origin of slope-break 坡折带成因
pattern of slope-break 坡折带类型
evolution of slope-break 坡折带演化
Characteristics of Slope Break Belt 大型坳陷湖盆沉积坡折带特征及其对砂体与油气的控制作用以鄂尔多斯盆地三叠系延长组为例
One possibility is that the spring sunshine caused blocks of the ice to expand and break apart, sending loose dust and ice particles crashing down the slope.
一种可能的解释是春季逐渐强烈的光照使得这些干冰膨胀破裂，挤压悬崖边疏松的土和冰滚落下来。
The fault slope break is a favorable area of oil accumulation and new target of subtle reservoir exploration in terrigenous fault-depression.
断层坡折带是油气藏聚集的有利地带，也是陆相断陷盆地隐蔽油气藏勘探的新领域。
The depositional slope-break belt controls the development of sediment system of eroded valley-low stand delta.
低水位时期坡折带控制了下切谷-低位三角洲沉积体系的发育。
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