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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第46卷

期数:

2024年第06期

页码:

711-728

栏目:

基础地质与矿床地质

出版日期:

2024-12-15

文章信息/Info

Title:

Formation Age, Geochemical Characteristics and Geological Significance of Ergunahe Formation in Enhehada Area of Erguna Block, China

文章编号:

1672-6561(2024)06-0711-18

作者:

周传芳1; 2; 3; 魏小勇1; 2; 孙彦峰1; 2*; 王久懿1; 2; 赵文志1; 2; 张璇璞1; 2; 贾立明1; 牛广元1; 2; 齐宏运1; 2; 刘意仁1; 孟玲禹1; 付 友1

(1.中国地质调查局哈尔滨自然资源综合调查中心,黑龙江 哈尔滨 150086;2.自然资源部哈尔滨黑土地地球关键带野外科学观测研究站,黑龙江 哈尔滨 150086; 3.中国地质大学(北京)地球科学与资源学院,北京 100083)

Author(s):

ZHOU Chuan-fang1; 2; 3;  WEI Xiao-yong1; 2;  SUN Yan-feng1; 2*;  WANG Jiu-yi1; 2;  ZHAO Wen-zhi1; 2;  ZHANG Xuan-pu1; 2;  JIA Li-ming1;  NIU Guang-yuan1; 2;  QI Hong-yun1; 2;  LIU Yi-ren1;  MENG Ling-yu1;  FU You1

(1. Harbin Center for Integrated Natural Resources Survey, China Geological Survey, Harbin 150086, Heilongjiang, China; 2. Observation and Research Station of Earth Critical Zone in Black Soil of Harbin, Ministry of Natural Resources, Harbin 150086, Heilongjiang, China; 3. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China)

关键词:

地球化学;  额尔古纳河组;  变质岩;  锆石U-Pb年龄;  额尔古纳地块;  兴蒙造山带

Keywords:

geochemistry;  Ergunahe Formation;  metamorphic rock;  zircon U-Pb age;  Erguna Block;  Xing’an-Mongolian orogenic belt

分类号:

P595; P588.34

DOI:

10.19814/j.jese.2024.06027

文献标志码:

A

摘要:

额尔古纳河组是额尔古纳地块变质结晶基底重要的组成部分,记录了前寒武纪构造演化历史,但其分布面积小,自然露头差,目前研究相对较少。通过对额尔古纳地块恩和哈达地区额尔古纳河组进行系统的野外地质调查,结合LA-ICP-MS锆石U-Pb定年和岩石主量、微量元素分析,探讨了额尔古纳河组的形成时代、原岩类型、物质来源和沉积环境。结果表明:额尔古纳河组主要为一套副变质岩,绢云千枚岩和绿泥片岩质糜棱岩岩石地球化学特征总体较为相似,显示出富Si(SiO₂含量(质量分数,下同)为63.45%～79.01%)、富K(K₂O含量为2.22%～3.33%)和高Al(Al₂O₃含量为9.76%～17.10%)的特征; 锆石U-Pb加权平均年龄为(583.0±1.7)Ma,形成于新元古代震旦纪; 球粒陨石标准化稀土元素配分模式呈轻稀土元素富集、重稀土元素亏损的右倾模式,具有不明显的负Eu异常; 微量元素亏损高场强元素Nb、Ti、P和大离子亲石元素Ba、Sr,富集高场强元素Zr、Th、U、Hf和大离子亲石元素Rb; 物源以长英质砂岩为主,原岩为砂泥质岩石和中酸性火山岩,成熟度较低,为近源沉积,沉积环境为活动大陆边缘,并存在被动大陆边缘物质。

Abstract:

Ergunahe Formation is an important component of the metamorphic crystalline basement of Erguna Block, recording the Precambrian tectonic evolution history; however, it has small distribution area, poor natural outcrops, and relatively little research. Therefore, the systematic field geological survey of Ergunahe Formation in Enhehada area of Erguna Block combined with LA-ICP-MS zircon U-Pb dating, the characteristics of major and trace elements were analyzed; the formation age, protolith types, material source and sedimentary environments of Ergunahe Formation were explored. The results show that Ergunahe Formation is mainly a set of parametamorphic rocks, the sericite phyllite and chlorite schistose mylonite have similar overall petrogeochemical characteristics, showing rich Si(SiO₂ content is 63.45%-79.01%), K(K₂O content is 2.22%-3.33%)and Al(Al₂O₃ content is 9.76%-17.10%); the zircon U-Pb weighted average age is(583.0±1.7)Ma, formed in Neoproterozoic Sinian. The chondrite-normalized REE pattern shows a right-leaning pattern with enrichment of LREE and depletion of HREE, and a insignificant negative Eu anomaly. Trace elements are depleted in high field strength elements Nb, Ti, P, and large ion lithophile elements Ba, Sr, and enriched in high field strength elements Zr, Th, U, Hf, and large ion lithophile element Rb. The material source is dominated by felsic sandstone, with the protolith being sandy mudstone and intermediate-acidic volcanic rocks, indicating low maturity, proximal deposition, and a sedimentary environment of an active continental margin, and the presence of passive continental margin materials.

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备注/Memo:

收稿日期:2024-06-20; 修回日期:2024-10-04
基金项目:中国地质调查局地质调查项目(DD2016007803,DD20230504)
*通信作者:孙彦峰(1988-),男,甘肃庆阳人,中国地质调查局哈尔滨自然资源综合调查中心高级工程师,E-mail:584025657@qq.com。

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