|Table of Contents|

Characteristics of Pyrite Typomorphic Elements in Baicao Mining Area of Panzhihua-Xichang Region, the Western Margin of Yangtze Plate, China and Their Indication(PDF)

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

Issue:
2021年第02期
Page:
262-275
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Characteristics of Pyrite Typomorphic Elements in Baicao Mining Area of Panzhihua-Xichang Region, the Western Margin of Yangtze Plate, China and Their Indication
Author(s):
ZHANG Gui-shan1; 2;  QIU Hong-xin1;  PENG Ren1;  MENG Qian-kun1;  WEN Han-jie1; 3;  LI Shi-lei4
(1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits of Ministry of Natural Resources, Xi'an 710054, Shaanxi, China; 3. State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, Guizhou, China; 4. Mining Corporation of Sichuan Province Tranvic Group, Chengdu 610059, Sichuan, China)
Keywords:
geochemistry;  pyrite;  electron microprobe;  typomorphic element;  magmatic liquated mineralization;  hydrothermal action;  metallization mechanism;  the western margin of Yangtze plate
PACS:
P571; P595
DOI:
10.19814/j.jese.2020.09002
Abstract:
Pyrite is an important metal sulfide mineral, which occurs in many kinds of deposits. Its typomorphic characteristics are of great significance to the genesis of deposit and the spatial distribution of ore bodies. Taking pyrite in Baicao mining area of Panzhihua-Xichang region, the western margin of Yangtze plate as the research object, the typomorphic element characteristics of pyrite in four kinds of ores, such as disseminated, dense massive, taxitic and net vein, were comparatively studied by analytical methods of mineralography and electron probe micro-analyzer(EPMA). The results show that the average contents of Fe and S in pyrite are 46.030% and 52.815%, respectively, which are between magmatic and hydrothermal origins; according to ore characteristics, pyrite is mainly of magmatic origin, and a small amount of hydrothermal process also participate in the formation of pyrite; compared the δFe-δS characteristics of pyrite in Baicao mining area with those in Jinchuan and other typical Cu-Ni sulfide deposits, it is proved that the sulfide minerals in Baicao mining area are typical magmatic liquation type; the ratio of Co/Ni is less than 5 due to the existence of V-Ti magnetite, which indicates the symbiotic relationship between V-Ti magnetite and sulfide; the ratio of S/Se is 812-10 466, which is less than that of magmatic endogenetic pyrite(15 000), indicating that pyrite is of magmatic endogenetic origin; the ratio of Se/Te increases with the decrease of temperature, indicating that the crystallization order of pyrite is disseminated ore→dense massive ore→taxitic ore→net vein ore; the primitive mantle-normalized major and trace elements spider diagram shows that pyrite in Baicao mining area has both magmatic and hydrothermal origins. Based on the above typomorphic element characteristics, it is considered that pyrite in Baicao mining area is mainly caused by magmatic liquated mineralization and contains a small amount of hydrothermal action.

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