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| 黑龙江伊春地区早中生代花岗岩成矿作用 及成矿能力差异性探讨 | |
| 引用本文： | 李仰春.黑龙江伊春地区早中生代花岗岩成矿作用 及成矿能力差异性探讨[J].地质与勘探,2013,49(1):28-38. |
| 作者姓名： | 李仰春 |
| 作者单位： | 1. 中国地质大学(北京)地球科学与资源学院,中国地质大学地质过程与矿产资源国家重点实验室,北京100083;中国地质调查局发展研究中心,北京100037 2. 中国地质调查局发展研究中心,北京,100037 3. 中国地质大学(北京)地球科学与资源学院,中国地质大学地质过程与矿产资源国家重点实验室,北京100083 |
| 基金项目： | 中国地质调查局基础地质调查项目 |
| 摘 要： | 伊春地区晚三叠世-早侏罗世花岗岩分布广泛,岩石主要类型有似斑状二长花岗岩-二长花岗斑岩、正长-碱长-碱性花岗岩等,在该地区已发现的与早中生代花岗岩侵入密切相关的铁多金属及金等大小矿床的成因类型主要为斑岩型、矽卡岩型、矽卡岩-热液型、岩浆热液型、浅成低温热液型等,成岩、成矿时代为晚三叠世-早侏罗世(U-Pb锆石LA-ICPMS年龄为191～225Ma之间),成矿时代略晚于成岩时代.依据早中生代花岗岩岩石类型、时代、构造-岩浆演化、花岗岩成因类型及其陆陆碰撞不同阶段构造背景下的成矿作用特征,将矿床成矿系列划分为:碰撞-碰撞后构造转换型似斑状二长花岗岩-二长花岗斑岩Mo-Pb-Zn-Fe-W-Au (Ag)成矿亚系列和碰撞后崩塌型正长-碱长-碱性花岗岩Fe-Mo-Pb-Zn-NbTa成矿亚系列,其成矿元素、矿化强度、类型等成矿特征上的差异,可能与源区物源、壳幔混合程度、混合比例和侵位深度,以及与成矿构造背景不同等综合因素有关. |
| 关 键 词： | 早中生代花岗岩 矿床成矿系列 成矿作用 成矿能力差异性 伊春地区 |
| 收稿时间： | 2012/4/22 0:00:00 |
| 修稿时间： | 2012/10/26 0:00:00 |
Metallogenesis and Metallogenic Differences of the Early Mesozoic Granites in the Yichun Area, Heilongjiang Province |
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| LI Yang-chun.Metallogenesis and Metallogenic Differences of the Early Mesozoic Granites in the Yichun Area, Heilongjiang Province[J].Geology and Prospecting,2013,49(1):28-38. | |
| Authors: | LI Yang-chun |
| Institution: | Metallogenesis and Metallogenic Differences of the Early Mesozoic Granites in the Yichun Area, Heilongjiang Province |
| Abstract: | Abstract: The late Triassic to early Jurassic granites are widely distributed in the Yichun area, Heilongjiang Province, which are dominated by porphyaceous monzonitic granite, monzonitic granite porphyry, syenogranite, alkali-feldspar granite and alkali granite. And the discovered iron-plolymetallic deposits and gold deposits related to these rocks are mainly of porphyry, skarn, skarn-hydrothermal, magmatic hydrothermal and epithermal hydrothermal types. The major rock-forming and ore-forming ages are late Triassic to early Jurassic (U-Pb zircon LA-ICPMS age of 191~225Ma), and the ore-forming age is slightly later than the metallogenic epoch. This paper studies the major rock types, geologic ages, tectono-magmatic evolution, genetic types of the early Mesozoic granites and mineralization characteristics of different continental-collision stages. We divide the metallogenic series into two metallogenic subseries: the Mo-Pb-Zn-Fe-W-Au(Ag) metallogenic subseries of porphyaceous monzonitic granite-monzonitic granite porphyry of continental collisional-postcollisional structural transposition and the Fe-Mo-Pb-Zn-NbTa metallogenic subseries of syenogranite-alkali-feldspar granite-alkali granite of postcollisional collapse episode. These two metallogenic subseries differ in metallogenic features, i.e., ore-forming elements, mineralization intensity and types. And these differences are related with granite source areas, the degree of crust-mantle mixture, mixture ratio, granite emplacement depth and metallogenic tectonic background. |
| Keywords: | early Mesozoic granites metallogenic series metallogenesis metallogenic difference Yichun area |
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