Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (5): 1365-1383.doi: 10.13278/j.cnki.jjuese.201505110

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Space-Time Distribution,Source Bed and Stratabound Mechanisms of Zn-Pb Deposits in Western Margin of Yangtze Platform

Chen Da   

  1. Institute of Geology and Mineral Resource Exploration, Non-Ferrous Metals and Nuclear Industry Geological Exploration Bureau of Guizhou(GNNG), Guiyang 550005, China
  • Received:2014-12-09 Published:2015-09-26

Abstract:

In order to find the metallogenic pattern of the Zn-Pb deposits at the junction of Sichuan, Yunnan, and Guizhou provinces, comprehend the metallogenic theory and predict ore prospecting, the author studied the space-time distribution of these Zn-Pb deposits in this area. The conclusions are listed as follows: 1)Zn-Pb deposits are distributed together, and can be divided into three ore-concentration areas. 2)Statistically, Sinian and Carboniferous stratum have a higher metallogenic probability of 51.57%, and Dengying and Baizuo Formation hold 80.98% metal reserve. 3)Tectonic units control the distribution of ore-forming units, but ore-concentration area does not correspond to the second tectonic unit at all. Ore-concentration area Ⅰ and Ⅱ are jointly controlled by Kangdian axis, Longmenshan depression, and cross region of Yangtze platform. 4)The space coupling between siderite (hematite) deposits,lead-zinc deposits, and close association of Pb-Zn minerals with siderite (hematite) indicate the genetic relationship between Zn-Pb deposits and Fe deposits. During the early stage of basin evolution, at the depression belt (or sea basin) in the edge of the ancient land mass, two types of iron formations were formed from Llandovery Telychian stratum of Silurian to Dewuan stratum of the Lower Carboniferous and the Lower Kunyang Group (Huili Group) in the middle of Proterozoic. Ore-forming elements, such as Pb and Zn, are pre-concentrated and further enriched by the later circulated hydrothermal fluids during diagenesis to form the deposit. Iron-formations provided the main ore-forming materials for Pb-Zn deposits. 5)The sulfur source, gypsum beds, is derived from the underlain Cambrian stratum of Dengying and Baizuo Formations. 6)Both ore-forming elements and sulfur source beds control the formation of ore concentration areas and the strata bound distribution of orebodies, which are considered to be the most important controlling factors.

Key words: Yangtze platform, Zn-Pb deposits, source bed, iron formation, ore-concentration area

CLC Number: 

  • P618.4

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