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黔东北沿河县奥陶系湄潭组碎屑锆石特征、物源——构造意义及其成矿年代学启示

何垚砚, 牛志军, 张遵遵, 宋芳, 姚华舟, 杨文强, 龚银杰, 王忠伟, 甘金木, 王志宏

何垚砚, 牛志军, 张遵遵, 宋芳, 姚华舟, 杨文强, 龚银杰, 王忠伟, 甘金木, 王志宏. 黔东北沿河县奥陶系湄潭组碎屑锆石特征、物源——构造意义及其成矿年代学启示[J]. 中国地质, 2020, 47(4): 1025-1040. DOI: 10.12029/gc20200409
引用本文: 何垚砚, 牛志军, 张遵遵, 宋芳, 姚华舟, 杨文强, 龚银杰, 王忠伟, 甘金木, 王志宏. 黔东北沿河县奥陶系湄潭组碎屑锆石特征、物源——构造意义及其成矿年代学启示[J]. 中国地质, 2020, 47(4): 1025-1040. DOI: 10.12029/gc20200409
HE Yaoyan, NIU Zhijun, ZHANG Zunzun, SONG Fang, YAO Huazhou, YANG Wenqiang, GONG Yinjie, WANG Zhongwei, GAN Jinmu, WANG Zhihong. Detrital zircons of the Meitan Formation during Ordovician in Northeastern Guizhou and its significance for provenance-tectonic and implications for metallogenic chronology[J]. GEOLOGY IN CHINA, 2020, 47(4): 1025-1040. DOI: 10.12029/gc20200409
Citation: HE Yaoyan, NIU Zhijun, ZHANG Zunzun, SONG Fang, YAO Huazhou, YANG Wenqiang, GONG Yinjie, WANG Zhongwei, GAN Jinmu, WANG Zhihong. Detrital zircons of the Meitan Formation during Ordovician in Northeastern Guizhou and its significance for provenance-tectonic and implications for metallogenic chronology[J]. GEOLOGY IN CHINA, 2020, 47(4): 1025-1040. DOI: 10.12029/gc20200409

黔东北沿河县奥陶系湄潭组碎屑锆石特征、物源——构造意义及其成矿年代学启示

基金项目: 

中国地质调查局地质矿产调查评价专项项目 DD20179385

中国地质调查局地质矿产调查评价专项项目 DD20179232

国家自然科学基金项目 41272065

详细信息
    作者简介:

    何垚砚, 男, 1991年生, 博士生, 地层学与沉积地质学; E-mail:heyaoyan306@qq.com

    通讯作者:

    牛志军, 男, 1970年生, 研究员, 从事地层古生物学研究工作; E-mail:nzhijun@qq.com

  • 中图分类号: P597;P534.42

Detrital zircons of the Meitan Formation during Ordovician in Northeastern Guizhou and its significance for provenance-tectonic and implications for metallogenic chronology

Funds: 

the project of China Geological Survey DD20179385

the project of China Geological Survey DD20179232

National Natural Science Foundation of China 41272065

More Information
    Author Bio:

    HE Yaoyan, male, born in 1991, doctor candidate, majors in stratigraphy and sedimentary geology; E-mail:heyaoyan306@qq.com

    Corresponding author:

    NIU Zhijun, male, born in 1970, professor, mainly engages in the study of stratigraphy and palaeontology; E-mail:nzhijun@qq.com

  • 摘要:

    黔东北沿河县位于中扬子地区,分布有众多低温热液矿床,构造上位于加里东期前陆盆地的隆后带,是研究盆地物源-构造响应的良好场所,然而在中扬子的大部分地区,奥陶纪地层序列多以碳酸盐岩为主夹泥质岩,因而从岩性上制约了碎屑锆石年代学等定量分析手段的开展。近来,笔者注意到沿河县及周边地区下—中奥陶统湄潭组(O1-2m)为泥岩、灰岩夹(钙质)砂岩,采样分析结果表明,湄潭组碎屑锆石年龄大于1.0 Ga的锆石仅8颗(占12%)且未形成峰值,最年轻一组谐和年龄的加权平均值((457.8 ±8.1)Ma)与该组沉积上限十分接近,反映湄潭组碎屑主要来自新隆升的物源区,且具有相对较高的沉积速率。根据年龄的分布和特征峰值,可分为5组:~461 Ma(Ⅰ)、~580 Ma和~606 Ma(Ⅱ)、~722 Ma(Ⅲ)、~865 Ma(Ⅳ1)和~936 Ma(Ⅳ2),其中Eu正异常的锆石集中分布于第Ⅰ组(占62%),而在第Ⅱ组和第Ⅳ2组中缺失,结合稀土元素等的分析,认为其物源主要分为3部分,第Ⅰ组、第Ⅱ组和第Ⅳ2组、第Ⅲ和Ⅳ1组,分别主要来自3个不同的物源区,分别对应黔中隆起、扬子西缘康滇古陆(另有少量来自扬子东南缘—华夏地区)、武陵—雪峰隆起。此外,第Ⅰ组年龄450~511 Ma范围内发育了高达73%的热液锆石,与区域低温热液成矿时间对应,认为其形成是物源区流体的活跃导致的,可能与奥陶纪区域构造体制从伸展到挤压的转换有关,暗示此时加里东运动已经开始波及中扬子沿河地区,但主要表现为热液活动,并没有发生大规模岩浆作用。

    Abstract:

    Located in northeastern Guizhou of middle Yangtze area, Yanhe County has many low-temperature hydrothermal deposits. It is a good place for studying the provenance-tectonic response of the basin due to its back-bulge position during Ordovician. However, in most area of middle Yangtze, stratigraphic sequence is composed mainly of carbonate rocks intercalated with mudstone, which restricts the development of quantitative analytical methods such as the detrital zircon geochronology. Recently, the authors noticed that there are mudstone and carbonate intercalated with sandstone around Yanhe in the Metitan Formation (O1-2m) of lower-middle Ordovician. A detrital zircon sample from the sandstone shows that only 8 zircons (12%) are older than 1.0 Ga and they have no age peaks, and the weighted average of the youngest group of zircons ((457.8 ±8.1) Ma) is close to the upper limit of the Meitan Formation. This means that the detritus of the Meitan Formation was mainly derived from a newly formed source area and had a relatively high deposition rate. The age of zircons can be divided into five groups according to their age distribution and peaks: ~461 Ma (Ⅰ), ~580 Ma and ~606 Ma (Ⅱ), ~722 Ma (Ⅲ), ~865 Ma (Ⅳ1) and ~936 Ma (Ⅳ2). On the basis of isotope ratio and REE, the authors consider that the ages can be divided into three parts:Ⅰ, Ⅱ and Ⅳ2, Ⅲ and Ⅳ1, which are mainly derived from three different source areas. Combined with the previous study, the authors hold that the three source areas are Qianzhong uplift, Kangdian ancient land, and Wuling-Xuefeng uplift, with Qianzhong and Kangdian being newly formed source area. What's more, there are many (73%) hydrothermal zircons in age group Ⅰ (450 ~511 Ma), and this age matches well with low-temperature hydrothermal mineralization, suggesting that it was caused by the activation of the fluid, probably due to the regional tectonic regime converted from extension to compression. This implies that the Caledonian movement had begun to affect the Yanhe area, but was mainly manifested as hydrothermal activity, with no large scale of magmatism.

  • 致谢: 中国地质调查局武汉地质调查中心同位素室卢山松在数据处理方面提出了建设性意见,审稿专家和编辑老师对本文的修改完善提出了有益的建议,在此一并表示衷心感谢。
  • 图  1   研究区地质简图(据张遵遵等,2018b修改,红色星号为本文采样位置,白色星号为前人样品点)

    1—新元古界;2—奥陶—志留系;3—中生界;4—断裂;5—寒武系;6—上古生界;7—地质界线;8—江南造山带

    Figure  1.   Sketch geological map of the study area (modified from Zhang Zunzun et al., 2018b, red star shows sample location, white stars show cited sample location)

    1-Neoproterozoic; 2-Ordovician-Silurian; 3-Mesozoic; 4-Fault; 5-Cambrian; 6-Upper Paleozoic; 7-Geological boundary; 8-Jiangnan Orogen

    图  2   实测岩石地层序列及采样层位(地层对比据汪啸风,2016;年代地层据樊隽轩等,2018

    a—湄潭组宏观露头;b—本文锆石采样处;c—湄潭组含钙细砂岩中的笔石化石

    Figure  2.   Measured stratigraphic sequence and sampling position (chronostratigraphic and stratigraphic correlation after Wang Xiaofeng, 2016 and Fan Junxuan et al., 2018)

    a-Outcrops of the Meitan Formation; b-Sampling place of this paper; c-Graptolite in calcium-bearing fine sandstone of the Meitan Formation

    图  3   碎屑锆石代表性阴极发光(CL)图像、测点位置及年龄(Ma)

    Figure  3.   Representative CL images and dating spots of the detrital zircon grains

    图  4   沿河县湄潭组碎屑锆石年龄频率分布图及与区域相当层位的对比

    a—邻近地区前寒武纪碎屑锆石年龄谱;b—云南昆明奥陶系红石崖组碎屑锆石年龄谱;c—贵州沿河湄潭组碎屑锆石年龄谱;d—湖南江永奥陶系桥亭子组碎屑锆石年龄谱;e—贵州沿河湄潭组碎屑锆石年龄频率分布图(图c的局部放大)

    Figure  4.   Relative probability plots of detrital zircon sample from the Meitan Formation in Yanhe County, and correlation with its equivalent strata.

    a-Detrital zircon age spectra of Precambrian near the study area; b- Detrital zircon age spectra of the Hongshiya Formation in Kunming, Yunnan; c- Detrital zircon age spectra of the Meitan Formation in this study; d- Detrital zircon age spectra of the Qiaotingzi Formation in Jiangyong, Hunan; e-Enlargement of Fig. c

    图  5   沿河县湄潭组碎屑锆石谐和图及变质年龄分析

    (图a、b为4组年龄在谐和图中的分布,图c为最年轻1组锆石的加权平均年龄)

    Figure  5.   Concordia diagram of detrital zircon and the analyses of metamorphic age from the Meitan Formation in Yanhe County

    (Figs. a and b show the distribution of age range in concordia diagram; Fig. c shows the weighted average age of the youngest group)

    图  6   沿河县湄潭组碎屑锆石稀土元素配分曲线(a)、铕异常分布图(b)、Th/U比值分布(c)

    Figure  6.   Plot of REE patterns (a), Eu anomaly (b) and ratio of Th/U (c) from detrital zircon sample of the Yanhe Fromation, Yanhe County

    图  7   沿河地区中奥陶统湄潭组沉积时期物源组成及热液影响示意图(据黄福喜等,2011黄乐清等,2018修改)

    Figure  7.   Schematic diagram of provenance and hydrothermal area in the Yanhe area during the depositional time of the Meitan Fromation, middle Ordovician (modified from Huang Fuxi et al., 2011 and Huang Leqing et al., 2018)

    The region defined by the pink ellipse has affected by the hydrothermal activity; the arrows represent provenance of detritus

    表  1   沿河湄潭组碎屑锆石U-Pb定年及同位素数据

    Table  1   Isotope composition and age of detrital zircons from the Meitan Formation in Yanhe County

    下载: 导出CSV

    表  2   沿河湄潭组碎屑锆石(17YH)微量元素(10-6)数据

    Table  2   Trace elements of detrital zircons from the Meitan Formation in Yanhe County(10-6)

    下载: 导出CSV
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  • 收稿日期:  2019-04-03
  • 修回日期:  2020-04-07
  • 网络出版日期:  2023-09-25
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