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The 2011 Mw 6.8 Burma earthquake: fault constraints provided by multiple SAR techniques

机译:2011年mw 6.8缅甸地震:多种saR技术提供的断层限制

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摘要

We used two tracks of ALOS PALSAR images to investigate the focal mechanism and slip distribution of the 2011 March 24, MW 6.8 Burma strike-slip earthquake. Three different SAR techniques, namely conventional interferometry, SAR pixel offsets (SPO) and multiple-aperture InSAR (MAI), were employed to obtain the coseismic surface deformation fields along the ∼30 km length of the fault rupture. Along-track measurements from SPO and MAI techniques show a high correlation, and were subsequently used to precisely determine the location and extent of the surface fault trace. The best-fitting fault model geometry derived from an iterative inversion technique suggests that the rupture occurred on a near-vertical sinistral strike-slip fault west of the Nam Ma fault with a strike of 70°. A maximum slip of 4.2 m occurs at a depth of 2.5 km, with significant slip constrained only to the upper 10 km of the crust.
机译:我们使用两条轨道的ALOS PALSAR图像调查了2011年3月24日MW 6.8缅甸走滑地震的震源机制和滑动分布。三种不同的SAR技术,即常规干涉法,SAR像素偏移(SPO)和多孔径InSAR(MAI),被用于获得沿断裂破裂长度约30 km的同震表面形变场。 SPO和MAI技术的沿轨测量显示出高度相关性,随后被用于精确确定表面断层痕迹的位置和范围。由迭代反演技术得出的最佳拟合断层模型几何形状表明,破裂发生在南马断裂以西的近垂直左旋走滑断裂上,走向为70°。最大的滑移发生在深度为2.5千米的情况下,最大滑移发生在地壳的上10千米处。

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