|Table of Contents|

Typomorphic Characteristics of Magnetite from Songhu Iron Deposit in West Tianshan, China and Their Constrains on Ore-forming(PDF)

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

Issue:
2021年第01期
Page:
80-99
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Typomorphic Characteristics of Magnetite from Songhu Iron Deposit in West Tianshan, China and Their Constrains on Ore-forming
Author(s):
JING De-long1 WANG Bang-yao2* WANG Zhi-hua1 ZHAO Xiao-jian1 TENG Jia-xin1 JIANG Chang-yi2 YANG Zhen-xi3
(1. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits of Ministry of Natural Resources, Xi’an Center of Geological Survey, China Geological Survey, Xi’an 710054, Shaanxi, China; 2. School of Earth Science and Resources, Chang’an University, Xi’an 710054, Shaanxi, China; 3. The Fourth Institute of Geological and Mineral Exploration, Gansu Provincial Bureau of Geology and Mineral Resources, Jiuquan 735000, Gansu, China)
Keywords:
Key words: genesis of deposit iron deposit magnetite typomorphic characteristic trace element explosion temperature lattice parameter West Tianshan
PACS:
P575; P611.1
DOI:
10.19814/j.jese.2020.09006
Abstract:
Songhu iron deposit is located at the western segment of Awulale metallogenic belt, which lies on the the northwest edge of Yili plate in West Tianshan, Xinjiang. The wall rocks are mainly andesite and andesitic volcaniclastic rocks of Lower Carboniferous Dahalajunshan Formation. The origin of this deposit is still controversial, and the focus is whether there is magmatic magnetite. In view of the above, the typomorphic characteristics of magnetite were carried out for various typical ores in Songhu iron deposit to constrain its ore genesis, and the trace element compositions of magnetite were analyzed by in-situ LA-ICP-MS. The results show that magnetites in disseminated and massive ores are typically high in contents of V, Ni and Ti, and low in contents of Al, Mn, Co, Zn and Sn, indicating similar geochemical characteristics with igneous magnetites; whereas magnetites in banded and brecciated ores have relatively high contents of Mg, Al, Mn and Zn, and low contents of V, which are approximate to hydrothermal magnetites in skarn deposit. The explosion temperature of magnetite inclusion indicates that there are two phases of inclusions in disseminated and massive ores, and their forming temperatures are 328 ℃-397 ℃ and 424 ℃-485 ℃, respectively; the coarse-grained magnetites in banded and brecciated ores contain fewer inclusions that form at 343 ℃-385 ℃. Based on the typomorphic characteristics of magnetite, it is considered that the forming temperature of magnetites in disseminated ores is highest, that of magnetites in massive ores is higher, that of magnetites in brecciated ores is high, and that of magnetites in banded ores is low. This is also the forming order of these ores during the mineralization in Songhu iron deposit. Petrographical and trace element geochemical characteristics indicate that there are ore-magmas erupted during the early stage of mineralization in this deposit, and the hydrothermal magnetites are mainly formed by volcanic hydrothermal metasomatism rather than sedimentation. In conclusion, Songhu iron deposit genetically belongs to a volcanic magmatic-hydrothermal compound type.

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Last Update: 2021-03-10