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Sakai, Toshihiro; Matsuoka, Toshiyuki
JAEA-Research 2015-004, 109 Pages, 2015/06
We update the geologic map and the database of the geological mapping published by Funaki et al. (2005a) and Ota et al. (2007) based on geological survey and topographical analysis data in and around the Horonobe area. There are many geological survey data which are derived from natural resources (petroleum, natural gas and coal, etc.) exploration in and around Horonobe-cho. We also use these data in addition to data in Funaki et al. (2005a) and Ota et al. (2007)'s data. As results of this report, we also construct a digital geologic map and a digital database of geological survey using GIS. These results can be expected to improve the precision of modeling and analyzing of geological environment, and its long-term evaluation.
Mukoyama, Sakae*; Inomata, Takayuki*; Makita, Hiroko*
PNC TJ7362 96-001, 74 Pages, 1996/03
None
Hiura, Yuki; Kawamura, Makoto; Umeda, Koji*; Niwa, Masakazu
no journal, ,
One of the technical issues related to volcanic and igneous activities is the sophistication of technology for grasping the range of influence of magma. To address this issue, it is important to accumulate survey cases, especially when the dike develops over a radius of 15 km from the center of the Quaternary volcano, but it lies beneath the existing volcanic body. It is practically difficult to grasp the distribution of the conduits and the dikes derived from them. Therefore, the purpose of this study was to develop a method for estimating the distribution range of dikes distributed under the Quaternary volcanic body based on topographical data such as digital elevation models. In this study, we used digital maps and GIS software to target six volcanoes, such as stratovolcanoes and calderas. The parameters were measured, and modeling of the three-dimensional distribution range of radial dikes was examined from each parameter for each altitude. As a result, the transition of the center of gravity position for each altitude suggests the transition of the center of activity in the process of forming the volcanic body to some extent, and it is possible to extract not only the activity of the central crater but also the activity of lateral volcanoes. This suggests the possibility of quantitative evaluation of the transition and stability of the conduit even in volcanoes whose activity history is not clear by applying this method.
Nishiyama, Nariaki*; Kawamura, Makoto; Umeda, Koji*; Goto, Akira; Niwa, Masakazu
no journal, ,
The authors assume that the topography of the mountain body reflects the actual distribution area of the dike, and we are developing a method to do the model the distribution area of the center conduit and radial dikes by topographical analysis of the mountain body using GIS software. In this study, we proposed a method that enables topographical analysis volcanoes whose activity history is not clear, conducted topographical analysis at each volcano, and modeled the distribution area of dikes. As a result, the analysis method used in this study made it possible to capture the features of the topography formed by the activity of the volcano without including the expert judgement. This makes it possible to compare the analysis results of this study with the geology, and this analysis results are considered to be useful information. In addition, the distribution tendency of the centroid of each altitude obtained in this study shows the results consistent with the wide-area stress field at the time of the eruption, and shows the validity of the analysis results.
Kawamura, Makoto; Nishiyama, Nariaki; Niwa, Masakazu; Umeda, Koji*
no journal, ,
As the efforts of the notation, "examination of the method of estimating the distribution range of the rock veins distributed under the Quaternary volcano body based on the topographical data of the numerical elevation model" and "Collection and organization of dikes from geological maps (database)" was carried out. These studies are expected to be used as basic information for evaluating the direction and range that are likely to be affected by the horizontal movement of magma due to future volcanic and igneous activities.