块体搬运的重力流顺斜坡演化为浊流，进入盆地轴部后转为由东往西顺盆地走向流动，并在轴部形成一套经典浊积岩。
The turbidity current transformed from gravitational sliding on slopes were transported from east to west along the axis of the basin.
沉积特征表明杂砾岩成因具冰海相和水下块体重力流的双重(复合)性质。
Based on depositional characteristics, the heterogeneous conglomerate has a dual character combining glaciomarine facies and subaqueous block flow by gravity in origin.
着重介绍了异地碳酸盐岩块体和碳酸盐岩重力流沉积的研究进展，即线源式的碳酸盐岩裙沉积和点源式的碳酸盐岩海底扇沉积；
This paper introduced the research progress of the allochthonous carbonate blocks and carbonate gravity flow for the line sourced carbonate aprons and the point sourced carbonate submarine fans.
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