东昆仑与成矿有关的三叠纪花岗岩演化：基于莫河下拉岩体岩石学、地球化学和锆石U-Pb年代学的证据

张炜; 周汉文; 朱云海; 毛武林; 佟鑫; 马占青; 曹永亮

doi:10.3799/dqkx.2016.520

Volume 41 Issue 8

Aug. 2016

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Article Navigation > Earth Science > 2016 > 41(8): 1334-1348

Zhang Wei, Zhou Hanwen, Zhu Yunhai, Mao Wulin, Tong Xin, Ma Zhanqing, Cao Yongliang, 2016. The Evolution of Triassic Granites Associated with Mineralization within East Kunlun Orogenic Belt: Evidence from the Petrology, Geochemistry and Zircon U-Pb Geochronology of the Mohexiala Pluton. Earth Science, 41(8): 1334-1348. doi: 10.3799/dqkx.2016.520

Citation:

Zhang Wei, Zhou Hanwen, Zhu Yunhai, Mao Wulin, Tong Xin, Ma Zhanqing, Cao Yongliang, 2016. The Evolution of Triassic Granites Associated with Mineralization within East Kunlun Orogenic Belt: Evidence from the Petrology, Geochemistry and Zircon U-Pb Geochronology of the Mohexiala Pluton. Earth Science, 41(8): 1334-1348. doi: 10.3799/dqkx.2016.520

Citation:

Zhang Wei, Zhou Hanwen, Zhu Yunhai, Mao Wulin, Tong Xin, Ma Zhanqing, Cao Yongliang, 2016. The Evolution of Triassic Granites Associated with Mineralization within East Kunlun Orogenic Belt: Evidence from the Petrology, Geochemistry and Zircon U-Pb Geochronology of the Mohexiala Pluton. Earth Science, 41(8): 1334-1348. doi: 10.3799/dqkx.2016.520

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The Evolution of Triassic Granites Associated with Mineralization within East Kunlun Orogenic Belt: Evidence from the Petrology, Geochemistry and Zircon U-Pb Geochronology of the Mohexiala Pluton

doi: 10.3799/dqkx.2016.520

Zhang Wei^{1,2
,},
Zhou Hanwen^{1,3
,
,},
Zhu Yunhai¹,
Mao Wulin¹,
Tong Xin¹,
Ma Zhanqing⁴,
Cao Yongliang⁴

1.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Nanjing Center of China Geological Survey, Nanjing 210016, China
3.
Three Gorges Research Center for Geo-Hazards of Ministry of Education, China University of Geosciences, Wuhan 430074, China
4.
Qaidam Synthetical Exploration Institute of Geology and Mineral Resources, Golmud 816000, China

Received Date: 2016-03-08
Publish Date: 2016-08-15

Abstract

Abstract

The East Kunlun orogenic belt is not only an important intrusive magmatic tectonic belt, but also a very important poly-metallic metallogenic belt for national economy. There are a large number of granites associated with mineralization formed in Triassic in this area, but the connection between them and the relationship about the tectogenesis are still not clear. In this paper, detailed petrography, element geochemical and zircon geochronological studies are presented for the Mohexiala granite-porphyry associated with silver poly-metallic ore; we summarize the characteristics of Triassic granites associated with mineralization within the East Kunlun orogenic belt, and discuss their evolution. Results show that: (1) the Triassic granites associated with mineralization within East Kunlun orogenic belt have a clear trend from low-K and mid-K calc-alkaline series to high-K calc-alkaline and shoshonite series during 250-200 Ma, their A/NK ratios decreased from 2.0 to 1.0 during 240-200 Ma; (2) the (⁸⁷Sr/⁸⁶Sr)_i ratios between 0.710 to 0.715, ε_Nd(t)=-0.6-0.0, the value of ε_Hf(t) are concentrated in -5-1 and the peak ranges between -2 to -1, indicating that the East Kunlun Triassic granites associated with mineralization were derived from the sources of ancient crust and mixed by mantle material; (3) the East Kunlun area got into the post-orogenic stage at 240 Ma and a large number of calc-alkaline granites formed, the granites gradually reduced after 220 Ma and some alkaline A-type granites occurred between 204 Ma and 210 Ma which indicates that the orogenic belt transformed from collision-orogeny to the intraplate break-up stage.
- Triassic granites,
- geochemistry,
- petrology,
- post-collisional,
- Mohexiala,
- East Kunlun orogenic belt

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References(91)

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The Evolution of Triassic Granites Associated with Mineralization within East Kunlun Orogenic Belt: Evidence from the Petrology, Geochemistry and Zircon U-Pb Geochronology of the Mohexiala Pluton

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