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首页> 外文期刊>Journal of Volcanology and Geothermal Research >Comparative mass balance of volcanic edifices at the southern volcanic zone of the Andes between 33°S and 46°S
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Comparative mass balance of volcanic edifices at the southern volcanic zone of the Andes between 33°S and 46°S

机译:安第斯山脉南部火山区33°S至46°S之间的火山构造的相对质量平衡

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Volcano edifice volume calculations are presented for 65 volcanoes of the 1400 km long Chilean Southern Volcanic Zone (SVZ) as a basic step in subduction zone mass budgets. Volume calculations are performed in a Geographical Information System that integrates Digital Elevation Models based on of Shuttle Radar Topography Mission as well as ASTER-GDEM topographic data, LANDSAT satellite images and geological maps. The method of volume calculation is straightforward for isolated, morphologically well-defined stratovolcanoes. Uncertainties increase for volcanic edifices that formed on pre-existing rugged terrain, for multi-phase eruptive centers, as well as for eroded edifices. A revised segmentation of the arc is used to describe the spatial volume distribution of extruded magma along the SVZ and to discuss controlling tectonic factors. Peak volumes between arc and back arc are offset by 400 km. The total volcanic extrusion is in the range of 10-13 km~3/km/Ma. Major differences between the SVZ and the Central American subduction system are notable with regard to volcano density and maximum volumes.
机译:给出了1400公里长的智利南部火山区(SVZ)中65座火山的火山建筑物体积计算,这是俯冲带总体预算的基本步骤。在地理信息系统中执行体积计算,该系统集成了基于航天飞机雷达地形任务的数字高程模型以及ASTER-GDEM地形数据,LANDSAT卫星图像和地质图。对于孤立的,形态学明确的平流层火山,体积计算方法非常简单。在预先存在的崎地形上形成的火山建筑物,多相喷发中心以及侵蚀建筑物的不确定性增加。弧线的修正分段用于描述挤压岩浆沿SVZ的空间体积分布,并讨论控制构造因素。弧和反弧之间的峰值量相差400 km。火山喷发总量在10-13 km〜3 / km / Ma范围内。 SVZ和中美洲俯冲系统之间的主要区别是火山密度和最大体积。

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