| Citation: |
CHEN Li, LIU Han, HE Juan. LA-ICP-MS zircon U-Pb ages of the two phases of magmatism in the Xiuwacu W-Mo deposit, northwest Yunnan, and their implications for ore genesis[J]. Geological Bulletin of China, 2020, 39(6): 929-942.
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LA-ICP-MS zircon U-Pb ages of the two phases of magmatism in the Xiuwacu W-Mo deposit, northwest Yunnan, and their implications for ore genesis
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Abstract
Two phases of intrusive magmatism were developed in the Xiuwacu deposit, northwest Yunnan.This study focused on the geochronological and geochemical characteristics of these intrusive rocks so as to define the petrogenesis of the Xiuwacu deposit.The LA-ICP-MS zircon U-Pb dating results show that biotite granite from the east of Xiuwacu deposit was formed at 214.9±1.3 Ma, granite porphyry and monzogranite from the west of Xiuwacu deposit was formed at 87.47±0.51 Ma and 83.29±0.60 Ma.The results of the studies show that the molybdenite from the Xiuwacu deposit was formed at 82~86 Ma, corresponding to Late Yanshanian.The two phases of intrusions have similar geochemical characteristics, both belonging to the shoshonitic type and metaluminous to slight peraluminous series, with enrichment of LILE(Rb, Th, U)and depletion of HFSE(Nb, Sr, Zr, Hf).The Y-Nb and Yb-Ta discrimination diagrams indicate that the two phases of intrusions were formed in different tectonic environments.The Late Triassic intrusive rocks fall into the field of syn-collision granites while the Late Cretaceous intrusive rocks fall into the field of intra-plate granites.Based on comprehensive study with regional geology and acquired achievements in fluid inclusions, S and Pb isotopes as well as zircon Hf isotopes, the authors infer that the partial melting of thickened lower crust in the Late Cretaceous seems to have been the main metallogenic material source of the Xiuwacu deposit.The ore-bearing thermal fluid migrated along the fault-crack system in the Xiuwacu deposit, and then the W-Mo orebodies were formed at the favorable position along with the combined effect of both temperature decreasing and the mixing with meteoric water.
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Keywords:
- zircon U-Pb age /
- Late Cretaceous /
- Xiuwacu /
- W-Mo deposit
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References
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CHEN Li, LIU Han, HE Juan. LA-ICP-MS zircon U-Pb ages of the two phases of magmatism in the Xiuwacu W-Mo deposit, northwest Yunnan, and their implications for ore genesis[J]. Geological Bulletin of China, 2020, 39(6): 929-942.
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Figure 1.
Simplified geological maps of the Yidun Arc(a)and Shangri-La region(b)
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Figure 2.
Simplified geological map(a)and geological section(b)of the Xiuwacu W-Mo deposit
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Figure 3.
Zircon CL images of biotite granite, granite porphyry and monzonitic granite in the Xiuwacu deposit
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Figure 4.
Zircons U-Pb concordia diagrams for biotite granite(a), granite porphyry(b)and monzonitic granite(c)in the Xiuwacu deposit
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Figure 5.
TAS(a), SiO2 versus K2O(b), NaO2 versus K2O(c)and A/CNK versus A/NK plots(d) of the Xiuwacu deposit
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Figure 6.
Chondrite-normalized REE patterns(a)and primitive mantle-normalized trace element diagram(b) of the Xiuwacu deposit
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Figure 7.
Diagrams of Y-Nb(a)and Yb-Ta(b)in the Xiuwacu W-Mo deposit
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Figure 8.
Homogenization temperatures and salinities of fluid inclusions from the Xiuwacu deposit