Baiganhu quartz vein type gold deposit concerned with hypabyssal(新疆白干湖与浅成斑岩有关的石英脉型金矿床)
白干湖金矿床是近年来西安工程学院发现的重要金矿床之一.该矿床属与浅成斑岩有关的石英脉型金矿床.含金石英脉体产出于石英斑岩与灰岩的接触带,成矿物质主要来自石英斑岩围岩;流体萃取周围介质中的成矿元素,集中于接触带中,金富集沉淀成矿.矿床形成分热液成矿期和表生氧化期,其中热液成矿期又分黄铁矿-毒砂-石英阶段、金-黝铜矿-方铅矿-闪锌矿-石英阶段、石英-碳酸盐阶段....
| Main Authors: | , , |
|---|---|
| Format: | Article |
| Language: | zho |
| Published: |
Zhejiang University Press
2002-03-01
|
| Series: | Zhejiang Daxue xuebao. Lixue ban |
| Subjects: | |
| Online Access: | https://doi.org/zjup/1008-9497.2002.29.2.209-212 |
| _version_ | 1797236515196108800 |
|---|---|
| author | QUWen-jun(屈文军) LANXiang(兰翔) HANZhao-xin(韩照信) |
| author_facet | QUWen-jun(屈文军) LANXiang(兰翔) HANZhao-xin(韩照信) |
| author_sort | QUWen-jun(屈文军) |
| collection | DOAJ |
| description | 白干湖金矿床是近年来西安工程学院发现的重要金矿床之一.该矿床属与浅成斑岩有关的石英脉型金矿床.含金石英脉体产出于石英斑岩与灰岩的接触带,成矿物质主要来自石英斑岩围岩;流体萃取周围介质中的成矿元素,集中于接触带中,金富集沉淀成矿.矿床形成分热液成矿期和表生氧化期,其中热液成矿期又分黄铁矿-毒砂-石英阶段、金-黝铜矿-方铅矿-闪锌矿-石英阶段、石英-碳酸盐阶段. |
| first_indexed | 2024-04-24T17:05:05Z |
| format | Article |
| id | doaj.art-c21efa211e1b4aa0b1731e9c3d9501cb |
| institution | Directory Open Access Journal |
| issn | 1008-9497 |
| language | zho |
| last_indexed | 2024-04-24T17:05:05Z |
| publishDate | 2002-03-01 |
| publisher | Zhejiang University Press |
| record_format | Article |
| series | Zhejiang Daxue xuebao. Lixue ban |
| spelling | doaj.art-c21efa211e1b4aa0b1731e9c3d9501cb2024-03-29T01:58:18ZzhoZhejiang University PressZhejiang Daxue xuebao. Lixue ban1008-94972002-03-01292209212zjup/1008-9497.2002.29.2.209-212Baiganhu quartz vein type gold deposit concerned with hypabyssal(新疆白干湖与浅成斑岩有关的石英脉型金矿床)QUWen-jun(屈文军)0LANXiang(兰翔)1HANZhao-xin(韩照信)2 1.Department of Geoscience, Yanta Campus, Chang'an U niversity, Xi'an 710054, China( 1.长安大学雁塔校区地球科学系，陕西 西安 710054) 2.Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China( 2.浙江大学地球科学系，浙江 杭州 310027) 1.Department of Geoscience, Yanta Campus, Chang'an U niversity, Xi'an 710054, China( 1.长安大学雁塔校区地球科学系，陕西 西安 710054)白干湖金矿床是近年来西安工程学院发现的重要金矿床之一.该矿床属与浅成斑岩有关的石英脉型金矿床.含金石英脉体产出于石英斑岩与灰岩的接触带,成矿物质主要来自石英斑岩围岩;流体萃取周围介质中的成矿元素,集中于接触带中,金富集沉淀成矿.矿床形成分热液成矿期和表生氧化期,其中热液成矿期又分黄铁矿-毒砂-石英阶段、金-黝铜矿-方铅矿-闪锌矿-石英阶段、石英-碳酸盐阶段.https://doi.org/zjup/1008-9497.2002.29.2.209-212白干湖金矿矿床成因浅成斑岩 |
| spellingShingle | QUWen-jun(屈文军) LANXiang(兰翔) HANZhao-xin(韩照信) Baiganhu quartz vein type gold deposit concerned with hypabyssal(新疆白干湖与浅成斑岩有关的石英脉型金矿床) Zhejiang Daxue xuebao. Lixue ban 白干湖金矿 矿床成因 浅成斑岩 |
| title | Baiganhu quartz vein type gold deposit concerned with hypabyssal(新疆白干湖与浅成斑岩有关的石英脉型金矿床) |
| title_full | Baiganhu quartz vein type gold deposit concerned with hypabyssal(新疆白干湖与浅成斑岩有关的石英脉型金矿床) |
| title_fullStr | Baiganhu quartz vein type gold deposit concerned with hypabyssal(新疆白干湖与浅成斑岩有关的石英脉型金矿床) |
| title_full_unstemmed | Baiganhu quartz vein type gold deposit concerned with hypabyssal(新疆白干湖与浅成斑岩有关的石英脉型金矿床) |
| title_short | Baiganhu quartz vein type gold deposit concerned with hypabyssal(新疆白干湖与浅成斑岩有关的石英脉型金矿床) |
| title_sort | baiganhu quartz vein type gold deposit concerned with hypabyssal 新疆白干湖与浅成斑岩有关的石英脉型金矿床 |
| topic | 白干湖金矿 矿床成因 浅成斑岩 |
| url | https://doi.org/zjup/1008-9497.2002.29.2.209-212 |
| work_keys_str_mv | AT quwenjunqūwénjūn baiganhuquartzveintypegolddepositconcernedwithhypabyssalxīnjiāngbáigànhúyǔqiǎnchéngbānyányǒuguāndeshíyīngmàixíngjīnkuàngchuáng AT lanxianglánxiáng baiganhuquartzveintypegolddepositconcernedwithhypabyssalxīnjiāngbáigànhúyǔqiǎnchéngbānyányǒuguāndeshíyīngmàixíngjīnkuàngchuáng AT hanzhaoxinhánzhàoxìn baiganhuquartzveintypegolddepositconcernedwithhypabyssalxīnjiāngbáigànhúyǔqiǎnchéngbānyányǒuguāndeshíyīngmàixíngjīnkuàngchuáng |