Mineralization age and sources of ore‐forming material of the Nanmushu Zn‐Pb deposit in the Micangshan Tectonic Belt at the northern margin of the Yangtze Craton, China: Constraints from Rb‐Sr dating and Sr‐Pb isotopes. Issue 3 (25th June 2020)

• Record Type: Journal Article
• Authors: Song, Zhijiao; Chen, Cuihua; Yang, Yulong; Zhang, Yan; Yin, Li; Li, Hongzhi
• Is Part Of: Resource geology. Volume 70:Issue 3(2020)
• Page Start: 273
• Page End: 295
• Publication Date: 2020-06-25
• Subjects: mineralization age -- mineralization material source -- Nanmushu Zn‐Pb deposit -- Rb‐Sr dating -- Sr‐Pb isotopes -- Yangtze Craton; Mining geology -- Periodicals; Mining geology -- Pacific Area -- Periodicals; Mining geology -- Asia -- Periodicals; Geochemistry -- Periodicals; Environmental geology -- Periodicals; 553
• DOI: 10.1111/rge.12235
• Languages: English
• ISSNs: 1344-1698

Abstract

Abstract: The Nanmushu Zn‐Pb deposit, hosted by the Neoproterozoic Dengying Formation dolostone, is located in the eastern part of the Micangshan tectonic belt at the northern margin of the Yangtze Craton, China. This study involves a systematic field investigation, detailed mineralogical study, and Rb‐Sr and Pb isotopic analyses of the deposit. The results of Rb‐Sr isotopic dating of coexisting sphalerite and galena yield an isochron age of 486.7 ± 3.1 Ma, indicating the deposit was formed during the Late Cambrian to Early Ordovician. This mineralization age is interpreted to be related to the timing of destruction of the paleo‐oil reservoir in the Micangshan tectonic belt. All initial 87 Sr/ 86 Sr ratios of sphalerite and galena (0.70955–0.71212) fall into the range of the Mesoproterozoic Huodiya Group basement rocks (0.70877–0.71997) and Dengying Formation sandstone (0.70927–0.71282), which are significantly higher than those of Cambrian Guojiaba Formation limestone (0.70750–0.70980), Cambrian Guojiaba Formation carbonaceous slate (0.70766–0.71012), and Neoproterozoic Dengying Formation dolostone (0.70835–0.70876). Such Sr isotope signatures suggest that the ore strontium was mainly derived from a mixed source, and both of the Huodiya Group basement rocks and Dengying Formation sandstone were involved in ore formation. Both sphalerite and galena are characterized by an upper‐crustal source of lead ( 206 Pb/ 204 Pb = 17.849–18.022, 207 Pb/ 204 Pb = 15.604–15.809, and 208 Pb/ 204 Pb = 37.735–38.402), and their Pb isotopes are higher than, but partly overlap with, those of the Huodiya Group basement rocks, but differ from those of the Guojiaba and Dengying Formations. This suggests that the lead also originated from a mixed source, and the Huodiya Group basement rocks played a significant role. The Sr and Pb isotopic results suggest that the Huodiya Group basement rocks were one of the most important sources of metallogenic material. The geological and geochemical characteristics show that the Nanmushu Zn‐Pb deposit is similar to typical Mississippi Valley type, and the fluid mixing may be a reasonable metallogenic mechanism for Nanmushu Zn‐Pb deposit. Abstract : The Pb‐Zn mineralization age was determined to 486.7 ± 3.1 Ma by Rb‐Sr isotopic dating. The Huodiya Group basement rock is the main source of ore‐forming material. The Zn‐Pb mineralization was related to the paleo‐oil reservoir destruction.