Quartenary palaeovolcanic structures and recent magmatic CO2 degassing zones in the Eger rift: The maar Mýtina / the scoria cone Zelezna hurka and the magmatically active zone of Milhostov - Hartousov

该项目的目的是研究更新世火山复合体Mytina Maar和火山渣锥Zelezna hurka/ eisenb<e:1>的结构和火山环境。主要结果将是该地区的古火山情景（地质模式、构造控制、喷发物分布）。结果将与米霍斯托夫-哈图索夫mofette油田的调查进行比较，在那里，地幔衍生的富含二氧化碳的流体的呼出是目前正在进行的岩浆和脱气过程的一种表达，在西埃格尔裂谷地区的大陆内岩石圈中，关于潜在的未来爆发。为了比较这两个地区，将解释以下方法：地电学、地磁、地震、重力和二氧化碳-土壤气体测量、岩石学-地球化学和遥感数据。预期的结果将有助于更好地了解地质、火山学和构造环境，并有助于绘制中欧埃格尔裂谷西部分区域未来火山风险评估的地图。

The aim of the project is to investigate the structure and volcanic setting of the Pleistocene volcanic complex Mytina Maar and the cinder cone Zelezna hurka/Eisenbühl. The principal result will be a palaeo volcanic scenario (geological model, tectonic control, distribution of eruptiva) of the region.The outcome will be compared with investigations in the mofette field of Milhostov- Hartousov, where the exhalation of mantle-derived CO2-enriched fluids is an expression of presently ongoing magmatic and degassing processes in the intra-continental lithosphere of the western Eger rift region, with regard to potential future eruptions.To compare both regions the following methods will be interpreted: geoelectrics, geomagnetics, seismics, gravity and CO2-soil gas measurements, petrographic-geochemical and remote sensing data.The expected results will be serve as for better understanding of geologic, volcanologic and tectonic settings as well as for to create maps of future volcanic risk assessment in sub-regions of the western Eger Rift, Central Europe.