云开地块印支期构造热事件叠加改造：来自片麻岩中多矿物U-Pb年代学的证据

王祥东; 徐德明; 王磊; 周岱; 胡军; 柯贤忠

doi:10.3799/dqkx.2019.151

Volume 45 Issue 5

May 2020

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Article Navigation > Earth Science > 2020 > 45(5): 1653-1675

Wang Xiangdong, Xu Deming, Wang Lei, Zhou Dai, Hu Jun, Ke Xianzhong, 2020. Reworking of Indosinian Tectono-Thermal Events in the Yunkai Massif:Gneissic Multi-Mineral U-Pb Geochronological Evidence. Earth Science, 45(5): 1653-1675. doi: 10.3799/dqkx.2019.151

Citation:

Wang Xiangdong, Xu Deming, Wang Lei, Zhou Dai, Hu Jun, Ke Xianzhong, 2020. Reworking of Indosinian Tectono-Thermal Events in the Yunkai Massif:Gneissic Multi-Mineral U-Pb Geochronological Evidence. Earth Science, 45(5): 1653-1675. doi: 10.3799/dqkx.2019.151

Citation:

Wang Xiangdong, Xu Deming, Wang Lei, Zhou Dai, Hu Jun, Ke Xianzhong, 2020. Reworking of Indosinian Tectono-Thermal Events in the Yunkai Massif:Gneissic Multi-Mineral U-Pb Geochronological Evidence. Earth Science, 45(5): 1653-1675. doi: 10.3799/dqkx.2019.151

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Reworking of Indosinian Tectono-Thermal Events in the Yunkai Massif:Gneissic Multi-Mineral U-Pb Geochronological Evidence

doi: 10.3799/dqkx.2019.151

Wuhan Center of China Geological Survey, Wuhan 430205, China

Received Date: 2019-06-20
Publish Date: 2020-05-15

Abstract

Abstract

The Phanerozoic tectonic evolution of the Yunkai massif has long been one of the hot topics in the South China Block. LA-ICP-MS U-Pb dating was carried out on the monazite, apatite and zircon of two gneiss samples from the Yunkai massif, yielding two magmatic zircon ages of 434±6 Ma (MSWD=3.0) and 437±12 Ma (MSWD=6.0) respectively, which represent the crystallization age of gneiss protolith (granitic rocks) and are basically consistent with the ages of regional Caledonian tectonic-magmatic-metamorphic-anatexis events responding to the Wuyi-Yunkai Caledonian orogenesis. Apatite yields metamorphic ages of 241±13 Ma (MSWD=2.2) and 242±6 Ma (MSWD=1.4) respectively; and monazite also yields metamorphic ages of 236.2±0.8 Ma (MSWD=0.66) and 229.4±1.2 Ma (MSWD=2.4) respectively. These U-Pb ages are consistent with the biotite Ar-Ar ages of the tectonite in the Yunkai massif, indicating the Indosinian (230-240 Ma) tectono-thermal reworking in the Yunkai massif. EPMA data of biotite from the gneiss show high Al, Ti and Mg contents, but low Fe content, with X_Mg ratios ranging from 0.37 to 0.45, which indicates ferruginous biotite affinity. The Ti saturation temperature of biotite is 650-700 ℃ (±50 ℃), agreeing with the monazite estimated temperature of 580-640 ℃ (±25 ℃), which indicates that the temperature of Indosinian reworking maybe reached up to 700 ℃. In conclusion, the present tectonic pattern of the Yunkai massif is superimposed by Indosinian tectono-thermal events on the basis of Caledonian orogeny, and the superimposed temperature may reach 700 ℃. In addition, the effect of Indosinian tectono-thermal events on mineral composition should be taken into account when restoring Caledonian metamorphic P-T path with mineral thermometers and baresthesiometers.
- multi-mineral U-Pb geochronology,
- mineral geochemistry,
- reworking,
- Indosinian,
- Yunkai massif,
- tectonics

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Reworking of Indosinian Tectono-Thermal Events in the Yunkai Massif:Gneissic Multi-Mineral U-Pb Geochronological Evidence

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