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陆缘深水区重力流与底流交互作用的过程、响应及动力学机制是海洋沉积学研究的前沿和薄弱环节。在不发育堤岸且持续地向一个方向迁移的深水单向迁移水道内，重力流(包括浊流)和底流(等深流、内波和潮汐底流)同时、同地存在，是重力流与底流交互作用有利的形成发育场所。
深水单向迁移水道内的重力流与底流交互作用研究
【摘 要】
：
陆缘深水区重力流与底流交互作用的过程、响应及动力学机制是海洋沉积学研究的前沿和薄弱环节。在不发育堤岸且持续地向一个方向迁移的深水单向迁移水道内，重力流(包括浊
【机 构】
：
浙江大学海洋学院,浙江舟山310058;油气资源与探测国家重点实验室(中国石油大学(北京)),北京102249DepartmentofGeologicalSciences,JacksonSchoolo
【出 处】
：
2015全国沉积学大会
【发表日期】
：
2015年10期
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