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山东省优势大地构造相划分初步方案
引用本文:李洪奎,耿科,禚传源,王峰,刘继梅.山东省优势大地构造相划分初步方案[J].山东地质,2010(6):1-6.
作者姓名:李洪奎  耿科  禚传源  王峰  刘继梅
作者单位:山东省地质科学实验研究院,山东济南250013
摘    要:大地构造相是反映陆块区、造山系和叠加造山-裂谷相系形成演变过程中的一套岩石构造组合,是表达大陆岩石圈板块经历离散、聚合、碰撞、造山等动力学和地质构造作用过程而形成的综合产物。根据优势大地构造相的划分原则与沉积岩、火山岩、侵入岩和变质岩建造构造等特征,山东大地构造相可划分为3个相系(Ⅰ级)、4个大相(Ⅱ级)、17个相(Ⅲ级)和51个亚相(Ⅳ级)。

关 键 词:大地构造相  相系  建造与构造  岩性岩相  相划分  初步方案  山东省

Primary Scheme on Division of Geotectonic Phases in Shandong Province
LI Hongkui,GENG Ke,ZHUO Chuanyuan,WANG Feng,LIU Jimei.Primary Scheme on Division of Geotectonic Phases in Shandong Province[J].Geology of Shandong,2010(6):1-6.
Authors:LI Hongkui  GENG Ke  ZHUO Chuanyuan  WANG Feng  LIU Jimei
Institution:(Shandong Institute and Laboratory of Geological Sciences, Shandong Jinan 250013, China)
Abstract:Tectonic phase is a combination of rock structure which can reflect the formation and evolution process of land mass area, orogenic system and superimposed orogeny system. It is an integrated production formed by dynamics and geological tectonism of the continental lithospheric plate, such as discrete, aggregation, collision and orogeny. According to the division rule of superior tectonic facies and characteristics of sedimentary rocks, volcanic rocks, intrusive rocks and metamorphic rocks, tectonic phases in Shandong province can be divided into three phase systems ( Ⅰ level), four major phases ( Ⅱ level), 17 phases ( Ⅲ level) and 51 sub -phases ( Ⅵ level).
Keywords:Tectonic phases  phase system  foundation and construction  lithologic facies  phase division  primary scheme  Shandong province
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