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- W2376245220 abstract "Beihuaiyang tectonic belt lies in the northern margin of the Dabie Mountains. The Foziling lithogroup, one of the metamorphic tectono-stratigraphic units in the eastern part of the belt, is the key to a better understanding of the evolution of the Beihuaiyang tectonic belt. The Huanglonggang lithoformation occurred as a tectonic boundary zone which separates the upper part of the Foziling lithogroup from the lower part of the same Lithogroup. The upper part differs from the lower part in many aspects, such as in metamorphism and in deformation. The lower part of the Foziling lithogroup is composed of Zhengtangzi, Xianrenchong and Xiangyunzhai lithoformations. It's characterized by the development of the intra-folds, which is interpreted as the result of extensional tectonic deformation. The deformations in the lower part indicate an extensive tectonic replacement. In contrast, the upper part of the Foziling lithogroup, which consists of Zhufoan, Badaojian and Panjialing lithoformations, is dominated by buckling deformation, which is thought to be the result of contraction in crust. Based on our study, we propose to divide the former Foziling lithogroup into two lithogroups: The lower part named as Luzhenguan melange and the upper part Zhufoan lithogroup. The former Huanglonggang lithoformation is identified as a horizontal ductile detachment shear zone." @default.
- W2376245220 created "2016-06-24" @default.
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- W2376245220 date "2004-01-01" @default.
- W2376245220 modified "2023-09-25" @default.
- W2376245220 title "Earlier deformation of the metamorphic tectono-stratigraphic unitin the eastern Beihuaiyang belt and its significance in regional geology" @default.
- W2376245220 hasPublicationYear "2004" @default.
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