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- W2010478985 abstract "The Paleozoic tectonic evolution of Hsieh-fen-shan, western Hunan, belongs to the Caledonian and Hercynian tectonic cycles. The base of the lower Paleozoic group is defined by a geographical unconformity; the Sinian system unconformably overlies the Pan-ch'i group of the Proterozoic. The Hsieh-fen movement represented by this unconformity had not transformed this area into a platform. The lower Paleozoic group may be divided into four structural stages: Lower Sinian, Upper Sinian-Cambrian, Lower Ordovician and Middle Ordovician-Silurian. These stages are represented by the corresponding sedimentary formations: lower terrigenous elastic formation, siliceous and carbonate rocks intercalated with shale, flush formation and upper terrigenous elastic. Due to the absence of magmatic activity it is believed to be of the miogeosyncline type. In the Variscan cycle this area was already consolidated and partly covered with upper Paleozoic neoplatform sediments. Hereditary characters of the early Paleozoic tectonic ..." @default.
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- W2010478985 date "1968-11-01" @default.
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- W2010478985 title "Developmental history of Paleozoic structure of Hsieh-fen-shan region of western Hunan and problem of boundary of Southwest Platform" @default.
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- W2010478985 doi "https://doi.org/10.1080/00206816809474996" @default.
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