大别山北淮阳带东段石榴斜长角闪岩石炭纪变质作用的测定

刘贻灿; 王辉; 杨阳; 侯克斌; 李洋; 宋彪

doi:10.3799/dqkx.2019.082

Volume 45 Issue 2

Feb. 2020

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Article Navigation > Earth Science > 2020 > 45(2): 355-366

Liu Yican, Wang Hui, Yang Yang, Hou Ke-Bin, Li Yang, Song Biao, 2020. Dating of Carboniferous Metamorphism for Garnet Amphibolite from the Eastern Beihuaiyang Zone in the Dabie Orogen. Earth Science, 45(2): 355-366. doi: 10.3799/dqkx.2019.082

Citation:

Liu Yican, Wang Hui, Yang Yang, Hou Ke-Bin, Li Yang, Song Biao, 2020. Dating of Carboniferous Metamorphism for Garnet Amphibolite from the Eastern Beihuaiyang Zone in the Dabie Orogen. Earth Science, 45(2): 355-366. doi: 10.3799/dqkx.2019.082

Citation:

Liu Yican, Wang Hui, Yang Yang, Hou Ke-Bin, Li Yang, Song Biao, 2020. Dating of Carboniferous Metamorphism for Garnet Amphibolite from the Eastern Beihuaiyang Zone in the Dabie Orogen. Earth Science, 45(2): 355-366. doi: 10.3799/dqkx.2019.082

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Dating of Carboniferous Metamorphism for Garnet Amphibolite from the Eastern Beihuaiyang Zone in the Dabie Orogen

doi: 10.3799/dqkx.2019.082

Liu Yican^{1
,
,},
Wang Hui¹,
Yang Yang¹,
Hou Ke-Bin^1,2,
Li Yang¹,
Song Biao³

1.
CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
2.
Anhui Academy of Geological Survey, Hefei 230001, China
3.
Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2019-02-18
Publish Date: 2020-02-15

Abstract

Abstract

In comparison with the Triassic ultra-high-pressure metamorphic belt in the southern Dabie orogen, the Beihuaiyang zone (BZ) is generally regarded to be a relatively low-grade metamorphic unit located in the northern part of the orogen. The BZ can be subdivided into eastern and western segments separated by Shangcheng-Macheng fault zone, respectively. Among of them, the eastern segment of the BZ has no record related to Paleozoic oceanic subduction similar to those in the western segment. Also, there are rare reports on the Paleozoic magmatism and metamorphism in the region. As a result, these have greatly impeded the deep understanding and precise recognition on the formation and evolution of the Dabie orogen. The eastern segment of the BZ is mainly composed of three groups of rocks:(1) metamorphic rocks, e. g., meta-granitoid (granitic gneiss), (garnet) amphibolite, marble, mica-quartz schist and meta-flysch; (2) igneous rocks mainly including Mesozoic granite, syenite and volcanics; (3) basin sediments mainly composed of Mesozoic-Cenozoic and subordinate Carboniferous rocks. However, no petrological record of the Paleozoic metamorphism has been reported in the region. Therefore, SHRIMP zircon U-Pb dating and preliminary petrographic observations on the garnet amphibolite coexisting with marble from Tiechong, Jinzhai in the eastern segment of the BZ are carried out in this study. The results suggest that the studied rocks experienced a strong metamorphism with the peak at 355±5 Ma. It is reported for the first time on the Carboniferous metamorphism in the region, and thus provides new constraints on the eastern extension of the Qinling-Tongbai orogen and the Paleozoic tectonic evolution of the Dabie collisional orogen.
- zircon,
- SHRIMP U-Pb dating,
- garnet amphibolite,
- Carboniferous metamorphism,
- eastern segment of the Beihuaiyang zone,
- Dabie orogen,
- geochemistry

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References(104)

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Dating of Carboniferous Metamorphism for Garnet Amphibolite from the Eastern Beihuaiyang Zone in the Dabie Orogen

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