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海底地形:索姆和哈特拉斯深海平原之间的分界线。

Ocean-Bottom Topography: The Divide between the Sohm and Hatteras Abyssal Plains.

出版信息

Science. 1965 Jun 18;148(3677):1598-9. doi: 10.1126/science.148.3677.1598.

Abstract

A compilation of precision echo soundings has delineated the complex topography between the Sohm and Hatteras abyssal plains off the Atlantic coast of the United States. At present the divide between the two plains is a broad, flat area about 4950 meters deep; however, the configuration of channels and depressions suggests spillage of turbidity currents from the Sohm Plain into the Hatteras Plain and a shifting of the divide toward the northeast. Hudson Canyon terminates in the divide area and has probably fed sediment into both plains.

摘要

一组精确的回声测深资料描绘了美国大西洋海岸附近的索姆和哈特拉斯深海平原之间复杂的地形。目前,两个平原之间的分界线是一个宽阔、平坦的区域,深度约为 4950 米;然而,通道和洼地的形态表明,索姆平原的浊流溢出到哈特拉斯平原,并且分界线正在向东北方向移动。哈德逊峡谷终止于分界线区域,可能已经向两个平原输送了沉积物。

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