大陆斜坡是联系浅水台地与深水盆地的枢纽地带，以包括巨大岩块在内的巨厚斜坡边缘型沉积为特征。
The continental slope is the key zone connecting the shallow platform and the deep basin. It is of the feature of thick slope margin sediments including huge rock blocks.
它们位于大陆边缘区的后缘，其地球动力学作用以大陆架、大陆斜坡和边缘海沉降区域的裂谷作用为特征。
These are proper rear boundaries of continental margins, the geodynamics of which are characterized by rifting on shelves, continental slopes, and marginal oceanic depressions.
它们能经常在大陆架的斜坡上找到，尽管目前来看其开采难度之大令人望而却步。
They can often be found on the slopes of the continental shelf, though as yet they are impossibly awkward to extract.
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