|Table of Contents|

Ore Sources and Organic Mineralization in the Jinding Lead-Zinc Deposit, Yunnan Province(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2009年第04期
Page:
376-382
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Ore Sources and Organic Mineralization in the Jinding Lead-Zinc Deposit, Yunnan Province
Author(s):
WANG Xin-li1; 2;  YANG Shu-sheng1;  PANG Yan-chun2;  FU Xiu-gen3;  LI De-liang2
(1.Xinda Gold and Silver Development Center, Beijing 100038, China; 2.Institute of Sedimentary Geology,Chengdu University of Technology, Chengdu 610059, Sichuan, China; 3.Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, Sichuan, China)
Keywords:
organic mineralization;  Jinding Lead-Zinc deposit;  Ore source;  Biomarker;  Yunnan
PACS:
P618.42
DOI:
-
Abstract:
This paper focuses on discussing the origin of ore-forming substances and organic mineralization through analyzing the isotope and biomarker compounds of Jinding Lead-zinc Deposit. The result shows that most of lead metal in the ore originated form upper mantle and the ore-forming fluids mainly derived from mantle fluids and basin saline. The matrix of organic substances mainly derived from low-grade water-sourced alga, while associated with a certain mount of high-grade continent-sourced botanic components. Organic substance derived from carbonate rocks in Triassic Sanhedong Formation. The roles organic substance possibly playing among the forming process of Jinding lead zinc deposit are: deoxidized the sulfate to produce the sulfur which needed in ore-forming process; formed organic complex and metallic complex; activated and transited ore-forming metallic elements; changed the physical-chemical environment of ore-formation; deoxidized and deposited ore-forming materials.

References:

[1] Giordano T H,Barnes H L.Lead-Zinc Transport in Mississippi Valley-type Ore Solutions[J].Economic Geology,1981,76:2200-2211.
[2] Manning D A,Gize A P.Organic Gechemistry:Principles and Application[M].New York:Plenum Press,1993.
[3] Dianar J R,Sureau J F.Organic Matter in Ore Genesis:Process and Perspectives[J].Organic Geochemistry,1990,16:577-599.
[4] Dianar J R.A Comparison of Mineralization Histories for Two MTV Deposits,Treves and Malines(Causses Basin,France),Based on the Geochemistry ofAssociated Organic Matter[J].Ore Geology Reviews,1996,11:133-156.
[5] 张志坚,张文淮.有机成矿流体研究进展[J].地质科技情报,1998,17(2):45-50.
[6] Xue C J,Liu S W,Chen Y C,et a1. Giant Mineral Deposits and Their Geodynamics Setting in the Lanping Basin,Yunnan,China[J].Acta Geologica Sinica,2004,78(2):368-374.
[7] 薛春纪,陈毓川,杨健民,等.金顶铅锌矿床地质-地球化学[J].矿床地质, 2002,21(3):270-277.
[8] 覃功炯,朱上庆.金顶铅锌矿床成因模式及找矿预测[J].云南地质,1991,10(2):145-190.
[9] 胡明安.有机质的热液成熟作用在云南金顶铅锌矿床形成过程中的意义[J].地球科学——中国地质大学学报,1989,14(5):503-512.
[10] 薛春纪,陈毓川,杨健民,等.滇西北兰坪铅锌银铜矿田含烃富CO2成矿流体及其地质意义[J].地质学报,2002,76(2):244-253.
[11] 薛春纪,高永宝,曾 荣,等.滇西北兰坪盆地金顶超大型矿床有机岩相学和地球化学[J].岩石学报,2007,23(11):2889-2900.
[12] 常向春,张金亮.金顶铅锌矿区中原油地球化学特征及其意义[J].特种油气藏,2003,10(5):15-19.
[13] 付修根,林 丽,庞艳春,等.金顶铅锌矿床中碳沥青的分布特征及成矿作用[J].吉林大学学报:地球科学版,2005,35(5):581-586.
[14] 付修根,林 丽,庞艳春,等.云南金顶铅锌矿床中的有机质特征及成矿作用探讨[J].成都理工大学学报:自然科学版,2006,33(6):621-630.
[15] 刘显凡,陶 专,卢秋霞,等.云南金顶超大型铅锌矿床地幔流体成矿作用探讨[J].矿床地质,2006,25(增刊):79-82.
[16] 云南地质矿产局第三地质大队.云南省兰坪县金顶铅锌矿床勘探地质报告[R].昆明:云南省地质矿产局,1984.
[17] 陶晓风,朱利东,刘登忠,等.滇西兰坪盆地的形成及演化[J].成都理工学院学报,2002,29(5):521-525.
[18] 高建华.滇西金顶铅锌矿床和蒸发岩建造成因关系的初步探讨[J].地球科学——中国地质大学学报,1989,14(5):513-522.
[19] 曾 荣,薛春纪,刘淑文,等.金顶超大型铅锌矿床成矿条件分析[J].地球科学与环境学报,2005,27(2):21-25.
[20] 薛春纪,陈毓川,杨健民,等.滇西兰坪盆地构造体制和成矿背景分析[J].矿床地质, 2002,21(1):36-44.
[21] 温春齐.矿床学研究方法[R].成都:成都理工大学,2003.
[22] 朱上庆,黄华盛.层控矿床地质学[M].北京:冶金工业出版社,1988.
[23] 张 乾.云南金顶超大型铅锌矿床的铅同位素组成及铅来源探讨[J].地质与勘探,1993,29(5):21-28.
[24] 叶庆同,胡云中,杨岳清,等.三江地区区域地球化学背景和金银铅锌成矿作用[M].北京:地质出版社,1992.
[25] Zartman R E,Doe B R.Plumbotectonics:the Model[J].Tectonophysics,1981,75:135-162.
[26] 王彦斌,曾普胜,李延河,等.云南金顶和白秧坪矿床He、Ar同位素组成及其意义[J].矿物岩石,2004,24(4):76-80.
[27] 温春齐,蔡建明,刘文周,等. 金顶铅锌矿床流体包裹体地球化学特征[J].矿物岩石,1995,15(4):78-84.
[28] 薛春纪,陈毓川,王登红,等.滇西北金顶和白秧坪矿床:地质和He,Ne,Xe同位素组成及成矿时代[J].中国科学D辑:地球科学,2003,33(4):315-322.
[29] Moldowan J M, Sundaraman P,Schoell M.Sensitivity of Biomarker Properties to Depositional Enviroment and/or Source Input in the Lower Toarcian of Southwest-Germany[J].Organic Geochemistry,1986,10:915-926.
[30] 苏晶文,胡 凯,李 贶.粤北凡口超大型铅锌矿有机质成矿地球化学特征[J].高校地质学报,2005,11(1):58-66.
[31] 曾宪章,梁狄刚,王忠然,等.中国陆相原油和生油岩中的生物标志物[M].兰州:甘肃科学技术出版社,1989.
[32] 王启军,陈建渝.油气地球化学[M].北京:中国地质大学出版社,1988.
[33] 刘建明,刘家军,顾雪祥.沉积盆地中的流体活动及其成矿作用[J].岩石矿物学杂志,1997,16(4):341-352.
[34] Macgroman D,Surdam R C.Difunctional Carboxylic and Acid Anions in Oilfield Waters[J].Organic Geochemistry,1988,12:245-259.
[35] 傅家谟,刘德汉,卢家烂.有机质演化对金属元素离散和富集的控制作用[R].广州:中国科学院有机地球化学开放实验室,1986.
[36] 张志坚,张文淮.滇黔桂地区低温矿床有机成矿流体与矿化的关系[J].矿物学报,1997,17(4):483-490.
[37] 谢树成,殷鸿福.南京栖霞山铅锌银多金属矿床的生物成矿作用[J].高校地质学报,1997,3(2):192-201.
[38] 张文淮,张志坚,伍 刚.成矿流体种类和成矿机理[J].地学前缘,1996,3(4):245-252.
[39] 谢 徽.北大巴山大型毒重石矿床的有机地球化学特征及形成环境[D].北京:中国地质大学,2006.

Memo

Memo:
-
Last Update: 2009-12-20