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首页> 外文期刊>Geophysical Research Letters >Deep source model for Nevado del Ruiz Volcano, Colombia, constrained by interferometric synthetic aperture radar observations
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Deep source model for Nevado del Ruiz Volcano, Colombia, constrained by interferometric synthetic aperture radar observations

机译:受干涉式合成孔径雷达观测约束的哥伦比亚内华多德尔鲁伊斯火山深源模型

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摘要

Nevado del Ruiz is part of a large volcano complex in the northern Andes of Colombia. Interferometric synthetic aperture radar observations from the RADARSAT-2 satellite since 2011 show steady inflation of the volcano since 2012 at 3-4cm/yr. The broad (>20km) deformation pattern from both ascending and descending track data constrain source models for either point or spheroidal sources, both located at >14km beneath the surface (mean elevation 4.2km) and 10km SW of Nevado del Ruiz, below nearby Santa Isabel Volcano. Stress change computations for both sources in the context of a compressive regional stress indicate that dikes propagating from the source should become trapped in sills, possibly leading to a more complex pathway to the surface and explaining the significant lateral separation of the source and Nevado del Ruiz Volcano.
机译:内华多德尔鲁伊斯(Nevado del Ruiz)是哥伦比亚北部安第斯山脉的一座大型火山群的一部分。自2011年以来从RADARSAT-2卫星进行的干涉式合成孔径雷达观测表明,自2012年以来火山以3-4厘米/年的速度稳定膨胀。来自上升和下降轨道数据的宽(> 20 km)形变模式限制了点或球状源的源模型,这些源模型都位于附近圣塔下方的内华多德尔鲁伊斯表面以下(平均海拔4.2 km)和西南10 km处> 14 km伊莎贝尔火山。在局部压缩应力的情况下,两种震源的应力变化计算表明,从震源传播的堤坝应被困在窗台中,可能导致通往地面的路径更加复杂,并解释了震源和内华达河谷鲁伊斯的明显横向分离火山。

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