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小兴安岭西北部卧都河地区落马湖岩群年代学及构造背景

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付俊彧, 那福超, 钱程, 杨晓平, 孙巍, 钟辉, 张广宇, 刘英才. 小兴安岭西北部卧都河地区落马湖岩群年代学及构造背景[J]. 地质与资源, 2023, 32(1): 1-13. doi: 10.13686/j.cnki.dzyzy.2023.01.001
引用本文: 付俊彧, 那福超, 钱程, 杨晓平, 孙巍, 钟辉, 张广宇, 刘英才. 小兴安岭西北部卧都河地区落马湖岩群年代学及构造背景[J]. 地质与资源, 2023, 32(1): 1-13. doi: 10.13686/j.cnki.dzyzy.2023.01.001
shu
FU Jun-yu, NA Fu-chao, QIAN Cheng, YANG Xiao-ping, SUN Wei, ZHONG Hui, ZHANG Guang-yu, LIU Ying-cai. GEOCHRONOLOGY AND TECTONIC SETTING OF LUOMAHU COMPLEX IN WODUHE AREA, NORTHWESTERN DAXINGANLING MOUNTAINS[J]. Geology and Resources, 2023, 32(1): 1-13. doi: 10.13686/j.cnki.dzyzy.2023.01.001
Citation: FU Jun-yu, NA Fu-chao, QIAN Cheng, YANG Xiao-ping, SUN Wei, ZHONG Hui, ZHANG Guang-yu, LIU Ying-cai. GEOCHRONOLOGY AND TECTONIC SETTING OF LUOMAHU COMPLEX IN WODUHE AREA, NORTHWESTERN DAXINGANLING MOUNTAINS[J]. Geology and Resources, 2023, 32(1): 1-13. doi: 10.13686/j.cnki.dzyzy.2023.01.001
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小兴安岭西北部卧都河地区落马湖岩群年代学及构造背景

  • 中国地质调查局 沈阳地质调查中心, 辽宁 沈阳 110034

  • 基金项目:
    中国地质调查局项目"东北地区区域基础地质调查"(编号DD20221632);"中国大地构造演化和国际亚洲大地构造图编制"(编号DD20190360)
详细信息
    作者简介: 付俊彧(1966-), 男, 正高级工程师, 主要从事区域地质矿产研究, 通信地址 辽宁省沈阳市皇姑区黄河北大街280号, E-mail//fjyzxy@163.com
    通讯作者: 钟辉(1964-), 女, 正高级工程师, 主要从事岩石学及矿物学研究工作, 通信地址 辽宁省沈阳市皇姑区黄河北大街280号, E-mail//2418734955@qq.com

  • 中图分类号: P597.1

GEOCHRONOLOGY AND TECTONIC SETTING OF LUOMAHU COMPLEX IN WODUHE AREA, NORTHWESTERN DAXINGANLING MOUNTAINS

  • Shenyang Center of China Geological Survey, Shenyang 110034, China

More Information

    摘要

  • 出露于小兴安岭西北部的"落马湖岩群"是多宝山矿集区重要的地质建造之一, 由于缺少化石及顶底不全, 其形成时代一直存在争议, 制约了对区域构造演化及成矿背景的认识. 为了探讨其形成时代及古构造背景, 采用锆石U-Pb(LA-ICP-MS)方法对卧都河乡附近的"落马湖岩群"变粉砂质泥岩的碎屑锆石进行了年代学研究, 85个测点中68个有效测点年龄介于216~2 636 Ma, 分为8个年龄组: 216~347 Ma (n=8)、430~443 Ma (n=2)、463~502 Ma (加权平均485±5 Ma, n=21)、513~572 Ma (加权平均528±7 Ma, n=16)、596~613 Ma (加权平均606±12 Ma, n=7)、718~739 Ma (加权平均730±12 Ma, n=3)、830~882 Ma (加权平均850±26 Ma, n=5)、1 769~2 636 Ma (n=6), 以第Ⅲ-第Ⅶ年龄组构成明显的峰值. 综合分析锆石晶态、CL图像、U含量特征及地质体宏观岩相学特点, 认为第Ⅲ年龄组代表样品层位沉积下限. 结合区域研究成果, 认为"落马湖岩群"形成于奥陶纪至志留纪罗德洛世; 其碎屑锆石主要来源于"额尔古纳-兴安联合地块"及奥陶纪弧火山岩区, 形成于弧后盆地构造背景; 其与多宝山弧岩浆岩带共同构成早古生代弧-盆系.

    Due to the lack of fossils and incomplete roof and bottom, the forming age of Luomahu Complex, one of the important geological formations in Duobaoshan ore concentration area, has been controversial, restricting the cognition of regional tectonic evolution and metallogenic background. The geochronology of detrital zircons in meta-silty mudstones from Luomahu Complex near Wuduhe Township are studied by zircon U-Pb LA-ICP-MS dating method to investigate the formation age and paleotectonic setting. Among the 85 survey points, 68 effective ones range in age from 216 to 2 636 Ma and can be divided into eight age groups: 216-347 Ma, 430-443 Ma, 463-502 Ma, 513-572 Ma, 596-613 Ma, 718-739 Ma, 830-882 Ma and 1 769-2 636 Ma, with the third to seventh groups forming obvious peak values. Based on the comprehensive analysis of zircon crystalline state, CL image, U content characteristics and macro petrographic features of geological body, it is considered that the third age group represents the maximum sedimentary age of sample layers. Combined with the regional research results, it is concluded that Luomahu Complex was formed in Ordovician-Silurian Ludlovian, with the detrital zircons mainly derived from the Erguna-Xing'an block and Ordovician arc volcanic rocks and formed in the tectonic setting of back-arc basin. The Luomahu Complex, together with Duobaoshan arc magmatic belt, formed the Early Paleozoic arc-basin system.

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  • 图 1  小兴安岭西北部卧都河地区地质简图

    Figure 1. 

    下载: 全尺寸图片 幻灯片

    图 2  变粉砂质泥岩岩相学特征

    Figure 2. 

    下载: 全尺寸图片 幻灯片

    图 3  变粉砂质泥岩（17W06TW1）锆石U－Pb年龄谐和图

    Figure 3. 

    下载: 全尺寸图片 幻灯片

    图 4  变粉砂质泥岩典型锆石CL图像

    Figure 4. 

    下载: 全尺寸图片 幻灯片

    图 5  落马湖群碎屑锆石U－Pb年龄频率

    Figure 5. 

    下载: 全尺寸图片 幻灯片
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收稿日期:  2022-03-07
修回日期:  2022-04-11
刊出日期:  2023-02-25

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