Wechat
J4 ›› 2011, Vol. 19 ›› Issue (2): 47-51.
• article • Previous Articles Next Articles
LIU Wenhua1,ZHANG Dianlong1,YANG Jinsheng1,ZHANG Tao2
Received:
Revised:
Online:
Published:
Abstract:
Starting from morphology,composition,structure and properties,we can research the typomorphic characteristics of pyrite,it is great significance for theory research and evaluation of gold deposit genesis.According to system research of pyrite occurrence,morphological characteristics,chemical composition,lattice parameter,thermo -electric coefficient,we find the relationship between pyrite genesis and gold mineralization.With the evolution of ore-forming stage,N-type pyrite shows increase trending,but P-N type shows decline trending correspondingly,also the research shows that the peak value of N-type pyrite thermoelectric coefficient (-369~-400 μv/℃)can be used as the typomorphic characteristics of gold prospecting of Bushang gold mine.In addition,the value of a0 in pyrite is smaller at the main ore-forming stage,and the share of P-type pyrite is lower,mainly to N-type,it can be used to guide gold prospecting of the area.
Key words: Pyrite, Genetic mineralogy, Thermoelectric coefficient, Typomorphic characteristics, Bushang gold mine, Shandong Province
CLC Number:
LIU Wenhua,ZHANG Dianlong,YANG Jinsheng,ZHANG Tao. Study on Genetic Minerageny of Pyrite in Bushang Gold Mine,Shandong Province[J].J4, 2011, 19(2): 47-51.
0 / / Recommend
Add to citation manager EndNote|Reference Manager|ProCite|BibTeX|RefWorks
URL: http://www.goldsci.ac.cn/EN/
http://www.goldsci.ac.cn/EN/Y2011/V19/I2/47
[1]山东省地矿局第六地质勘查院.山东省招远县埠上金矿区详细普查地质报告[R].招远:山东省地矿局第六地质勘查院,1986. [2]任英忱.山东招远掖县地区金矿床的矿物分带[J].地质找矿论丛,1988,3(3):18- 22. [3]陈光远,邵伟,孙岱生.胶东金矿成因矿物学与找矿[M].重庆:重庆出版社,1989:22- 28. [4]李兆龙,许文斗.胶东地区金矿稳定同位素地球化学特征及金矿成因[M].辽宁:东北大学出版社,1989. [5]姚凤良,刘连登.招掖金矿带的稳定同位素地质及金矿床成因[J].长春地质学院学报,1990,8(4):53- 58. [6]王炳成.玲珑花岗岩的岩石化学与地球化学特征[J].山东国土资源,1986,2(1):8- 12. [7]陈振胜.胶东区域岩石铅同位素地球化学背景研究[J].地质找矿论丛,1994,9(1):14- 19.
Cited