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Post-subduction margin structures along Boyd Strait, Antarctic Peninsula

机译:南极半岛博伊德海峡沿俯冲带的边缘构造

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The Pacific margin of the Antarctic Peninsula to the southwest of the Hero Fracture Zone (HFZ) is a former subducting margin which became inactive following the arrival of ridge crest segments of the Antarctic - Phoenix ridge at the margin during the Tertiary. In contrast, the part of the margin to the northeast of the HFZ remains active. Tertiary convergence was approximately perpendicular to the margin and ongoing motion is thought to have the same orientation. A new seismic reflection profile running along Boyd Strait, just northeast of the landward projection of the HFZ, shows major structural components similar to those typically observed along the margin to the southwest of the HFZ. In order of increasing proximity to the margin, these components are: the inner shelf, the shelf basin, the mid-shelf basement high (MSBH), and the outer shelf. The continuation of the post-subduction margin structures to the active margin suggests that the boundary between crust with passive and active margins characteristics is not sharply defined. Our postulated scenario for tectonic evolution along Boyd Strait is that: (1) before the arrival of the last ridge crest segment to the southwest of the HFZ, the inner shelf and the shelf basin were part of a Cretaceous-Tertiary arc and forearc area, (2) after the arrival, thermal effects resulting from interaction of the ridge crest with the margin just southwest of the HFZ lead to the formation of the MSBH to the northeast, but MSBH uplift in Boyd Strait did not prevent concurrent cross-shelf sediment transport contributing to development of an extensive outer shelf on the seaward flank of the MSBH, (3) Recent extension in Bransfield Strait, a marginal basin to the northeast of the landward projection of the HFZ, has caused about 10 kin of seaward deflection in the strike of the part of the MSBH to the northeast of the projection of the HFZ. (C) 2002 Elsevier Science B.V. All rights reserved. [References: 24]
机译:南极半岛太平洋边缘在英雄断裂带(HFZ)的西南部是一个前俯冲边缘,随着第三纪南极-凤凰山脊的脊顶段到达边缘,该俯冲边缘变得不活动。相反,HFZ东北边缘的部分仍处于活动状态。三级会聚大致垂直于边缘,并且正在进行的运动被认为具有相同的方向。沿着HFZ陆地投影东北方的博伊德海峡(Boyd Strait)的新地震反射剖面显示出主要结构成分,与HFZ西南边缘通常观察到的相似。为了增加与边缘的距离,这些组成部分是:内部货架,货架盆地,中层货架高地下室(MSBH)和外部货架。俯冲后边缘结构到活动边缘的延续表明,具有被动边缘和主动边缘特征的地壳之间的边界没有被清晰地定义。我们在博伊德海峡沿岸构造演化的假定情景是:(1)在最后的脊峰段到达HFZ西南之前,内陆架和陆架盆地是白垩纪-第三系弧和前臂区域的一部分, (2)到达后,由于脊顶与HFZ西南缘的相互作用而产生的热效应导致向东北方向形成MSBH,但博伊德海峡的MSBH隆升并未阻止同时发生的跨架沉积物迁移(3)布兰斯菲尔德海峡(HFZ的陆地向东北方向的边缘盆地)最近的扩张,导致罢工造成约10平方公里的海向偏转MSBH到HFZ投影东北的部分。 (C)2002 Elsevier Science B.V.保留所有权利。 [参考:24]

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