彭玉鲸, 齐成栋, 周晓东, 卢兴波, 董红辰, 李壮. 吉黑复合造山带古亚洲洋向滨太平洋构造域转换[J]. 地质与资源, 2012, 21(3): 261-265. DOI: 10.13686/j.cnki.dzyzy.2012.03.012
    引用本文: 彭玉鲸, 齐成栋, 周晓东, 卢兴波, 董红辰, 李壮. 吉黑复合造山带古亚洲洋向滨太平洋构造域转换[J]. 地质与资源, 2012, 21(3): 261-265. DOI: 10.13686/j.cnki.dzyzy.2012.03.012
    PENG Yu-jing, QI Cheng-dong, ZHOU Xiao-dong, LU Xing-bo, DONG Hong-chen, LI Zhuang. TRANSITION FROM PALEO-ASIAN OCEAN DOMAIN TO CIRCUM-PACIFIC OCEAN DOMAIN FOR THE JI-HEI COMPOSITE OROGENIC BELT: Time Mark and Relationship to Global Tectonics[J]. Geology and Resources, 2012, 21(3): 261-265. DOI: 10.13686/j.cnki.dzyzy.2012.03.012
    Citation: PENG Yu-jing, QI Cheng-dong, ZHOU Xiao-dong, LU Xing-bo, DONG Hong-chen, LI Zhuang. TRANSITION FROM PALEO-ASIAN OCEAN DOMAIN TO CIRCUM-PACIFIC OCEAN DOMAIN FOR THE JI-HEI COMPOSITE OROGENIC BELT: Time Mark and Relationship to Global Tectonics[J]. Geology and Resources, 2012, 21(3): 261-265. DOI: 10.13686/j.cnki.dzyzy.2012.03.012

    吉黑复合造山带古亚洲洋向滨太平洋构造域转换

    TRANSITION FROM PALEO-ASIAN OCEAN DOMAIN TO CIRCUM-PACIFIC OCEAN DOMAIN FOR THE JI-HEI COMPOSITE OROGENIC BELT: Time Mark and Relationship to Global Tectonics

    • 摘要: 构造运动、岩浆活动、变质作用、矿床形成等地质事件节律的耦合,表明吉黑复合造山带古亚洲洋构造体制结束的综合标志时间为250~230 Ma,太平洋构造体制启动的综合标志时间为227~222 Ma.从全球构造观之,它们受Pangaea联合古陆形成的时间(330~230 Ma)和进入新超大陆旋回(230~0 Ma)首次裂解的时间(224 Ma)所制约.

       

      Abstract: The rhythmic coupling of geological events of tectonic movement, magmatism, metamorphism, deposit formation and so on indicate that, for the Ji-Hei composite orogenic belt, the ending time of the Paleo-Asian Ocean tectonic domain is 250-230 Ma; while the starting time of the Pacific Ocean tectonic domain is 227-222 Ma. From the view of global tectonics, they are constrained by the forming time of Pangaea (330-230 Ma) and its first splitting time (224 Ma) after it entered the new super-continent cycle(230-0 Ma).

       

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