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| 贵州西北部江子山—蟒硐构造带两类铅锌矿床特征及其形成机制 | |
| 引用本文： | 陈大,黄智龙,张伦尉,龙汉生,蔡国盛,曾道国,吴林锋,刘玲.贵州西北部江子山—蟒硐构造带两类铅锌矿床特征及其形成机制[J].矿物学报,2012,32(3):432-442. |
| 作者姓名： | 陈大 黄智龙 张伦尉 龙汉生 蔡国盛 曾道国 吴林锋 刘玲 |
| 作者单位： | 1. 贵州省有色金属和核工业地质勘查局地质矿产勘查院,贵州贵阳,550005 2. 中国科学院地球化学研究所,贵州贵阳,550002 3. 贵州省有色金属和核工业地质勘查局地质矿产勘查院,贵州贵阳550005 昆明理工大学国土资源学院,云南昆明650093 |
| 摘 要： | 贵州西北部江子山—蟒硐铅锌成矿带,位于扬子板块西南缘之菱形断块北东边界断裂南东段,经历了加里东—印支期裂陷作用和燕山期褶皱造山过程,以及海西—印支期、燕山期两次岩浆活动。铅锌成矿特征显示,本区矿化层位较多,根据矿化特征分析并差异分辨,矿床类型划分为受上司组和摆佐组主控的矿床、受垭都—蟒硐断裂主控的矿床2种,成矿金属主要来源于下伏D-C铁质、炭质、泥质碎屑岩类,但硫的来源有所不同,其中第一种类型形成机制差别在于赋矿的上司组和摆佐组地层沉积了成矿主要的硫源,并在印支期和燕山期发生富金属流体上行与地层中富硫酸盐热液的混合成矿和二次叠加,矿床成因类型为层控类型;第二种类型成矿过程为构造驱动富金属成矿流体上行至构造空间,与断裂穿层逆冲过程中下行之硫酸盐流体混合成矿,矿床成因类型为热液类型;两种类型的划分对深入研究本区铅锌成矿作用和找矿实践具有参考意义。 |
| 关 键 词： | 黔西北 蟒硐 构造带 矿床特征 形成机制 |
Geological Characteristics and Formation Mechanism of Two Types Pb-Zn Deposits in Jiangzi Mountain-Mangdong Tectonic Belt |
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| CHEN Da,HUANG Zhi-long,ZHANG Lun-wei,LONG Han-sheng,CAI Guo-sheng,ZENG Dao-guo,WU Lin-feng,LIU Ling.Geological Characteristics and Formation Mechanism of Two Types Pb-Zn Deposits in Jiangzi Mountain-Mangdong Tectonic Belt[J].Acta Mineralogica Sinica,2012,32(3):432-442. | |
| Authors: | CHEN Da HUANG Zhi-long ZHANG Lun-wei LONG Han-sheng CAI Guo-sheng ZENG Dao-guo WU Lin-feng LIU Ling |
| Institution: | 1(1.Guizhou Nonferrous Metal and Nuclear Industry Geological Exploration Bureau,Guiyang 550005,China; 2.Institute of Geochemistry Chinese Academy Sciences,Guiyang,550002,China;3.Kun ming University College of Land Resources,Kunming 650093 China) |
| Abstract: | Jiangzimountain-Mangdong Pb-Zn Metallogenetic belt in Northwestern Guizhou Province is located at the southeast of NE-trending boundary fault of diamond fault-block in the southwest Margin of Yangtze plate.It has experienced riftogenesis in onian-Indosinian stages,orogenic process in Yanshan stages,and magmatic actions in Hercynian-Indosinian and Yanshan stages.Pb-Zn metallogenic characteristics show that this area have many mineralized layers.Based on mineralization characteristics,Pb-Zn deposits can be classified into following two types: one type primarily dominated by Shangsi Formation and Baizuo Formation;the other primarily dominated by Yadu-Mangdong fault.The metallogenic substance mainly comes from the ferruginous,carbon-base and pelitic clasolite in the lower strata(D-C),but the source of sulphur is different.One genetic type is stratabound ore deposit whose formation mechanism is different from the other one.As the source of sulfur,it is sedimented in Shangsi Formation and Zuobai Formation.Mixed mineralization and two superimposed between high-metal fluid and high-sulfates thermal fluid occurred in Indosinian and Yanshan stages;The other one is thermal deposit,and its mineralization processes was that tectonic movement made the high-metal fluids move up to the geological structure and be mixed with sulfate fluids from strata-dissecting fault.The division of the two kinds of Pb-Zn deposits is an important reference for further studies on mineralization and prospecting of Pb-Zn deposits in this area. |
| Keywords: | NW Guizhou Jiangzi mountain Mangdong tectonic zone geological characteristics formation mechanism |
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