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The Lüliang Complex is located at the western margin of the middle segment of the Trans-North China Orogen, along which the Western and Eastern Blocks collided to form the North China Craton. The complex mainly consists of metamorphosed granitic plutons and supracrustal rocks, of which the latter are subdivided into the Jiehekou, Lüliang, Yejishan, Lanhe and Heichashan Groups. The Lanhe Group is composed...
Meta-mafic rocks in the Daqingshan–Wulashan Complex, in the central segment of the Paleoproterozoic Khondalite Belt of the North China Craton, are composed predominantly of garnet-bearing mafic granulites, mafic granulites, and amphibolites. They occur mainly as irregular lenses and as a set of deformed dyke/sill swarms within dioritic–granitic orthogneisses and Al-rich paragneisses. An integrated...
Analyses of mineral inclusions within complexly zoned zircons, combined with SIMS UPb ages for various domains within the zircons, provide evidence of the origin and multistage metamorphic evolution of the Diancang Shan−Ailao Shan metamorphic complex, southeastern Tibetan Plateau. Zircons separated from paragneisses, amphibolites, garnet pyroxenites, and marbles were subdivided into inherited (magmatic...
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