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Source-to-sink of Late carboniferous Ordos Basin:Constraints on crustal accretion margins converting
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文山古木街台地东部边缘泥盆纪的斜坡碳酸盐沉积类型包括重力流和非重力流,重力流有碎屑流、滑移滑积层及浊流;常见的层序组合有3......
