王砚耕,陈建书,陈启飞.贵州构造—建造划分及其意义[J].贵州地质,2018,35(3):167-170,209
贵州构造—建造划分及其意义
Structure-Formation Division and Its Significance of Guizhou
  
DOI:
中文关键词:  大地构造  构造层  亚构造层  地质建造  划分  意义  贵州
英文关键词:Geotectonic  Structural layer  Sub-structural layer  Geologic formation  Division  Significance  Guizhou
基金项目:中国地质调查局项目《中国矿产地质与区域成矿规律综合研究项目》子项目《贵州省矿产资源调查成果综合集成与服务产品开发》编号:12120114058401资助。本文是《贵州省矿产资源调查成果综合集成与服务产品开发》(简称《贵州省矿产地质志》)成果。
作者单位
王砚耕 贵州省地质矿产勘查开发局贵州贵阳550000 
陈建书 贵州省地质调查院贵州贵阳550081 
陈启飞 贵州省地质调查院贵州贵阳550081 
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中文摘要:
      本文以活动论的大地构造学说为指导,对贵州新元古代至今约870百万年的地质记录进行了构造-建造的划分。以威尔逊旋回及造山作用不整合界面为依据,将其分为武陵、扬子—加里东、海西—印支、燕山和喜马拉雅5个构造层,并简述了它们的基本特征;按控制原型盆地地动力背景的不同,划分出10个亚构造层,分别注明它们在地壳结构中的所处部位——盖层或基底。依据一定地质时期和环境条件下形成的、有成因联系的岩石共生组合不同,分别划分出沉积建造49个、岩浆建造9个,并指出它们的含矿性。从而建立了贵州构造-建造完整体系,为重塑贵州地壳构造演化和探讨成矿规律奠定了基础。
英文摘要:
      In this paper, according to the geotectology of activity theory, structure-formation of about 870 million years geological record from Newprpterozoic to this day are divided in Guizhou. According to Wilson cycle and orogenic uncomfortable plane, it’s divided into 5 structural layers: Wuling, Yangtze-Caledon, Heisey-Indosinian, Yanshan and Himalaya, their basic features are also summarized: for the difference of control prototype basin dynamic background, 10 sub-structural layers are divided, their positions of crustal structure-caprock and basement are marked. According to the difference of genetic relationship rock paragenetic assemblage formed in some geologic period and environmental condition, 49 sedimentary formations and 9 magmatic formations are divided, their ore-bearing potential are pointed out. So the absolute structure-formation system are built up, it will be the base for crustal structure evolution and metallogenic regulation discussion of Guizhou.
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