等深流是指沿海底等深线水平流动的底流,是因地球旋转而形成的温盐循环底流,平行海底等深线稳定低 速流动,主要在陆隆区。
等深流沉积是深水牵引流沉积中的一种重要类型。
A contourite is an important type of deep water traction current deposits.
在等深流与上覆低密度水体之间的界面上具备产生大规模界面内波的条件；
The contour currents colliding with the overlapped low density normal seawater can create internal waves of large scale at the interface of the thermohaline.
盐湖等深流沉积。风暴重力流、纵向重力流和滑塌重力流中的“ABAB”序和“BBB”序中—细砂岩是油气聚集的有利场所。
The "ABAB", "BBB" sequences middle-fine grained sandstones in longitudinal gravity flows, slide gravity flows and storm gravity flows are favorable for oil and gas accumulation.
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