黔西玄武岩铂族元素赋存状态及地质意义

• 基础地质·矿床·盆地 • 上一篇下一篇

黔西玄武岩铂族元素赋存状态及地质意义

来雅文¹，王林根²，肖国拾²，甘树才²，段国正¹

1.吉林大学地球探测科学与技术学院，吉林长春 130026；2.吉林大学化学学院，吉林长春 130026

收稿日期:2004-12-02 修回日期:1900-01-01 出版日期:2005-09-26 发布日期:2005-09-26
通讯作者: 来雅文

Study on the Occurrence States of the Platinum Group Elements in Basaltfrom Western Guizhou Province and Their Geological Significance

LAI Ya-wen¹,WANG Lin-gen², XIAO Guo-shi²,GAN Shu-cai², DUAN Guo-zheng¹

1.College of GeoExploration Science and Technology,Jilin University, Changchun 130026,China; 2.College of Chemistry,Jilin University,Changchun 130026,China

Received:2004-12-02 Revised:1900-01-01 Online:2005-09-26 Published:2005-09-26
Contact: LAI Ya-wen

摘要/Abstract

摘要： 在地球化学系统中，元素的亲合性是制约元素地球化学行为的基本属性，而赋存状态则反映元素质的属性。对黔西基性玄武岩原岩与流体包体中Pt、Pd的赋存状态进行研究，结果说明了利用元素亲合性对指导其赋存状态查定的重要性，同时表明了研究该地区玄武岩中同生流体包体中铂族元素对重演古流体中元素迁移与富集具有重要的理论与实际意义。

关键词: 地球化学亲合性, 玄武岩, 赋存状态, 流体包体

Abstract: In a geochemical system, the affinity of an element controls its geochemical behaviors while its occurrence state represents its nature. The abundance and occurrence state of an element shows its difference in affinity and could provide important information for the geochemistry system and for the behaviors of an element in the system. The occurrences states of Pt and Pd in the parental rocks and in the fluid inclusions of the Western Guizhou Province basalt are studied. The result of this study shows the importance of determing the occurrence state of an element using its affinity, revealing that the PGE can be used in studying the migration and enrichment of elements in syngenetic fluid of the basalts.

Key words: geochemical affinity, basalt, occurrence states, fluid inclusion

中图分类号:

P595

来雅文，王林根，肖国拾，甘树才，段国正. 黔西玄武岩铂族元素赋存状态及地质意义[J]. J4, 2005, 35(05): 607-610.

LAI Ya-wen,WANG Lin-gen, XIAO Guo-shi,GAN Shu-cai, DUAN Guo-zheng. Study on the Occurrence States of the Platinum Group Elements in Basaltfrom Western Guizhou Province and Their Geological Significance[J]. J4, 2005, 35(05): 607-610.

参考文献

相关文章 11

[1]	闫佰忠, 邱淑伟, 肖长来, 梁秀娟. 长白山玄武岩区地热异常区遥感识别[J]. 吉林大学学报(地球科学版), 2017, 47(6): 1819-1828.
[2]	曾令高, 张均, 孙腾, 李斌, 朱光辉, 贾子超, 方权, 陈庚户. 峨眉山大火成岩省烂纸厂铁矿床地质特征、成因及其找矿勘查启示[J]. 吉林大学学报(地球科学版), 2016, 46(2): 412-424.
[3]	曹晓峰, Mohamed Lamine Salifou Sanogo, 吕新彪, 何谋春, 陈超, 朱江, 唐然坤, 刘智, 张彬. 甘肃枣子沟金矿床成矿过程分析——来自矿床地质特征、金的赋存状态及稳定同位素证据[J]. J4, 2012, 42(4): 1039-1054.
[4]	曹锐, 木合塔尔·扎日, 陈斌, 李德威, 曹福根, 刘德民. 东天山板块缝合带石炭纪火山岩地球化学和Sr-Nd同位素特征及其大地构造意义[J]. J4, 2012, 42(2): 400-409.
[5]	严再飞, 黄智龙, 陈觅, 周家喜, 赵正, 丁伟. 峨眉山溢流玄武岩省高钛玄武岩的两种不同地幔源特征[J]. J4, 2010, 40(6): 1311-1322.
[6]	廖震文. 滇黔邻区与峨眉山玄武岩有关的铜矿、金矿地质特征对比[J]. J4, 2010, 40(4): 821-827.
[7]	于德利, 张培萍, 肖国拾, 张东丽. 大洋锰结核中钴的赋存状态及提取实验研究[J]. J4, 2009, 39(5): 824-827.
[8]	付长亮, 孙德有, 魏红艳, 苟军. 伊通新生代玄武岩地球化学成分差异性研究[J]. J4, 2009, 39(3): 446-454.
[9]	黎应书，秦德先，邹滔，贾福聚，万朝英，孙彩霞，周年胜. 云南个旧拉丁尼克期玄武岩地球化学特征及其大地构造背景[J]. J4, 2008, 38(4): 624-0630.
[10]	黎应书，秦德先，党玉涛，薛传东，谈树成，洪托. 云南个旧锡矿的玄武岩成矿[J]. J4, 2006, 36(03): 326-335.
[11]	匡永生,赵书跃,秦秀峰,马江水,刘旭光,李仰春, 张昱. 大兴安岭北段早石炭世洋岛型玄武岩的确立及成因意义[J]. J4, 2005, 35(04): 423-0429.

Metrics

Viewed

Full text

Abstract

Cited

Shared

Discussed