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- W2387809586 abstract "An investigation of the structural deformation, metamorphism, illite crystallinity, and illite K-Ar and Rb—Sr dating of the Penglai Group of the Jiaobei region provides new information which constrains its tectonic history and style. The Penglai Group, the dominant outcrop of the Jiaobei region, experienced intense deformation and low greenschist facies metamorphism during the Carboniferous (299±4Ma) under regional NNE-SSW compression. This Penglai event in the Jiaobei Belt, which is located in the southern mar- gin of the North China Plate, occurred therefore as the result of collision between the North China and Yangtze plates along the Jiaonan belt. The analyses also suggest that the collision between the two plates to the east of the Tan-Lu Fault Zone took place in the Late Carboniferous. The post-Penglai event only caused local NNE-SSW trending structures in the Jiaobei region and is interpreted as the result of either the Indosinian Orogeny or the Jurassic Yanshanian Orogeny." @default.
- W2387809586 created "2016-06-24" @default.
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- W2387809586 date "1993-01-01" @default.
- W2387809586 modified "2023-09-28" @default.
- W2387809586 title "GEOTECTONIC IMPLICATIONS OF THE DEFORMATION AND METAMORPHISM OF THE PENGLAI GROUP OF THE JIAOBEI REGION, CHINA" @default.
- W2387809586 hasPublicationYear "1993" @default.
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