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

卷:

第42卷

期数:

2020年第06期

页码:

819-832

栏目:

非主题来稿

出版日期:

2020-11-15

文章信息/Info

Title:

Paleo-Pacific Subduction in Early Jurassic: Geochronological and Geochemical Evidences of Gabbros in Helong Area of Yanbian, Jilin, China

文章编号:

1672-6561(2020)06-0819-14

作者:

张超¹; 2; 王路远¹; 耿瑞³; 刘正宏²; 4; 张乐彤⁵

1. 山东理工大学 资源与环境工程学院,山东 淄博 255000; 2. 自然资源部东北亚矿产资源评价重点实验室, 吉林 长春 130026; 3. 山东黄金集团有限公司,山东 济南 250101; 4. 吉林大学 地球科学学院,吉林 长春 130061; 5. 黑龙江省地球物理地球化学勘查院,黑龙江 哈尔滨 150036

Author(s):

ZHANG Chao¹; 2;  WANG Lu-yuan¹;  GENG Rui³;  LIU Zheng-hong²; 4;  ZHANG Le-tong⁵

1. School of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255000, Shandong, China; 2. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130026, Jilin, China; 3. Shandong Gold Group Co. Ltd., Jinan 250101, Shandong, China; 4. College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China; 5. Heilongjiang Institute of Geophysical and Geochemical Exploration, Harbin 150036, Heilongjiang, China

关键词:

辉长岩;  锆石U-Pb年龄;  Hf同位素;  早侏罗世;  活动大陆边缘;  古太平洋板块;  兴蒙造山带南缘;  吉林

Keywords:

gabbro;  zircon U-Pb age;  Hf isotope;  Early Jurassic;  active continental margin;  paleo-Pacific plate;  the southern Xing-Meng orogenic belt;  Jilin

分类号:

P581; P597

DOI:

10.19814/j.jese.2020.08019

文献标志码:

A

摘要:

吉林延边地区位于兴蒙造山带南缘东段,是古亚洲洋构造域和环太平洋构造域叠加与改造的地区。为确定吉林延边和龙地区沙松顶子辉长岩侵位时代和成因,探讨其大地构造背景,对沙松顶子辉长岩进行了岩相学、锆石U-Pb年代学、Hf同位素和地球化学分析。结果表明:沙松顶子辉长岩LA-ICP-MS锆石U-Pb加权平均年龄为(175.6±1.1)Ma,为早侏罗世晚期; 辉长岩具低Si、高Al特征和较高的Mg^#值,并含有较高的Cr、Ni、V、Co和Sc含量,Zr/Hf和Ba/Rb值具有幔源岩浆岩的特征,Nb/U值接近大陆地壳,反映沙松顶子辉长岩原始岩浆在上升过程中有陆壳物质的加入; 辉长岩稀土元素总含量较低,弱富集轻稀土元素,富集大离子亲石元素Cs、K、Sr等,亏损Nb、Ta等高场强元素,具有正Eu异常,地球化学特征表现出俯冲环境下形成的基性岩浆岩特征; 辉长岩具有显著亏损的Hf同位素组成特征,ε_Hf(t)为2.5～7.0,均为正值,说明辉长岩原始岩浆应起源于高度亏损的地幔。综上所述,沙松顶子辉长岩形成于古太平洋俯冲作用下活动大陆边缘的构造环境,其原始岩浆可能来源于亏损地幔,并遭受俯冲板片析出流体的交代作用和地壳物质的混染。

Abstract:

Yanbian area in Jilin, located at the eastern segment of the southern Xing-Meng orogenic belt, is an overlapped and transformed area between the paleo-Asian ocean and paleo-Pacific ocean tectonic domains. In order to confirm the emplaced age and discuss the petrogenesis and tectonic setting of Shasongdizi gabbros in Helong area of Yanbian, Jilin, the petrography, zircon U-Pb geochronology, Hf isotopic data and geochemistry of the gabbros were analyzed. The results show that the emplaced age of Shasongdingzi gabbro is in late Early Jurassic with the weighted mean age of(175.6±1.1)Ma; gabbros are characterized by the low SiO₂ contents and high Al₂O₃ contents, while the samples have high Cr, Ni, V, Co, Sc contents and Mg^# values; meanwhile, the ratios of Zr/Hf and Ba/Rb are similar to the ones of mantle igneous rocks, the ratios of Nb/U are similar to the ones of continental crust, indicating that the continental contamination occurs during evolution; gabbros have low total REE contents and positive Eu anomaly; all the samples are slightly enriched in LREE and enriched in LILE such as Cs, K, Sr, and depleted in HFSE such as Nb and Ta. The geochemical features suggest that the gabbros have subduction-reformed lithospheric mantle-derived primary magma contaminated by upper crustal materials during evolution. The gabbros have depleted Hf isotopic compositions with ε_Hf(t)of 2.5-7.0. In summary, the primary magma of gabbros may be from the depleted mantle, which is metasomatized by fluids from subducted oceanic slab and is contaminated by the crustal materials. Furthermore, the Shasongdingzi gabbros form in an active continental margin during the subduction of paleo-Pacific.

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备注/Memo

备注/Memo:

收稿日期:2020-08-13; 修回日期:2020-10-16; 网络首发日期:2020-11-20投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41802238); 国家重点研发计划项目(2017YFC0601300-01); 泰山学者计划项目(TS20190918); 国土资源部东北亚矿产资源评价重点实验室开放项目(DBY-KF-18-11)
作者简介:张 超(1986-),男,山东桓台人,山东理工大学讲师,理学博士,E-mail:czhang@sdut.edu.cn。

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更新日期/Last Update: 2020-12-20