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苏鲁高压-超高压带的结构、变形特征及形成背景探讨
引用本文:张忠义,吴淦国,宋明春,张达.苏鲁高压-超高压带的结构、变形特征及形成背景探讨[J].地球学报,2004,25(6):607-614.
作者姓名:张忠义  吴淦国  宋明春  张达
作者单位:中国地质大学,北京100083;中国地质大学,北京100083;山东省第四地质矿产勘查院,山东潍坊261021;中国地质大学,北京100083
基金项目:国土资源部科技项目(编号:2003401)
摘    要:苏鲁高压-超高压变质带由不同层次、不同级别、不同变质岩石组合的构造岩片堆叠而成,自北向南可分别为9个构造岩片。这种复杂的结构的形成和发展主要受早期的变质变形作用控制,并被晚期构造作用改造。本文重点对高压-超高压变质带的构造变形进行了分析,自元古宙—中生代韧性改造事件可分为4期。最后在以上工作的基础上对其形成的地质背景进行了探讨,指出了两次高压-超高压变质事件存在的可能,而且其新元古代的构造事件可与全球Rodinian超大陆的形成与裂解相对比。

关 键 词:高压-超高压变质带  结构  变形作用  Rodinia

Texture, Deformation and Formation Background of the Sulu High-Ultrahigh Pressure Metamorphic Belt
ZHANG Zhong-yi,WU Gan-guo,SONG Ming-chun and ZHANG Da.Texture, Deformation and Formation Background of the Sulu High-Ultrahigh Pressure Metamorphic Belt[J].Acta Geoscientia Sinica,2004,25(6):607-614.
Authors:ZHANG Zhong-yi  WU Gan-guo  SONG Ming-chun and ZHANG Da
Institution:China University of Geosciences, Beijing, 100083;China University of Geosciences, Beijing, 100083;No.4 Institute of Geological Exploration for Mineral Resources, Weifang, Shandong, 261021;China University of Geosciences, Beijing, 100083
Abstract:The Su-Lu high-ultrahigh pressure metamorphic belt results from the superimposition of tectonic slices of various grades. It can be divided into nine tectonic slices in southward direction, namely Weihai-Yangkou, Muping-Rushan, Taolin-Shangzhuang,Wulian-Jiaonan, Banquan-Rizhao, Linshu-Haitou, Donghai-Tushan, Lianyungang-Punan and Guanyun-Yangji. The formation and evolution of the complex structure were controlled mainly by early deformation and metamorphism. A study of the deformation indicates that from Proterozonic to Mesozonic the high-ultrahigh pressure metamorphic belt experienced four shear deformation stages. The investigation into the geological setting for the evolution of the high-ultrahigh pressure metamorphic belt reveals that there might have existed two high-ultrahigh metamorphic events in the evolution of the orogenic belt. The tectonic event during Neoproterozonic must have had a close relationship with global Rodinia supercontinent aggregation and cracking-disintegration.
Keywords:high-ultrahigh pressure metamorphic belt  structure  deformation  Rodinia
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