首页> 外文期刊>Open Journal of Geology >Detailed Study of Radon Spatial Anomaly in Tlamacas Mountain Area, Volcano Popocatepetl, Mexico
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Detailed Study of Radon Spatial Anomaly in Tlamacas Mountain Area, Volcano Popocatepetl, Mexico

机译:墨西哥波波卡特佩特火山Tlamacas山区of空间异常的详细研究

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Results of a soil radon survey accomplished by 2 different methods during 2 different periods in the area of Tlamacas Mountain are presented. The first study, carried out from 15-APR-2010 to 09-MAY-2010 in 30 measurement sites by means of CR39 solid state nuclear detectors, shows 2 active zones with intensive radon emanation with a characteristic dimension of about 300 meters located in the northwestern and western parts of the Mountain. The second survey, made on 05-JUL-2011 in 23 measurement sites with 10 min sampling by a SARAD RTM 1688 Radon/Thoron monitor, in contrast, revealed a sizeable area depleted in radon and 3 active areas of increased radon release in the lateral Mountain sides. These observed phenomena strengthen our assumption about the presence of an active geological structure in Tlamacas Mountain connected with a geodynamical processes in volcano Popocatepetl.
机译:介绍了在Tlamacas山地区在2个不同时期通过2种不同方法完成的土壤ra调查的结果。首次研究是通过CR39固态核探测器在2010年4月15日至2010年5月9日在30个测量地点进行的,显示了2个活动区,密集ra气散发,特征尺寸约为300米。山脉的西北和西部。相比之下,第二次调查于2011年7月5日在23个测量地点进行,并通过SARAD RTM 1688 Radon / Thoron监测仪进行了10分钟采样,结果显示ra中有一个较大的区域被耗尽,而lateral中3个活跃的区域在侧面中释放了更多的ra山边。这些观察到的现象加强了我们对Tlamacas山中活跃的地质结构与Popocatepetl火山的地球动力学过程相关的假设。

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