黔西玄武岩铂族元素赋存状态及地质意义

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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

Abstract

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

CLC Number:

P595

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.

References

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