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首页> 外文期刊>The Open Geology Journal >Mapping and Assessment of Volcanic Hazards Related to the IgnimbriticEruption by AMS in Bambouto Volcano (Cameroon Volcanic Line)
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Mapping and Assessment of Volcanic Hazards Related to the IgnimbriticEruption by AMS in Bambouto Volcano (Cameroon Volcanic Line)

机译:班布图火山(喀麦隆火山线)中由AMS进行的与火成岩爆发有关的火山灾害的制图和评估

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Pyroclastic deposits constitute major components of explosive volcanic activity. To help improve the safety ofthe population faced with natural disasters, a study is carried out at Bambouto volcano with a view to map potentialhazards related to pyroclastic flows. The Bambouto volcano is indeed considered to be still active since the recentdiscovery of Quaternary basalts (0.5 Ma) at Totap, a locality situated near the Bambouto Caldera. This discovery has ledto reclassify Mount Bambouto among active volcanoes of Cameroon and, therefore, considered as potentially dangerous.The dangerousness of this volcano is accentuated by the presence of ignimbrites that are witnesses of ancient pyroclasticflows. Because a map of volcanic hazards is non-existent on the volcano, anisotropy of magnetic susceptibility (AMS) isthe method used in this paper to characterize magnetic fabrics and provides an estimate of flow direction of eachignimbrite sheet (represented by massive lapilli tuff and massive lithic breccia facies). Inferred transport directions basedon the AMS data and field indicators show that Bambouto Caldera is the source of main pyroclastic deposits of MountBambouto. These results have enabled us to produce a new hazard map related to potential future pyroclastic flows.
机译:火山碎屑沉积物是火山爆发活动的主要组成部分。为了提高面对自然灾害的人口的安全,在班博图火山进行了一项研究,以绘制与火山碎屑流有关的潜在危害。自从最近在Bambouto火山口附近的一个地区Totap发现第四纪玄武岩(0.5 Ma)以来,Bambouto火山确实被认为仍在活跃。这一发现使班博图山重新归类为喀麦隆的活火山,因此被认为具有潜在危险。火山喷发是古代火山碎屑流的见证,它的危险性更加突出。由于火山上不存在火山危害图,因此磁化率各向异性(AMS)是本文用来表征磁性织物的方法,并提供了每个火成岩片的流动方向的估算值(以块状的拉皮利凝灰岩和块状的石块表示)角砾岩相)。根据AMS数据和现场指标推断出的运输方向表明,班博托火山口是MountBambouto主要热碎屑沉积物的来源。这些结果使我们能够绘制与未来潜在的火山碎屑流有关的新危害图。

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