|本期目录/Table of Contents|

[1]蔡昊龙,郭晋威,刘彬*,等.东海盆地丽水凹陷中侏罗世埃达克质花岗闪长岩地球化学特征、岩石成因及构造意义[J].地球科学与环境学报,2025,47(05):912-928.[doi:10.19814/j.jese.2025.02024]
　CAI Hao-long,GUO Jin-wei,LIU Bin*,et al.Geochemical Characteristics, Petrogenesis and Tectonic Implications of Mid-Jurassic Adakitic Granodiorites in Lishui Sag of East China Sea Basin[J].Journal of Earth Sciences and Environment,2025,47(05):912-928.[doi:10.19814/j.jese.2025.02024]
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东海盆地丽水凹陷中侏罗世埃达克质花岗闪长岩地球化学特征、岩石成因及构造意义(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第47卷
期数:
2025年第05期
页码:
912-928
栏目:
基础地质与矿床地质
出版日期:
2025-10-01

文章信息/Info

Title:
Geochemical Characteristics, Petrogenesis and Tectonic Implications of Mid-Jurassic Adakitic Granodiorites in Lishui Sag of East China Sea Basin
文章编号:
1672-6561(2025)05-0912-17
作者:
蔡昊龙1; 郭晋威1; 刘彬1; 2*; 黄晓松3; 唐贤君3; 朱正平1; 程琦1
(1. 长江大学 地球科学学院,湖北 武汉 430100; 2. 长江大学 非常规油气地质与工程湖北省工程研究中心,湖北 武汉 430100; 3. 中海石油(中国)有限公司上海分公司,上海 200335)
Author(s):
CAI Hao-long1;  GUO Jin-wei1;  LIU Bin1; 2*;  HUANG Xiao-song3;  TANG Xian-jun3;  ZHU Zheng-ping1;  CHENG Qi1
(1. School of Geosciences, Yangtze University, Wuhan 430100, Hubei, China; 2. Hubei Engineering Research Center of Unconventional Petroleum Geology and Engineering, Yangtze University, Wuhan 430100, Hubei, China; 3. Shanghai Branch of CNOOC(China)Ltd., Shanghai 200335, China)
关键词:
地球化学;  埃达克岩;  花岗闪长岩;  锆石U-Pb年龄;  侏罗纪;  岩浆弧带;  古太平洋板块俯冲;  东海盆地
Keywords:
geochemistry;  adakite;  granodiorite;  zircon U-Pb age;  Jurassic;  magma arc belt;  Paleo-Pacific Plate subduction;  East China Sea Basin
分类号:
P587; P597
DOI:
10.19814/j.jese.2025.02024
文献标志码:
A
摘要:
目前对东海盆地丽水凹陷内的埃达克岩研究较少,该岩石成因以及与古太平洋板块俯冲过程之间的联系仍缺乏系统的认识。以新钻遇的丽水凹陷埃达克质花岗闪长岩为研究对象,开展了全岩地球化学以及锆石U-Pb年代学研究,并分析了该埃达克质花岗闪长岩的成因机制以及所处的构造环境,最后探讨了东海盆地丽水凹陷侏罗纪构造背景以及古太平洋板俯冲与岩浆弧带的关系。结果表明:锆石U-Pb定年得到其岩石结晶年龄为(170.9±1.3)、(171.7±1.1)Ma; 全岩地球化学特征显示出相对较高的Sr/Y值、La/Yb值和较低的Ni和MgO含量,与下地壳来源的C型埃达克岩的地球化学特征一致; Mg#值、K2O含量和Na2O/K2O值暗示其可能源于加厚下地壳的部分熔融。丽水凹陷花岗闪长岩与邻区同时代的东海盆地瓯江凹陷花岗闪长岩、南海地区及日本飞弹地区的弧岩浆岩,可能在中国东部沿海地区共同组成了一条SW—NE向岩浆弧带。总之,这一岩浆弧带的形成与中生代古太平洋板块俯冲导致的挤压构造背景密切相关,体现了燕山运动对东海盆地所在区域的影响,可能引发中国东部沿海局部地区(如丽水凹陷)的地壳增厚。
Abstract:
Currently, the research on adakitic rocks in Lishui sag of East China Sea Basin is relatively limited, and there is still a lack of systematic understanding regarding their genesis and their connection with the Paleo-Pacific Plate(PPP)subduction process. Whole-rock geochemical and zircon U-Pb geochronology of the newly discovered adakitic granodiorites in Lishui sag were analyzed; both the petrogenetic mechanisms and tectonic setting of the adakitic granodiorites were investigated; and Jurassic tectonic setting of Lishui sag in East China Sea Basin and the relationship between PPP subduction and associated magmatic arc belt were discussed. The results show that LA-ICP-MS zircon U-Pb dating yields crystallization ages of(170.9±1.3)and(171.7±1.1)Ma; whole-rock geochemical analyses reveal relatively high Sr/Y and La/Yb ratios, and low Ni and MgO contents, consistent with the chemical characteristics of C-type adakites derived from the lower crust; the Mg#value, K2O content, and Na2O/K2O ratio suggest that the adakitic granodiorites may originate from partial melting of thickened lower crust. Combined with the coeval granodiorites in Oujiang sag of East China Sea Basin, as well as the arc-related magmatic rocks in South China Sea and Hida region of Japan, the adakitic granodiorites collectively form a SW-NE trending magmatic arc belt along the eastern coastal region of China. In general, the formation of the magmatic arc belt is closely related to the compressional tectonic setting induced by the Mesozoic PPP subduction, showing the influence of Yanshan movement on East China Sea Basin region, which may have triggered localized crustal thickening in the eastern coastal region of China(e.g. Lishui sag).

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备注/Memo

备注/Memo:
收稿日期:2025-02-24; 修回日期:2025-05-30
基金项目:国家自然科学基金项目(42130309,41502050,42302226); 安徽省自然科学基金项目(2208085MD96)
*通信作者:刘 彬(1987-),男,湖北荆州人,教授,博士研究生导师,理学博士,E-mail:binliu@yangtzeu.edu.cn。
更新日期/Last Update: 2025-10-01