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西准噶尔地区洋陆转换时代:来自锆石U-Pb定年与Lu-Hf同位素的约束

徐盛林, 陈宣华, 李廷栋, 丁伟翠, 史建杰, 李冰, 马飞宙

徐盛林, 陈宣华, 李廷栋, 丁伟翠, 史建杰, 李冰, 马飞宙. 西准噶尔地区洋陆转换时代:来自锆石U-Pb定年与Lu-Hf同位素的约束[J]. 中国地质, 2019, 46(5): 1061-1078. DOI: 10.12029/gc20190508
引用本文: 徐盛林, 陈宣华, 李廷栋, 丁伟翠, 史建杰, 李冰, 马飞宙. 西准噶尔地区洋陆转换时代:来自锆石U-Pb定年与Lu-Hf同位素的约束[J]. 中国地质, 2019, 46(5): 1061-1078. DOI: 10.12029/gc20190508
XU Shenglin, CHEN Xuanhua, LI Tingdong, DING Weicui, SHI Jianjie, LI Bing, MA Feizhou. Time of the ocean-continent transition in West Junggar: Constraints from zircon U-Pb dating and Lu-Hf isotopic composition[J]. GEOLOGY IN CHINA, 2019, 46(5): 1061-1078. DOI: 10.12029/gc20190508
Citation: XU Shenglin, CHEN Xuanhua, LI Tingdong, DING Weicui, SHI Jianjie, LI Bing, MA Feizhou. Time of the ocean-continent transition in West Junggar: Constraints from zircon U-Pb dating and Lu-Hf isotopic composition[J]. GEOLOGY IN CHINA, 2019, 46(5): 1061-1078. DOI: 10.12029/gc20190508

西准噶尔地区洋陆转换时代:来自锆石U-Pb定年与Lu-Hf同位素的约束

基金项目: 

中国地质调查局地质调查项目 DD20160083

中国地质调查局地质调查项目 DD20160344- 05

中国地质调查局地质调查项目 DD20190011

中央级公益性科研院所基本科研业务费项目 CAGS-YWF201706

国家重点研发计划项目 2018YFC0603701

详细信息
    作者简介:

    徐盛林, 男, 1991年生, 博士, 构造地质学专业, 从事构造地质学、岩石地球化学研究工作; E-mail:xushenglindizhi@163.com

    通讯作者:

    陈宣华, 男, 1967年生, 研究员, 博士生导师, 主要从事深地探测研究; E-mail:xhchen@cags.ac.cn

  • 中图分类号: P597;P542

Time of the ocean-continent transition in West Junggar: Constraints from zircon U-Pb dating and Lu-Hf isotopic composition

Funds: 

China Geological Survey Program DD20160083

China Geological Survey Program DD20160344- 05

China Geological Survey Program DD20190011

Fundamental Research Funds for Central Public Welfare Research Institutes CAGS-YWF201706

Development Program of China 2018YFC0603701

More Information
    Author Bio:

    XU Shenglin, male, born in 1991, doctor, majors in structural geology, engages in research on tectonics and geochemistry; E-mail: xushenglindizhi@163.com

    Corresponding author:

    CHEN Xuanhua, male, born in 1967, professor, supervisor of doctor candidates, engages in deep earth exploration; E-mail: xhchen@cags.ac.cn

  • 摘要:

    中亚造山带西部的西准噶尔地区是古生代洋陆构造转换最显著的地区之一,但是关于该地区洋陆转换的具体时间和地壳演化至今仍存在诸多争议。本文以西准噶尔地区的庙尔沟岩体及其西北侧新发现的柱状节理流纹岩为研究对象,通过锆石U-Pb定年的方法,判断庙尔沟岩体的年龄为302.8~308.8 Ma,柱状节理流纹岩的年龄为303.6~294.5 Ma。锆石Lu-Hf同位素测试结果显示,庙尔沟岩体和柱状节理流纹岩都具有相似的高176Hf/177Hf值和高正εHft)值,具有亏损地幔的源区属性,可能来源于下地壳底部残余洋壳或火山岛弧等新生地壳发生部分熔融。结合区域地质资料和前人研究成果,将西准噶尔地区由大洋俯冲向陆内环境转变的时间限定为晚石炭-早二叠世,其基底可能是以新元古代晚期-晚古生代形成的年轻洋壳和岛弧为主,不存在古老的结晶基底。

    Abstract:

    The West Junggar area of the western Central Asian Orogenic Belt is one of the most typical regions related to transition from the ocean to the continent in the late Paleozoic. It is still controversial about the specific time of ocean-continent transition and the continental growth of the West Junggar area at present. This paper reports zircon U-Pb age and zircon Lu-Hf isotope analytical results from the Miaoergou batholith and the newly discovered columnar jointed rhyolites on the northwest side of the Miaoergou batholith, West Junggar area. The zircon U-Pb ages indicate that the Miaoergou granitoids were formed at 302.8~308.8 Ma and the columnar jointed rhyolites were formed at 303.6~294.5 Ma, which indicates that the specific time of ocean-mainland transformation of the West Junggar area is limited to the Late Carboniferous-Early Permian. The zircon Lu-Hf isotope analytical results show that the Miaoergou granitoids and rhyolites have some similar characteristics in 176Hf/177Hf ratios and εHf(t) values. High 176Hf/177Hf ratios and εHf(t) values, similar to features of depleted mantle in nature, suggest that they resulted from partial melting of juvenile crust. Integrating regional geological data and previous research, the authors have reached the conclusion that the basement of West Junggar area was composed of juvenile oceanic crust and island arc which grew from late Neoproterozoic to late Paleozoic, with no old crystalline basement.

  • 碳酸钙是全球应用最广泛的非金属矿物材料之一,它不仅是建材、造纸、塑料、涂料、橡胶、油漆、冶金等行业的原料或改性功能材料,而且在日用化工、食品、医药、卫生保健等领域发挥着独特的作用。广西贺州大理岩矿产丰富,被誉为全国“重钙之都”,但石灰岩矿(轻质碳酸钙)勘查程度低,为了加快传统产业转型升级和新经济新业态转化培育,贺州市以粤港澳大湾区市场需求为引领,将重质碳酸钙领域拓展到轻质碳酸钙、氧化钙和氢氧化钙领域,构建绿色高端碳酸钙千亿元产业集群,本次在贺州市水声肚地区开展了石灰岩矿的勘查研究工作。

    通过开展详查工作,采用大比例尺地质填图圈定含矿层位;采用勘查线的布置形式,地表施工槽探、深部系统施工钻探揭露控制,最终通过全孔采样分析,圈定有色冶金熔剂用石灰岩矿体,估算资源量,实现了快速找矿突破。同时研究分析了水声肚矿区石灰岩矿体的主要赋矿层位,矿体规模、形态、产状、厚度、品位,矿石结构构造、矿物成分、化学成分、矿石类型,确定找矿标志。

    通过项目实施,水声肚矿区熔剂用石灰岩矿的主要含矿层位为融县组下段(D3r1)和桂林组上段(D3g3)(图 1a)。融县组下段岩性为浅灰色-灰白色中厚层亮晶微晶粒屑灰岩夹纹层状含生物屑微晶灰岩,厚50~60 m;桂林组上段岩性为深灰色生物碎屑灰岩夹多层层孔虫灰岩,厚67~131 m。

    图  1  水声肚矿区地质简图(a)、层孔虫灰岩矿石和镜下照片(b)及1号勘查线剖面图(c)
    Figure  1.  Simplified geological map of the Shuishengdu area (a), microscopic photos of stromatoporoid limestone ore (b) and section of No.1 exploration line (c) in the Shuishengdu area

    通过系统工程控制和采样分析,圈出了①号熔剂用石灰岩主矿体,矿体走向延长约2350 m,倾向延长约1650 m,水平投影面积约2.05 km2。矿体剖面形态呈单斜厚大层状、板状(图 1b)。矿体平均倾向193°,平均倾角21°。通过45个钻孔施工,控制矿体厚度11.01~179.53 m,平均99.02 m。单工程品位:CaO 53.75%~54.84%,平均54.44%;MgO 0.52%~1.17%,平均0.75%;SiO2 0.20%~1.33%,平均0.48%。

    矿石结构以生物碎屑(含层孔虫、腕足类)泥晶结构(图 1c)、微晶结构为主,构造主要为块状构造。矿石矿物成分主要为方解石(约98%),含少量的泥质(约2%)。据组合分析结果:Al2O3平均含量0.24%;Fe2O3平均含量0.08%;S平均含量0.022%;P平均含量0.0019%;烧失量平均43.57%。表明矿区熔剂用石灰岩有害组分含量极低。矿石工业类型为有色冶金熔剂用石灰岩,均达一级品,部分达特级品。

    (1) 本次勘查在水声肚矿区新发现超大型有色冶金熔剂用石灰岩矿床,共估算石灰岩矿石资源量(控制+推断)为72956.46万t,矿区北部直接出露地表的石灰岩矿石量超2亿t,为贺州市碳酸钙产业转型升级提供资源保障,也为贺州市创建“广西东融先行示范区”迈开了加速步伐。

    (2) 确定水声肚地区有色冶金熔剂用石灰岩矿的主要赋矿层位为融县组下段和桂林组上段。

    项目实施过程中得到了广西贺州市自然资源局的大力支持,谨此表示感谢。

    致谢: 本文在撰写过程中,与王增振和陈泓旭博士进行了有益探讨,审稿专家对本文提出了宝贵的修改意见,在此致以诚挚的感谢!
  • 图  1   西准噶尔地区地质构造与采样位置图

    Figure  1.   Geological structure sketch map showing sampling locations in the West Junggar

    图  2   庙尔沟岩体与柱状节理流纹岩野外产出特征

    a—庙尔沟岩体碱长花岗岩;b—庙尔沟岩体花岗闪长岩;c—柱状节理流纹岩整体特征;d—流纹岩流纹构造

    Figure  2.   Outcrop photos of Miaoergou batholith and columnar jointed rhyolite

    a-Miaoergou alkali feldspar granite; b-Miaoergou granodiorite; c-Outcrop features of columnar jointed rhyolite; d-Fluidal structure

    图  3   庙尔沟花岗岩和流纹岩锆石CL图像

    Figure  3.   Zircon CL images of Miaoergou granitoids and rhyolites

    图  4   庙尔沟花岗岩类和流纹岩U-Pb测年谐和图

    Figure  4.   Zircon U-Pb concordia diagrams of Miaoergou granitoids and rhyolites

    图  5   庙尔沟花岗岩类与流纹岩锆石Hf同位素特征

    Figure  5.   Zircon Hf isotopic features of Miaoergou granitoids and rhyolites

    图  6   西准噶尔晚石炭—早二叠世构造背景模式图

    Figure  6.   Schematic diagram of the tectonic settings in the West Junggar area during Late Carboniferous and Early Permian

    图  7   二阶模式年龄(Ma)分布图解

    Figure  7.   Distribution of two-stage Hf model ages (Ma)

    表  1   庙尔沟花岗岩类与流纹岩LA-MC-ICP-MS U-Pb同位素分析结果

    Table  1   LA-ICP-MS U-Pb isotopic data of Miaoergou granitoids and rhyolites

    下载: 导出CSV

    表  2   庙尔沟花岗岩类与流纹岩Lu-Hf同位素分析结果

    Table  2   Lu-Hf isotopeic analytical results of Miaoergou granitoids and rhyolites

    下载: 导出CSV
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出版历程
  • 收稿日期:  2019-04-17
  • 修回日期:  2019-08-25
  • 网络出版日期:  2023-09-25
  • 刊出日期:  2019-10-24

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