| 黑龙江老柞山金矿床地质、地球化学特征及其成矿构造背景 |
| |
| 引用本文： | 李明飞,叶松青,杨言辰,张国宾,侯晓光,明添学,唐忠.黑龙江老柞山金矿床地质、地球化学特征及其成矿构造背景[J].世界地质,2014,33(3):543-555. |
| |
| 作者姓名： | 李明飞 叶松青 杨言辰 张国宾 侯晓光 明添学 唐忠 |
| |
| 作者单位： | 1. 吉林大学 地球科学学院，长春 130061; 2. 云南省地质调查院，昆明 650051 |
| |
| 摘 要： | 在对老柞山矿床地质特征系统研究的基础上,对与成矿有关的岩石开展了进一步的主、微量元素地球化学测试分析。结果显示与成矿有关的花岗岩具富Sr、低Ti的高钾钙碱性火山弧花岗岩的特征,闪长玢岩具偏铝质钙碱性岩系列特征。岩石样品均呈现出富集轻稀土元素和大离子亲石元素(LILEs)、相对亏损重稀土元素和Nb、Ta、Ti等高场强元素(HFES)的特征,显示了与岛弧或活动大陆边缘岩浆岩相似的属性。流体包裹体特征显示,成矿流体主要来自岩浆水,矿床具中低温(125.6℃~324.5℃)、中浅成(1.0~7.1 km)成矿的特点。与成矿有关岩浆岩显示幔源岩浆特征,可能是地幔交代作用部分熔融所形成的。结合区域上同时期的火成岩时空展布认为,老柞山金矿床成矿可能分别与晚古生代古亚洲洋板块北向俯冲作用和中生代太平洋板块俯冲作用密切相关。
|
| 关 键 词： | 老柞山金矿 地质特征 地球化学特征 成矿构造背景 佳木斯地块 |
Geological and geochemical characteristics of Laozuoshan gold deposit in Heilongjiang and its metallotectonic setting |
| |
| LI Ming-Fei,YIE Song-Qing,YANG Yan-Chen,ZHANG Guo-Bin,HOU Xiao-Guang,MING Tian-Xue,TANG Zhong.Geological and geochemical characteristics of Laozuoshan gold deposit in Heilongjiang and its metallotectonic setting[J].World Geology,2014,33(3):543-555. |
| |
| Authors: | LI Ming-Fei YIE Song-Qing YANG Yan-Chen ZHANG Guo-Bin HOU Xiao-Guang MING Tian-Xue TANG Zhong |
| |
| Institution: | 1. College of Earth Sciences，Jilin University，Changchun 130061，China; 2. Geological Survey Institute of Yunnan Province，Kunming 650051，China |
| |
| Abstract: | On the basis of systematical studies of Laozuoshan gold deposit，the geochemical analyses (inclu- ding major and trace elements) were further undertaken for the ore-related rocks． The results show that the ore- related granites are low Ti and high Sr in content，belonging to High-K calcalkaline volcanic arc granites，while the diorite porphyrite appears the feature of metaluminous calc- alkaline rock series． All the rock samples are character- ized by enrichment in light rare earth elements (LＲEEs) and large ion lithophile elements (LILEs)，and relative depletion in heavy rare earth elements (HＲEEs) and high field strength elements (HFSEs)，such as Nb，Ta and Ti，with affinities to the igneous rocks formed in island arc or active continental margin settings． The features of fluid inclusions indicate that the ore- forming fluid mainly came from magmatic water，and the deposit was characterized by formation in the low- medium depth (1.0－7.1 km) under low-medium temperature (125. 6℃－324. 5℃)． Notably，the ore- related magmatic rocks show the characteristics of mantle- derived magma，suggesting that they were likely produced by partial melting of mantle experienced in metasomatism． According to the distribution of the coeval igneous rocks in the area，it is proposed that the formation of Laozuoshan gold deposit may be closely related to the Late Paleozoic northward subduction of the Paleo- Asian oceanic plate and the Mesozoic westward subduction of the Pacific oceanic plate，respectively． |
| |
| Keywords: | Laozuoshan gold deposit geological characteristics geochemical characteristics metallotectonic settings Jiamusi massif |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《世界地质》浏览原始摘要信息 |
| 点击此处可从《世界地质》下载免费的PDF全文 |
