SHRIMP Zircon U-Pb Age of the Sidingheishan Mafic-Ultramafic Intrusion in the Southern Margin of the Central Asian Orogenic Belt,NW China and its Petrogenesis implication
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作者:
SUN Tao
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机构:
School of Resource Environment and Earth Sciences,Yunnan UniversitySchool of Resource Environment and Earth Sciences,Yunnan University
SUN Tao
[1
]
QIAN Zhuangzhi
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机构:
MOE Key Laboratory of Western China's Mineral Resources and Geological Engineering,College of Earth Science and Recourses,Chang'an UniversitySchool of Resource Environment and Earth Sciences,Yunnan University
QIAN Zhuangzhi
[2
]
XU Gang
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机构:
MOE Key Laboratory of Western China's Mineral Resources and Geological Engineering,College of Earth Science and Recourses,Chang'an UniversitySchool of Resource Environment and Earth Sciences,Yunnan University
XU Gang
[2
]
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机构:
DUAN Jun
[2
]
LI Wanting
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School of Resource Environment and Earth Sciences,Yunnan UniversitySchool of Resource Environment and Earth Sciences,Yunnan University
LI Wanting
[1
]
ZHANG Aiping
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机构:
School of Resource Environment and Earth Sciences,Yunnan UniversitySchool of Resource Environment and Earth Sciences,Yunnan University
ZHANG Aiping
[1
]
机构:
[1] School of Resource Environment and Earth Sciences,Yunnan University
[2] MOE Key Laboratory of Western China's Mineral Resources and Geological Engineering,College of Earth Science and Recourses,Chang'an University
Pb;
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SHRIMP Zircon U-Pb Age of the Sidingheishan Mafic-Ultramafic Intrusion in the Southern Margin of the Central Asian Orogenic Belt;
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D O I:
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中图分类号:
P588.12 [侵入岩、深成岩];
P597.3 [];
学科分类号:
070901 ;
070902 ;
摘要:
Objective The Sidingheishan mafic-ultramafic intrusion is located in the eastern part of the North Tianshan Mountains.This work used zircon U-Pb age data,bulk rock major and trace elements,Sr-Nd-Pb isotope data to assess mantle source characteristics and crustal assimilation of the parental magma of the Sidingheishan intrusion.We have also discussed the tectonic evolution of the southern margin of the Central Asian Orogenic belt in the Late Paleozoic.