|Table of Contents|

Major Type of Hornfels-related Deposits and Application for Deep Prospecting(PDF)

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

Issue:
2011年第03期
Page:
221-229
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Major Type of Hornfels-related Deposits and Application for Deep Prospecting
Author(s):
WANG Deng-hong1; YING Li-juan1; TANG Ju-xing1; LIANG Ting2; WANG Dong-ming2; HEI Huan2
1. Key Laboratory of Metallogeny and Mineral Assessment of Ministry of Land and Resources, Institute ofMineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; 2. School of EarthSciences and Resources, Chang'an University, Xi'an 7
Keywords:
hornfels;  heat contact metamorphism;  metamorphic deposit;  nonmetallic deposit;  metallic deposit;  oil-gas reservoir;  deep prospecting
PACS:
P611.3;P618.2
DOI:
-
Abstract:
Hornfels, as one product of heat contact metamorphism with fine granular metacryst texture and massive structure, exists widely in the metamorphic nonmetallic deposits of graphite, wollastonite and andalusite, and various metal deposits and oil-gas reservoir. However, the research and investigation on hornfels are insufficient. Based on the literature review, combined with the geological prospecting practice in Nanling and Gangdese metallogenic belts, the general concept of hornfels related to mineralization was defined; the geological features of major types of hornfels-related deposits were summarized, i.e. W, Mo, Fe, Cu, U, Au, Pb-Zn, Sn, Ag and rare metal deposits, the metamorphic nonmetallic deposits of graphite, wollastonite and andalusite, and oil-gas reservoir; new advances of deep prospecting in mining districts with hornfels in recent years were presented, i.e. Taoxikeng W mine in Jiangxi, tin-polymetallic deposits in Dachang of Guangxi, Jiama Cu polymentallic mine in Tibet, and Laochang Ag-Pb-Zn mine, Yangla Cu mine and Xuejiping Cu mine in Yunnan; standards for metallogenic prediction of hornfels-related deposits were discussed. The results showed that the rock assemblage, humidity content, seal-open system, hornfels physicality and zonation, lithology of original rock and its spacial distribution should be considered during the deep prediction for blind rock body at the large scale of district and ore field; the space distribution and the specificity relationship between petrologic feature and ore minerals should be considered in the metallogenic assessment at the regional medium and small scales; the application of hornfels for blind rock body is promising and significant for deep prospecting. Study on the relationship between hornfels and mineralization should be strengthened, and the relationship between the hornfelization zone found in previous geological mapping and mineralization should be revaluated.

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