Ice-molten sedimentary structure is a kind of ice-induced sedimentary structure controlled mainly by ice.
冰成沉积构造是在冰直接控制下而形成的沉积构造,冰融沉积构造是其中的一类。
According to the sedimentary structure and lithology, the turbidite may be divided into the four types of turbidite facies.
按照沉积结构,构造和岩性特征,可划分出四种浊积岩相类型。
To restore the original occurrence condition of a primary sedimentary structure is a routine work for palaeocurrent analysis.
恢复原生沉积构造的原始产状要素,是古水流分析中的一项重要基础工作。
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