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Imaging trench-line disruptions: Swath mapping of subduction zone

机译:成像沟线破坏:俯冲带的条带图

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Analogous to other subduction zones in the world where the heavier oceanic plate shoves below the lighter continental plate, crustal movement along the Sumatra-Andaman trench line over the last two centuries released enormous stress causing earthquakes of highest impunity and generating, at times, devastating tsunamis. Such significant earth movements are presumed to have wide-ranging implications, stretching from geology to climate and to astronomy. A sea expedition within three months from the 2004 Sumatra-Andaman earthquake, and during the 2005 Sumatra earthquake is able to image the exact trench line, west of the Andaman Island. The multibeam bathymetry, gravity and fractal studies of about twenty-five thousand square kilometres off the west of Andaman Island have brought out several interesting features unknown earlier, including atypical disruption of the trench line.
机译:与世界上其他较重的俯冲带相比较,较重的洋洋板块推向较轻的大陆板块下方,过去两个世纪以来,沿苏门答腊-安达曼海沟线的地壳运动释放出巨大的压力,导致最高的有罪不罚地震,并有时造成毁灭性的海啸。据推测,这种重大的地球运动具有广泛的意义,从地质学到气候再到天文。从2004年苏门答腊-安达曼地震发生的三个月内,以及2005年苏门答腊地震期间,一次海上探险就可以对安达曼岛以西的确切海沟线进行成像。在安达曼岛以西约2万5千平方公里处进行的多波束测深,重力和分形研究,带来了一些以前未知的有趣特征,包括沟槽线的非典型破坏。

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