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Basaltic Lava Characterization Using Magnetic Susceptibility Identification and Presence of Opaque Minerals in Ijen Volcanic Complex, Banyuwangi, East Java

机译:玄武岩熔岩表征使用磁敏感性识别和Ijen火山复合物,Banyuwangi,东爪哇省的不透明矿物质存在

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Reliable volcanic map and deep understanding of magmatic processes are very important in exploration of natural resources and mitigation of volcanic hazards. The conservative method in volcanic mapping still depends on qualitative approach thus it often failed to characterize volcanic products properly. Rock magnetic methods are quantitative approaches that classify rocks based on their magnetic properties. In this study, magmatic processes in basaltic lavas from Ijen volcanic complex in Banyuwangi, East Java were studied using combined rock magnetic and petrogenesis approaches. Samples of basaltic lavas from 13 localities, taken from three eruption sources were measured for their mass-specific magnetic susceptibility. The samples were then also subjected to petrographic and X-ray Fluorescence Spectrometry (XRF) analyses for their minerals composition and petrogenesis. Preliminary results show that the distinction in magnetic characters might be due to the quantity of magnetic minerals contained in rocks.
机译:可靠的火山地图和对岩石过程的深刻理解在探索自然资源和对火山危害的缓解方面非常重要。火山映射中的保守方法仍然取决于定性方法,因此它通常无法正确表征火山产品。岩石磁性方法是根据其磁性分类岩石的定量方法。在这项研究中,使用组合岩石磁性和培养方法研究了鲍拜旺岛的Iben火山复合物的玄武岩熔岩的岩石过程。测量从三个喷发源的玄武岩熔岩样品用于其质量特异性磁化率。然后还对样品进行岩体和X射线荧光光谱法(XRF)分析它们的矿物质组合物和纤维化。初步结果表明,磁性特征的区别可能是由于岩石中含有的磁性矿物的数量。

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