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胶东—苏北构造带特征及动力学演化
引用本文:韩宗珠,赵广涛.胶东—苏北构造带特征及动力学演化[J].中国海洋大学学报(自然科学版),1992(3).
作者姓名:韩宗珠  赵广涛
作者单位:青岛海洋大学海洋地质系 (韩宗珠),青岛海洋大学矿物资源研究所(赵广涛)
摘    要:提出胶东—苏北构造带以广泛出露榴辉岩和超基性岩、普遍发育韧性剪切带和糜棱岩带为特征,具混杂岩特点。它经历了早元古代大陆推覆构造事件(2000~2400Ma)、早元古代末低角闪岩相变质热事件(1800~2000Ma)和元古代末大陆推覆构造事件(6O0~800Ma)。该构造带是华北陆块与华南陆块之间的过渡带。

关 键 词:胶东—苏北构造带  榴辉岩  超基性岩  韧性剪切带  糜棱岩带  大陆推覆构造  变质作用

THE FEATURE OF THE EASTERN SHANDONG-NORTHERN JIANGSU TECTONIC ZONE AND ITS DYNAMICAL EVOLUTION
Han Zongzhu.THE FEATURE OF THE EASTERN SHANDONG-NORTHERN JIANGSU TECTONIC ZONE AND ITS DYNAMICAL EVOLUTION[J].Periodical of Ocean University of China,1992(3).
Authors:Han Zongzhu
Institution:Han Zongzhu(Department of Marine Geology)Zhao Guangtao(Institute of Mineral Resources)
Abstract:The eastern Shandong-northern Jiangsu tectonic zone has the characteristics of wide-ranging emergence of eclogites and ultrabasic rocks,wide-spread growth of tenacity shearing zone and mylonite zones.It possesses the properties of mingle rocks.It underwent the continental napping event at the Suberthem(2000-2400Ma),the amphiboleface metamorphism event at the late Suberthem (1800-2000Ma) and the continental napping event at the late Proterozoic era(600-800Ma).This tectonic zone was a trantition zone between the northern China plate and the southern China plate.
Keywords:eastern Shandong-northern Jiangsu tectonic zone  eclogite  ultrabasic rock  tenacity shearing zone  mylonite zone  continental napping  metamorphism
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