MODE-I区域的水深测量

Patricia A. Bush
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引用次数: 9

摘要

结合中大洋动力学实验(MODE-I)之前和期间的深度测深数据,生成了MODE-I区域1:50万比例尺和1:25万比例尺的水深图。七个海底地貌被命名。百慕大隆起的西南部分以崎岖不平的底部地形为特征,通常从东北偏北到西南偏南。在布雷克巴哈马外脊的东南部,一个与低大陆隆起的区域等高线相平行的地貌区域,以及沿着百慕大隆起的许多陡坡的相关深度,表明海底地形可能受到底部水流侵蚀的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Bathymetry of the MODE-I region

Depth soundings before and during the Mid-Ocean Dynamics Experiment (MODE-I) are integrated to produce bathymetric charts of the MODE-I region at scales of 1:500,000 and 1:250,000. Seven undersea features are named. The southwestern portion of the Bermuda Rise is characterized by rugged bottom topography generally striking north-northeast to south-southwest. Southeast of the Blake Bahama Outer Ridge, a zone of morphology paralleling the regional contours of the lower continental rise and associated deeps along many of the steep slopes on the Bermuda Rise suggest that the submarine terrain may be influenced by erosion by bottom currents.

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