等深流（Contour current）是指沿海底等深線水平流動的底流，平行海底等深線穩定低速流動，此種海底流是由溫鹽差（thermohaline）導致的海底地轉流（geostraphic bottom current）。[1]。這一地質名詞最先由Hollister和Heezen於1972年提出[2]。
參考來源
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