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Jian Zheng, Yehua Shan and Simin Hu    
It is generally accepted that during the Mesozoic NE-NNE-trending folds overprinted E-W-trending folds to form the Longshan dome in the central South China continent, although the interference map does not tell the relative ages of the fold sets. In an e... ver más
Revista: Geosciences    Formato: Electrónico

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