| 鲁东碰撞带的初步研究 |
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| 引用本文： | 王来明.鲁东碰撞带的初步研究[J].山东国土资源,1994(1). |
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| 作者姓名： | 王来明 |
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| 作者单位： | 山东地矿局区域地质调查队 |
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| 摘 要： | 鲁东碰撞带是秦岭一大别碰撞带的东延部分，它由元古字变质地层混杂堆积体、花岗质片麻岩、榴辉岩、超镁铁质岩、镁铁质岩、麻粒岩及韧性剪切带组成。碰担带内存在一对平行展布的高压变质带－内部为榴辉岩带，边部为麻粒岩带。碰撞带形成于８．５亿年左右，３．２－３．５Ｍａ和２．０５－２．１３Ｍａ分别发生强烈活动，形成大规模推覆构造和走滑性韧性剪切构造。
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PKELIMINARY STUDY ON THE EASTERN SHANDONG COLLISION ZONE |
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| Wang Laiming.PKELIMINARY STUDY ON THE EASTERN SHANDONG COLLISION ZONE[J].Land and Resources in SHANDONG Province,1994(1). |
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| Authors: | Wang Laiming |
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| Abstract: | The eastern Shandong collision zone is an castern extension of the Qinling-Dabie cullisionzone between the Sino-Korcan and Yangtze cratons,which consists of the Proterozoicmetamorphic melange accumulation,granitic gneisses,eclogites,ultramafic rocks,mafic rocks,granulites and ductile-shear zones,There is a pair of parallel high-pressure meta-morphicbelts with in the collision zone in which the eclogite belt is distributed inside the zone and thegranulite belt on the margin. The collision zone was formed at ca.85OMa ago and laterexperienced strong movements at 300Ma and 200Ma ago respectively |
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