扬子地块西北缘~2.09 Ga和~1.76 Ga花岗质岩石：Columbia超大陆聚合-裂解的岩浆记录

邓奇; 汪正江; 任光明; 崔晓庄; 曹华文; 宁括步; 任飞

doi:10.3799/dqkx.2020.182

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3295-3312

Deng Qi, Wang Zhengjiang, Ren Guangming, Cui Xiaozhuang, Cao Huawen, Ning Kuobu, Ren Fei, 2020. Identification of the ~2.09 Ga and ~1.76 Ga Granitoids in the Northwestern Yangtze Block: Records of the Assembly and Break-Up of Columbia Supercontinent. Earth Science, 45(9): 3295-3312. doi: 10.3799/dqkx.2020.182

Citation:

Deng Qi, Wang Zhengjiang, Ren Guangming, Cui Xiaozhuang, Cao Huawen, Ning Kuobu, Ren Fei, 2020. Identification of the ~2.09 Ga and ~1.76 Ga Granitoids in the Northwestern Yangtze Block: Records of the Assembly and Break-Up of Columbia Supercontinent. Earth Science, 45(9): 3295-3312. doi: 10.3799/dqkx.2020.182

Citation:

Deng Qi, Wang Zhengjiang, Ren Guangming, Cui Xiaozhuang, Cao Huawen, Ning Kuobu, Ren Fei, 2020. Identification of the ~2.09 Ga and ~1.76 Ga Granitoids in the Northwestern Yangtze Block: Records of the Assembly and Break-Up of Columbia Supercontinent. Earth Science, 45(9): 3295-3312. doi: 10.3799/dqkx.2020.182

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Identification of the ~2.09 Ga and ~1.76 Ga Granitoids in the Northwestern Yangtze Block: Records of the Assembly and Break-Up of Columbia Supercontinent

doi: 10.3799/dqkx.2020.182

1.
Chengdu Center, China Geological Survey, Chengdu 610081, China
2.
Key Laboratory for Sedimentary Basin and Oil and Gas Resources, Ministry of Natural Resources, Chengdu 610081, China

Received Date: 2020-05-06
Publish Date: 2020-09-15

Abstract

Abstract

The Yangtze Block preserves large quantities of Paleoproterozoic rocks which hold the evidence of the Columbia supercontinent cycle, however, its evolution from the assembly to break-up and relative location in the palaeosupercontinent, are still in dispute. In this study, we present an integrated dataset of whole-rock geochemistry, zircon U-Pb age and Lu-Hf isotope of the Mayuan and Baiyu granitoids in the Beiba area of the northwestern Yangtze Block. Zircon U-Pb dating reveals that the Mayuan granodiorite and the Baiyu K-feldspar granite were emplaced at ~2 090 Ma and ~1 760 Ma, respectively. Geochemically, the Mayuan granodiorite shows strongly peraluminous characteristics with depletion in Sr, Cr, Ni, enrichment in Y and Yb, relatively enriched in LREE and depleted in HFSE, and these features bear resemblance to those of cal-alkali granite; in addition, its zircon Lu-Hf isotopic analyses yield positive ε_Hf(t) values of +0.91 to +2.59. The Baiyu K-feldspar granite is alkali-rich and enriched in Sr, low Al, Mg, Mn and P, with A/CNK of 0.96-1.04; the trace elements show enrichment in Th, Na, Ta, Zr, Hf and depletion in Sr, Eu, with high total REE concentration, high LREE/HREE ratio, and strongly negative Eu anomalies; moreover, the granite has high HFSEs (Zr+Nb+Ce+Y=797×10^-6-1 495×10^-6) and 10 000×Ga/Al ratios (3.30-3.73). Together with high zircon saturation temperatures (897-939 ℃) from the K-feldspar granite, they are classified as A-type granites with negative ε_Hf(t) values from -13.58 to -10.29. Integrated with the analysis of trace elements and oxygen fugacity of zircon and previous research results, the Mayuan 2 090-2 080 Ma granitoids were likely to be generated by remelting of both juvenile and old crustal components within an arc-related setting; the Baiyu 1 790-1 760 Ma K-feldspar granite may be derived from partial melting of ancient crustal materials within the intracontinental rift setting. And they are likely to be the responses to the assembly and break-up of the Columbia supercontinent. Taking account of geophysical data and magmatic-metamorphic events, it is suggested that the Yangtze Block was spatially linked to Laurentia in the Columbia supercontinent.
- Paleoproterozoic,
- zircon U-Pb dating,
- geochemistry,
- Columbia supercontinent,
- tectonic evolution,
- northwestern Yangtze Block

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References(101)

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