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| 大兴安岭—小兴安岭地区中生代岩浆-构造-钼成矿地质事件序列的初步框架 | |
| 引用本文： | 刘翠,邓晋福,许立权,张昱,赵寒冬,孔维琼,李宁,罗照华,白立兵,赵国春,苏尚国.大兴安岭—小兴安岭地区中生代岩浆-构造-钼成矿地质事件序列的初步框架[J].地学前缘,2011,18(3):166-178. |
| 作者姓名： | 刘翠 邓晋福 许立权 张昱 赵寒冬 孔维琼 李宁 罗照华 白立兵 赵国春 苏尚国 |
| 作者单位： | 1. 中国地质大学(北京),北京,100083 2. 内蒙古自治区地质调查院,内蒙古呼和浩特,010020 3. 黑龙江省区域地质调查所,黑龙江哈尔滨,150080 4. 黑龙江省地质调查研究总院,黑龙江哈尔滨,150036 5. 中国地质大学(北京),北京,100083;内蒙古自治区地质调查院,内蒙古呼和浩特,010020 |
| 基金项目： | 中国地质调查局项目(1212010911028,1212010881204); 国家自然科学基金项目(40802020); 国土资源部项目(1212010633902,1212010633903,1212010711814); 中国地质大学地质过程与矿产资源国家重点实验室项目(GPMR0735) |
| 摘 要： | 兴蒙造山带是中国一条重要的成矿带.通过近几年的调查研究,以及大量人力、物力和资金投入,在该区发现了一批大、中型钼矿床,但是钼矿产出的区域地质背景还不是很清楚.对该区中生代A型花岗岩类、地质图分析以及钼矿的研究得知:(1)研究区印支期和燕山期是两个独立的造山旋回,印支期造山在220～200Ma左右结束,以区域上发育一套碱... |
| 关 键 词： | 兴蒙造山带 岩浆-构造-钼矿事件序列 中生代 成矿时代 挤压逆冲 |
A preliminary frame of magma-tectonic-Mo metallogenic events of Mesozoic Era in Da Hinggan Mountains and Xiao Hinggan Mountains areas |
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| Liu Cui,Deng Jinfu,Xu Liquan,Zhang Yu,Zhao Handong,Kong Weiqiong,Li Ning,Luo Zhaohua,Bai Libing,Zhao Guochun,Su Shanguo.A preliminary frame of magma-tectonic-Mo metallogenic events of Mesozoic Era in Da Hinggan Mountains and Xiao Hinggan Mountains areas[J].Earth Science Frontiers,2011,18(3):166-178. | |
| Authors: | Liu Cui Deng Jinfu Xu Liquan Zhang Yu Zhao Handong Kong Weiqiong Li Ning Luo Zhaohua Bai Libing Zhao Guochun Su Shanguo |
| Institution: | Liu Cui1,Deng Jinfu1,Xu Liquan2,Zhang Yu3,Zhao Handong4,Kong Weiqiong1,Li Ning1,Luo Zhaohua1,Bai Libing1,2,Zhao Guochun1,Su Shangguo11.China University of Geosciences(Beijing),Beijing 100083,China2.Geological Survey Institute of Inner Mongolia,Hohhot 010020,China3.Heilongjiang Province Institute of Regional Geology Survey,Harbin 150080,China4.Heilongjiang Institute of Geological Survey,Harbin 150036,China |
| Abstract: | Mongolia-Hinggan Orogen is an important metallogenic belt of China;many Mo-deposits were discovered in this belt recently owing to the great deal of input by government and companies.But the regional geological background of Mo-deposits remains unknown.Based on the study of igneous rocks,the regional geological maps and Mo-deposits,this paper reaches the following conclusions:(1) The Indosinian orogeny and Yanshanian orogeny are independent orogenic cycles;the Indosinian orogeny was ended at about 220-200 M... |
| Keywords: | Mongolia-Hinggan Orogen series of magmatic-tectonic-Mo metallogenic events Mesozoic Era metallogenic epoch compression-thrust events |
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