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首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Tectonics of the Scotia-Antarctica plate boundary constrained from seismic and seismological data
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Tectonics of the Scotia-Antarctica plate boundary constrained from seismic and seismological data

机译:受地震和地震数据约束的斯科舍-南极板块边界的构造

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The plate boundary between the Scotia and Antarctic plates runs along the broadly E-W trending South Scotia Ridge. It is a mainly transcurrent margin that juxtaposes thinned continental and transitional crust elements with restricted oceanic basins and deep troughs. Seismic profiles and regional-scale seismological constraints are used to define the peculiarities of the crustal structures in and around the southern Scotia Sea, and focal solutions from recent earthquakes help to understand the present-day geodynamic setting. The northern edge of the western South Scotia Ridge is marked by a sub-vertical, left-lateral master fault. Locally, a narrow wedge of accreted sediments is present at the base of the slope. This segment represents the boundary between the Scotia plate and the independent South Shetland continental block. Along the northern margin of the South Orkney microcontinent, the largest fragment of the South Scotia Ridge, an accretionary prism is present at the base of the slope, which was possibly created by the eastward drift of the South Orkney microcontinent and the consequent subduction of the transitional crust present to the north. East of the South Orkney microcontinent, the physiography and structure of the plate boundary are less constrained. Here the tectonic regime exhibits mainly strike-slip behavior with some grade of extensional component, and the plate boundary is segmented by a series of NNW-SSE trending release zones which favored the fragmentation and dispersion of the crustal blocks. Seismic data have also identified, along the north-western edge of the South Scotia Ridge, an elevated region - the Ona Platform - which can be considered, along with the Terror Rise, as the conjugate margin of the Tierra del Fuego, before the Drake Passage opening. We propose here an evolutionary sketch for the plate boundary (from the Late Oligocene to the present) encompassing the segment from the Elephant Island platform to the Herdman Bank.
机译:Scotia和南极板块之间的板块边界沿E-W趋势的南Scotia脊延伸。它是主要的逆流边缘,与稀薄的大陆和过渡壳元素并列,这些海盆和海盆受到限制。地震剖面和区域规模的地震学约束条件用于定义斯科舍海南部及其周边地区的地壳结构的特殊性,而最近地震的焦点解决方案有助于了解当今的地球动力学环境。南斯科舍省脊西部的北部边缘有一个亚垂直的左主断裂。在局部,斜坡底部有一个狭窄的积聚沉积物楔子。该线段代表了斯科舍板块与独立的南设得兰群岛大陆块之间的边界。沿着南奥克尼微大陆的北缘,即南斯科舍海脊的最大片段,在斜坡的底部存在一个增生棱镜,这可能是由于南奥克尼微大陆向东漂移并随后俯冲而形成的。北部存在过渡壳。在南奥克尼州微大陆以东,板块边界的生理特征和结构受到的约束较少。这里的构造状态主要表现为走滑行为,并具有一定程度的伸展分量,板块边界被一系列NNW-SSE趋势释放带分割,有利于地壳块的破碎和分散。地震数据还沿着南斯科舍脊的西北边缘确定了一个高架区域-奥纳平台-与德雷克山脉一起,可以将其视为恐怖山脉的共轭边缘,在德雷克山脉之前通道开口。我们在这里提出板块边界的演化草图(从晚渐新世到现在),包括从象岛平台到赫德曼河岸的部分。

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