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山西省中生代侵入岩新认识
作者姓名:张玉生  李建荣  张诚  孙华  刘伟东  侯冬红  毛永栋  孙杰
作者单位:山西省地质调查院,太原 030001
基金项目:中国地质科学院地质研究所“山西区域地质调查片区总结与服务产品开发(编号: 121201102000150012-05)”项目资助
摘    要:根据区域地质调查资料,对山西省中生代侵入岩进行分析研究,将其划分为3个岩浆系列: 碱性偏碱性系列、亚碱性(基性)中性—中酸性系列和A型花岗岩(酸性)系列。碱性偏碱性岩系列形成于后碰撞构造环境,亚碱性(基性)中性—中酸性岩系列为大陆边缘弧和大陆岛弧及后造山构造环境,A型花岗岩系列为板内大陆裂谷或与地幔热点(地幔羽)有关的构造环境,板块俯冲作用为其提供了热能和含水溶液。大地构造分区划分为华北陆块区构造岩浆省(Ⅰ级),其中包括3个岩浆带(Ⅱ级): 南兴蒙岩浆带、北秦岭岩浆带和华北东部岩浆带,每个岩浆带又可划分为2个岩浆亚带(2期岩浆作用)(Ⅲ级),各个岩浆亚带均具有板块俯冲造山带火成岩的特征和发育演化极性。该成果为解决板块构造登陆问题提供了借鉴。

关 键 词:中生代侵入岩  岩浆系列  构造环境  造山带极性  岩浆带  
收稿时间:2019-03-11

New recognition of Mesozoic intrusive rocks in Shanxi Province
Authors:ZHANG Yusheng  LI Jianrong  ZHANG Cheng  SUN Hua  LIU Weidong  HOU Donghong  MAO Yongdong  SUN Jie
Institution:Shanxi Institute of Geological Suruey, Taiyuan 030001, China
Abstract:Mesozoic intrusive rocks in Shanxi Province were divided into three magma series according to the regional geological survey, which were alkaline- subalkaline series, subalkaline (base-)—medium acid series, type A-granite (acid) series. Alkaline-subalkaline series were formed in the post-collision tectonic environment. Subalkaline (base-)—medium acid series were formed in continental island arc, continental edge arc and post-mountain tectonic environment. Type A-granite (acid) series were formed in the construction environment of in rift valley in the plate subduction or the mantle hotspots (mantle plume), and the heat and aqueous solution was provided by the plate subduction. The geotectonic division belongs to the tectonic magma provinces in North China Craton, including three magma belts (Grade II), which are southern Xingmeng magma belt, northern Qinling Mountains magma belt and eastern North China magma belt. Each magma belt can be divided into two subzones ( Stage 2 Magma Action) (Grade Ⅲ), and each subzone has the characters of igneous rocks in the plate subduction zone and the evolution polarity. This achievement can provide some reference for landing problems of the plate structure.
Keywords:Mesozoic intrusion rocks  magma series  tectonic environment  orogenic belt polarity  magma belt  
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