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中国东北及邻区白垩纪岩浆活动与古太平洋板块俯冲的关系
Cretaceous Magmatism in NE China and Adjacent Areas and Its Relationship with the Paleo-Pacific Plate Subduction

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文摘 本文简要综述了古太平洋构造演化历史和中国东北及邻区构造单元,总结了中国东北及邻区白垩纪岩浆活动的时空分布规律及岩石组合特征,认为中国东北额尔古纳-兴安-松辽-佳木斯地块145 ~ 88 Ma岩浆活动显著,从西向东由老变新,特征岩石组合为软流圈地幔来源玄武质岩石,以及Ⅰ型和A型花岗岩类; 88~ 65 Ma岩浆活动较弱,仅少量OIB型玄武岩。完达山-锡霍特-阿林-延边地区白垩纪岩浆活动也具有从西向东由老变新的规律,特征岩石组合为高镁安山岩、埃达克岩、I型及S型花岗岩等中酸性岩石。上述岩浆活动分别形成于弧后(板内)及大陆弧。中国东北早白垩世大陆弧具有弧后伸展,与年老大洋岩石圈的俯冲有关,是现代地球上少见的俯冲类型; 晚白垩世中晚期,弧后发生构造挤压,与智利型大陆边缘相似。
其他语种文摘 This paper briefly reviewed the tectonic evolution history of the Paleo-Pacific Plate and tectonic regimes of NE China and adjacent areas. It also summarized the spatial and temporal association and petrogenesis of Cretaceous igneous rocks,proposing its relationship with Paleo-Pacific Plate subduction. The Erguna,Xing'an,Songliao,and Jiamusi blocks of NE China have significant igneous activities in 145-88 Ma,characterized by a spatial and temporal eastward migration and an association of I-and A-type granites and asthenosphere-derived basaltic rocks,with minor OIB-type basalts after~ 88 Ma. The Cretaceous magmatism in the Wandashan-Sikhote-Alin and Yanbian area is also characterized by eastward migration but an association of intermediate to acidic rocks including high-Mg andesites,adakites,and I-and S-type granites. Cretaceous magmatism in Erguna-Xing'an-Songliao-Jiangmusi and Wandashan-Sikhote-Alin-Yanbian areas was thought to be formed in back-arc(intra-plate) and continental arc settings,respectively,and was controlled by roll-back of the Paleo- Pacific Plate. The Early Cretaceous continental arc accompanied with back-arc extension was most likely to result from subduction of old oceanic lithosphere,which rarely occurred in the modern earth. The Late Cretaceous continental arc at NE China,characterized by back-arc compression,was similar to the present Chilean continental margin.
来源 矿物岩石地球化学通报 ,2016,35(6):1090-1097 【核心库】
DOI 10.3969/j.issn.l007-2802.2016.06.003
关键词 活动大陆边缘 ; 古太平洋 ; 白垩纪 ; 俯冲后撤
地址

中国科学院广州地球化学研究所, 同位素地球化学国家重点实验室, 广州, 510640

语种 中文
文献类型 研究性论文
ISSN 1007-2802
学科 地质学
基金 国家973计划
文献收藏号 CSCD:5901615

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引证文献 11

1 李成禄 小兴安岭西北部与永新金矿有关岩浆岩的年代学和地球化学及成矿构造环境 现代地质,2017,31(6):1114-1130
被引 10

2 李成禄 黑龙江省嫩江县永新碲金矿床黄铁矿标型特征及稳定同位素研究 矿物岩石地球化学通报,2018,37(1):75-86
被引 14

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