吉东大栗子铁矿区石英二长斑岩U-Pb年龄、地球化学及Hf同位素组成

叶丽娜; 孙丰月; 王力; 刘金龙; 张宇婷

doi:10.3799/dqkx.2019.173

Volume 45 Issue 5

May 2020

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Article Navigation > Earth Science > 2020 > 45(5): 1544-1555

Ye Lina, Sun Fengyue, Wang Li, Liu Jinlong, Zhang Yuting, 2020. Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Composition of the Quartz Monzonite Porphyry Intrusion from East Jilin Province. Earth Science, 45(5): 1544-1555. doi: 10.3799/dqkx.2019.173

Citation:

Ye Lina, Sun Fengyue, Wang Li, Liu Jinlong, Zhang Yuting, 2020. Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Composition of the Quartz Monzonite Porphyry Intrusion from East Jilin Province. Earth Science, 45(5): 1544-1555. doi: 10.3799/dqkx.2019.173

Citation:

Ye Lina, Sun Fengyue, Wang Li, Liu Jinlong, Zhang Yuting, 2020. Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Composition of the Quartz Monzonite Porphyry Intrusion from East Jilin Province. Earth Science, 45(5): 1544-1555. doi: 10.3799/dqkx.2019.173

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Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Composition of the Quartz Monzonite Porphyry Intrusion from East Jilin Province

doi: 10.3799/dqkx.2019.173

Ye Lina^{1
,
,},
Sun Fengyue^{1
,
,
,},
Wang Li¹,
Liu Jinlong²,
Zhang Yuting¹

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Shenyang Center, China Geological Survey, Shenyang 110034, China

Received Date: 2019-07-24
Publish Date: 2020-05-15

Abstract

Abstract

The distribution of Jurassic granite in the eastern Jilin province is relatively limited, with little discriminant evidence for regional tectonic evolution. This paper presents a synthesis study of zircon U-Pb chronology and geochemistry and Hf isotopes of the quartz monzonite porphyry in this area. The rocks yield an average zircon LA-ICP-MS U-Pb age of 165±1 Ma, indicating the Middle Jurassic. They show high SiO₂(61.01%-61.99%), ALK(5.78%-7.98%), belonging to calc-alkaline granites. In addition, they also display the characteristics of I-type granite with obvious enrichment in LREE, unconspicuous europium anomalies (0.92-1.01), low MgO, CaO, Fe₂O₃^Tas well as A/CNK(1.02-1.39). The Eu/Eu* values vary from -15.46 to -17.04, and T_DM2=2 189-2 289 Ma. These samples are enriched in LILE and depleted in HFSE, with Mg^#=26.90-33.04, low Yb(0.43×10^-6~0.48×10^-6) and Y(6.63×10^-6~7.12×10^-6). Zircon Ti temperature averages 744 ℃, belonging to low temperature granite. The magma was originated from the partial melting of Paleo-Proterozoic lower crust. The middle Jurassic igneous rocks in the eastpartofnorthern margin of the North China Craton were formed in the subduction rather than the remote effect of Mongols-Okhotsk Ocean closure. From late Jurassic to early Cretaceous, the continental margin of northeast China maydisplay the structural features of strike-slip.
- quartz monzonite porphyry,
- zircon U-Pb dating,
- Hf isotope,
- geochemistry

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References(60)

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Zircon U-Pb Geochronology, Geochemistry and Hf Isotopic Composition of the Quartz Monzonite Porphyry Intrusion from East Jilin Province

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