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A precise bathymetric map of the world’s deepest seafloor, Challenger Deep in the Mariana Trench

机译:这是世界上最深海底的精确测深图,马里亚纳海沟的挑战者深海

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摘要

Data from three bathymetric surveys by R/V Kairei using a 12-kHz multibeam echosounder and differential GPS were used to create an improved topographic model of the Challenger Deep in the southwestern part of the Mariana Trench, which is known as the deepest seafloor in the world. The strike of most of the elongated structures related to plate bending accompanied by subduction of the Pacific plate is N70°E and is not parallel to the trench axis. The bending-related structures were formed by reactivation of seafloor spreading fabric. Challenger Deep consists of three en echelon depressions along the trench axis, each of which is 6-10 km long, about 2 km wide, and deeper than 10,850 m. The eastern depression is the deepest, with a depth of 10,920 ± 5 m.
机译:R / V Kairei使用12 kHz多波束回声测深仪和差分GPS进行的三次测深调查的数据,被用于在马里亚纳海沟西南部创建挑战者深部的改进地形模型,该模型被称为马里亚纳海沟中最深的海底。世界。与平板弯曲有关的大多数细长结构的冲击伴随太平洋板块的俯冲为N70°E,并且不平行于沟槽轴。弯曲相关的结构是通过重新活化海底铺布形成的。挑战者深处沿沟渠轴线包括三个梯形凹陷,每个凹陷长6至10公里,宽约2公里,深于10,850 m。东部凹陷最深,深度为10,920±5 m。

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