首页> 外文期刊>Journal of Volcanology and Geothermal Research >Reply to: Barazzuoli P., Bertini G., Brogi A., Capezzuoli E., Conticellin S., Doveri M., Ellero A., Gianelli G., La Felice S., Liotta D., Marronin M., Manzella A., Meccheri M., Montanari D., Pandeli E., Principe C.,n Ruggieri R., Sbrana A., Vaselli V., Vezzoli L.
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Reply to: Barazzuoli P., Bertini G., Brogi A., Capezzuoli E., Conticellin S., Doveri M., Ellero A., Gianelli G., La Felice S., Liotta D., Marronin M., Manzella A., Meccheri M., Montanari D., Pandeli E., Principe C.,n Ruggieri R., Sbrana A., Vaselli V., Vezzoli L.

机译:回复:Barazzuoli P.,Bertini G.,Brogi A.,Capezzuoli E.,Conticellin S.,Doveri M.,Ellero A.,Gianelli G.,La Felice S.,Liotta D.,Marronin M.,Manzella A ,Meccheri M.,Montanari D.,Pandeli E.,Principe C.,Ruggieri R.,Sbrana A.,Vaselli V.,Vezzoli L.

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摘要

The volcanic spreading model by Borgia et al. (2014) is accurate in describing the extensional structures found on the edifice and the radial compressional structures existing all around the base of Amiata Volcano. Volcanic conduits, extensional structures, and direct contact between the volcanic rocks and the Tuscan Units, constitute the hydraulic connection between the potable fresh-water aquifer contained in the volcanites and the underlying hydrothermal system. Therefore, gaseous phases tend
机译:Borgia等人的火山扩散模型。 (2014年)准确地描述了在建筑物上发现的延伸结构以及遍布Amiata火山底部的径向压缩结构。火山管道,伸展结构以及火山岩石与托斯卡纳单元之间的直接接触,构成了火山岩中所含的饮用水和地下热液系统之间的水力连接。因此,气相倾向于

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