The turbidity current transformed from gravitational sliding on slopes were transported from east to west along the axis of the basin.
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 Marine strata with different anti-deformability in the cover formed polydirectional and polyphase decollements under the tectonic compression and gravitational sliding.
盖层内抗变形能力不同的海相地层在构造推挤和重力滑动中形成了多期次、多方向的滑脱构造。
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