福建漳平洛阳铁矿床成岩成矿年代学及其地质意义

张达; 吴淦国; 狄永军; 王长明; 姚继明; 张垚垚; 吕良冀; 袁远; 石建基

doi:10.3799/dqkx.2012.130

Volume 37 Issue 6

Jun. 2012

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Article Navigation > Earth Science > 2012 > 37(6): 1217-1231

ZHANG Da, WU Gan-guo, DI Yong-jun, WANG Chang-ming, YAO Ji-ming, ZHANG Yao-yao, LV Liang-ji, YUAN Yuan, SHI Jian-ji, 2012. Geochronology of Diagenesis and Mineralization of the Luoyang Iron Deposit in Zhangping City, Fujian Province and Its Geological Significance. Earth Science, 37(6): 1217-1231. doi: 10.3799/dqkx.2012.130

Citation:

ZHANG Da, WU Gan-guo, DI Yong-jun, WANG Chang-ming, YAO Ji-ming, ZHANG Yao-yao, LV Liang-ji, YUAN Yuan, SHI Jian-ji, 2012. Geochronology of Diagenesis and Mineralization of the Luoyang Iron Deposit in Zhangping City, Fujian Province and Its Geological Significance. Earth Science, 37(6): 1217-1231. doi: 10.3799/dqkx.2012.130

Citation:

ZHANG Da, WU Gan-guo, DI Yong-jun, WANG Chang-ming, YAO Ji-ming, ZHANG Yao-yao, LV Liang-ji, YUAN Yuan, SHI Jian-ji, 2012. Geochronology of Diagenesis and Mineralization of the Luoyang Iron Deposit in Zhangping City, Fujian Province and Its Geological Significance. Earth Science, 37(6): 1217-1231. doi: 10.3799/dqkx.2012.130

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Geochronology of Diagenesis and Mineralization of the Luoyang Iron Deposit in Zhangping City, Fujian Province and Its Geological Significance

doi: 10.3799/dqkx.2012.130

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
2.
Key Laboratory of Lithospheric Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China
3.
Bureau of Geology and Mineral Resources of Fujian Province, Fuzhou 350003, China

Received Date: 2012-07-19
Available Online: 2021-11-09
Publish Date: 2012-06-15

Abstract

Abstract

In order to determine the main mineralization time and ore forming genesis in the southwestern Fujian Province, this paper selects the Luoyang iron deposit to develop the study of LA-ICP-MS zircon U-Pb isotopic dating for granite and Re-Os geochronology for molybdenite from the iron ore body. According to the results, the molybdenite Re-Os isotopic model date is (133.0±1.9) to (134.0±4.2) Ma, which belongs to Early Cretaceous; and LA-ICP-MS zircon U-Pb isotopic dates for the granite porphyry and fine grain porphyritic granite are (131±1) Ma and (131.64 ±0.62) Ma respectively, which is very close to the mineralization time achieved by the Re-Os isotopic dating. According to the analysis of the granites, spatial distribution of magnetite and molybdenite ore bodies, and the mineralization and alteration characteristics, combining with the above granite and deposit chronological data, it is suggested that the Luoyang iron deposit mainly formed at Early Cretaceous when the contact thermofluid metasomatism occurred between the Early Cretaceous granites and the Carboniferous clastic and carbonate strata.
- Re-Os isotopic age,
- LA-ICP-MS zircon U-Pb isotopic dating,
- molybdenite,
- Luoyang iron deposit,
- petrology,
- ore prospecting,
- ore deposits

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References(47)

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Geochronology of Diagenesis and Mineralization of the Luoyang Iron Deposit in Zhangping City, Fujian Province and Its Geological Significance

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