Petrogenesis of Dahongliutan Biotite Monzogranite in Western Kunlun Orogen: Evidence from Zircon U-Pb Age and Li-Hf Isotope

DING Kun; LIANG Ting; Zhou Yi; FENG Yonggang; ZHANG Ze; DING Liang; LI Kan

doi:10.19751/j.cnki.61-1149/p.2020.01.003

Northwestern Geology > 2020 > 53(1): 24-34. > DOI: 10.19751/j.cnki.61-1149/p.2020.01.003

DING Kun, LIANG Ting, Zhou Yi, et al. Petrogenesis of Dahongliutan Biotite Monzogranite in Western Kunlun Orogen: Evidence from Zircon U-Pb Age and Li-Hf Isotope[J]. Northwestern Geology, 2020, 53(1): 24-34. DOI: 10.19751/j.cnki.61-1149/p.2020.01.003

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Petrogenesis of Dahongliutan Biotite Monzogranite in Western Kunlun Orogen: Evidence from Zircon U-Pb Age and Li-Hf Isotope

1. School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, Shaanxi, China;
2. The Laboratory of Mineralization and Dynamics, Chang'an University, Xi'an 710054, Shaanxi, China;
3. Xi'an Center of China Geological Survey/Northwest China Center for Geoscience Innovation, Xi'an 710054, Shaanxi, China

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Received Date: August 13, 2019
Revised Date: November 17, 2019
Available Online: July 28, 2022
Published Date: March 04, 2020

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Abstract

Abstract

The Dahongliutan pluton is located in the eastern part of the West Kunlun Orogenic Belt and is mainly consisted of biotite monzonitic granite, monzonitic granite and two mica granite. The Zircon LA-ICP-MS U-Pb dating of biotite monzonitic granite in the southeastern part of Dahongliutan intrusion shows that the emplacement age of biotite monzonitic granite is 214+1.8 Ma, indicating that the Dahongliutan pluton was formed in the Late Indosinian. The Dahongliutan pluton has higher value of δ7Li(0.76‰~3.25‰) and lower content of lithium(5.04~52.22)×10^-6. The biotite monzonitic granite has zircon εHf(t) values of -1.86 to 2.16, and the two-stage mode age ranged between 1113 and 1368 Ma. In the εHf(t) vs. age diagram,all the data points lie near the chondrite evolution line. The comprehensive research shows that the Dahongliutan pluton has derived from a mixed magma of mesoproterozoic crust and mantle.
- zircon U-Pb age,
- Li-Hf isotope composition,
- rock genesis,
- Dahongliutan pluton,
- West Kunlun orogen

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Petrogenesis of Dahongliutan Biotite Monzogranite in Western Kunlun Orogen: Evidence from Zircon U-Pb Age and Li-Hf Isotope

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