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논문 기본 정보

자료유형
학술저널
저자정보
Zhouxuan Xiao (School of Earth Science and Resources Chang’an University China) Licheng Ma (Key Laboratory of Paleomagnetism and Tectonic Reconstruction Ministry of Land and Resources China) Wan Jiang (Key Laboratory of Paleomagnetism and Tectonic Reconstruction Ministry of Land and Resources China) Ran Wang (School of Earth Science and Resources Chang’an University China) Yuyan Yao (School of Earth Science and Resources Chang’an University China) Jie Cai (School of Earth Science and Resources Chang’an University China) Jingyu Lin (School of Earth Science and Resources Chang’an University China) Lu Li (School of Earth Science and Resources Chang’an University China)
저널정보
한국지질과학협의회 Geosciences Journal Geosciences Journal Vol.24 No.3
발행연도
2020.1
수록면
249 - 266 (18page)

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초록· 키워드

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Detailed petrologic, geochemical and geochronological investigation on migmatites provide key information on the tectonic-magmatic history of the Quanji Massif, NW China. The studied migmatites are mainly composed of granitic gneisses, with lenticular refractory residua spread along its foliation. Zircon U-Pb ages of 1129.2 ± 7.4 Ma (1σ, MSWD = 0.34, N = 31) and 1135.1 ± 9.5 Ma (1σ, MSWD = 0.05, N = 22) were determined for the granitic gneiss and refractory residue, respectively. Garnet grains from the refractory residue show no distinctive intra-crystalline zonation, and are rich in Fe and Mg, but poor in Ca and Mn, akin to those from metapelite. Samples from the granitic gneisses have high contents of SiO2 (from 67.92% to 69.89%), K2O (from 3.94% to 5.00%) and A/CNK (1.11–1.17), with LREE enrichment and distinctly negative Eu anomalies (Eu/Eu* = 0.49–0.53) in the chondrite-normalized REE patterns, and significantly negative Nb, Ta, Ti and Sr anomalies in the primitive mantle-normalized spider diagrams. Granitic gneisses samples have consistent Nd isotope compositions with negative εNd(t) values ranging from –1.06 to –6.04, and TDM model ages ranging from 1.83 to 2.23 Ga. These geochemical features suggest that the granitic rocks belong to the S-type granites, which were predominately derived from a late Paleoproterozoic crustal source. The granitic gneiss was probably formed by partial melting of the sediments which had been suffered graunlite-facies metamorphism. The components with low melting points (e.g., felsic minerals) might replace the sediments to form migmatites and migmatitic granites, and thus preserved the refractory residua. Therefore, the late Mesoproterozoic orogenic event is the coeval response of the global Grenvillian orogeny, indicating an important crustal remelting episode in the Quanji Massif.

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