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华北地区燕山期岩石圈减薄的深部过程
引用本文:邓晋福,苏尚国,赵海玲,莫宣学,肖庆辉,周肃,刘翠,赵国春.华北地区燕山期岩石圈减薄的深部过程[J].地学前缘,2003,10(3):41-50.
作者姓名:邓晋福  苏尚国  赵海玲  莫宣学  肖庆辉  周肃  刘翠  赵国春
作者单位:1. 中国地质大学,地球科学与资源学院,北京,100083
2. 国土资源部,信息中心,北京,100812
基金项目:国家自然科学基金重点项目 (4 0 2 3 40 48),国家地质调查局资助项目 (2 0 0 113900018,K1.4 1 2 ),国土资源部岩石圈项目 (2 0 0 0 10 10 2 0 2 ),科学技术部国际合作项目 (2 0 0 1cb7110 0 2 ),教育部 2 11工程项目,IGCP 43 0项目
摘    要:大陆动力学领域今后 10~ 15a的主要科学目标是 ,建立东亚大陆中新生代演化的动力学模型 ,为资源勘查、灾害减轻和环境保护提供新的预测与评价理论。未来 10~ 2 0a会诞生地幔分异作用与岩石圈成因的综合性理论 ,为建立这个理论 ,采用地质学、岩石学探针、地球化学、数字模拟等学科交叉 ,以岩浆构造事件序列和火成岩构造组合为主线 ,探索华北燕山期岩石圈巨量减薄的机制与过程 ,对流地幔物质和热注入陆壳诱发壳幔相互作用、大规模岩浆活动和岩浆热构造变形之间的反馈关系。以岩石圈巨量减薄的深部过程这个视角 ,为华北地区大地构造性质的巨大转换 ,即从稳定的克拉通突发地转变为造山带的“燕山运动”或“大陆活化”提供深部动力学的科学依据。

关 键 词:华北地区  燕山期  岩石圈减薄  深部过程
文章编号:1005-2321(2003)03-0041-10
修稿时间:2003年4月20日

DEEP PROCESSES OF MESOZOIC YANSHANIAN LITHOSPHERE THINNING IN NORTH CHINA
DENG Jin-fu,SU Shang-guo,ZHAO Hai-ling,MO Xuan-xue,XIAO Qing-hui,ZHOU Su,LIU Cui,ZHAO Guo-chun.DEEP PROCESSES OF MESOZOIC YANSHANIAN LITHOSPHERE THINNING IN NORTH CHINA[J].Earth Science Frontiers,2003,10(3):41-50.
Authors:DENG Jin-fu  SU Shang-guo  ZHAO Hai-ling  MO Xuan-xue  XIAO Qing-hui  ZHOU Su  LIU Cui  ZHAO Guo-chun
Institution:DENG Jin-fu~1,SU Shang-guo~1,ZHAO Hai-ling~1,MO Xuan-xue~1,XIAO Qing-hui~2,ZHOU Su~1,LIU Cui~1,ZHAO Guo-chun~1
Abstract:The main goal of continent dynamics is creating the evolution dynamics model of Eastern Asia continent at the Mesozoic-Cenozoic era, and providing the new prediction and evaluation theory for resources exploring, disaster-reduction, and environmental protection. A general theory of mantle differentiation and lithosphere origin will be created in 10~20 years. For creating this new theory, we will use the main approaches of magmatic-tectonic event sequence and igneous petrotectonic assemblage on the basis of field geological, petrological, and geochemical studies, and numerical modelling. The following topics will be investigated: (1) Mechanism and processes of the large lithospheric thinning in the Jurassic-Cretaceous Yanshanian orogenic belt of North China; (2) Deep crust-mantle processes through input of juvenile materials and heat of mantle into crust; (3) Feedback relationship between large scale magmatism activity and magmatism-heat-deformation; (4) General model for origin and evolution of the orogenic belt and "Yanshan movement" in North China region which had a long-term tectonically stable cratonic history since the late Archean. Through those studies, we can provide the scientific evidences of deep earth dynamics for the answer of why there is a tremendous change of tectonic situation in North China in the Jurassic-Cretaceous. Namely, provide scientific evidence from deep dynamics for craton changing abruptly to the orogenic belt "Yanshan movement" or continental activation.
Keywords:North China region  Yanshanian epoch  lithospheric thinning  deep processes
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