison of geochemical parameters of the rare earth elements between the Middle Triassic chert in the Changning-Menglian suture zone and other typical cherts

      类型 环境 ∑REE(10-6 Ce/Ce* Eu/Eu* (La/Yb)N 文献来源
      现代大洋硅质岩 太平洋洋盆 5~132 0.19~0.61 0.67~1.63 0.48~1.97 Murray et al., 1992
      大西洋洋盆 9~189 0.47~1.12 0.91~1.18 0.76~1.86
      南极周缘洋盆 35~160 0.98~1.17 0.78~0.88 1.27~1.56
      古特提斯洋 大洋中脊 7.21~21.85 0.31~0.44 0.37~1.47 0.63~1.81 丁林和钟大赉,1995
      大洋盆地 15.89~90.52 0.49~0.80 0.48~0.86 0.52~1.86
      大陆边缘 8.46~63.32 0.72~0.98 0.57~0.84 0.59~2.27
      研究区硅质岩 34.20~237.62 0.92~1.11 0.68~1.02 0.52~1.96
      下载: 导出CSV
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