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- W2364314285 abstract "Late Cenozoic sediments of great thickness are well developed at foreland basins on both sides of the Tianshan range. The rhythmic sedimentary sequences within these basins reflect the tectonic evolutionary history of Tianshan orogen. The sedimentary feature and sporopollen assemblage demonstrate that the elastics of Miocene -Pliocene -early Pleistocene have clearly increasing amount of unstable components and arid artemisia, lamb's -quarters, but less amount of sporopollens of broadieaf plants, indicating a higher activity of the Tianshan range. The rapid uplift of the Tianshan orogen during the late Pliocene led to the occurence of mollase deposits on foreland basins along both sides of the Tianshan mountains. The change of atmospheric circulation due to the oxogenic uplift caused a higher isolation of the basins on both sides of the range. A clear continental climate was so formed, resulted to an obvious climatic change." @default.
- W2364314285 created "2016-06-24" @default.
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- W2364314285 date "2000-01-01" @default.
- W2364314285 modified "2023-10-14" @default.
- W2364314285 title "DEPOSITIONAL CHARACTERISTICS OF LATE CENOZOIC AND THEIR TECTONIC SIGNIFICANCE OF FORELAND BASINS AT BOTH SIDES OF TIANSHAN MOUNTAINS IN CHINA" @default.
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