Metadata 1500
Within the framework of an internal project of the Czech Geological Survey, a pilot GeoCIM model of a selected area in the Perštýn locality within the city of Liberec was developed. The work included the processing of available data obtained from data sources from CGS, from the Liberec City Hall and from the North Bohemian Museum in Liberec. In parallel to the research work, a proposal of possible layers of the model was prepared and consulted with the Liberec City Council. On the basis of the obtained da...
The EGDI3d database is a storage for geologic 3D models. Geometries from a variety of modelling tools are imported and stored in a common format, together with model metadata and geological descriptions in a GeoSciML inspired relational database.
The 3D model shows the shape of the paleo valley of the Svratka riverbed in the section between the villages of Doubravník and Borač. It allows to separately visualize faults, relief of the Svratka Crystalline complex and the Moravicum (crystalline complex), Neogene sediments and the modeled paleo valley itself. The spatial model of the paleo valley is set in the current relief. The model shows the basic faults that illustrate the overall tectonic complexity of the valley. The 3D model creates a spatial id...
Modelling areas of the different 3DGEO-EU workpackages.
Digital records of the gravity field changes in Greece (Nisyros, Thira) observed from repeated annual measuring campaigns in gravity network.
A layer represents aquifer media with direct of assignment of A index values for each aquifer delimitated (geological map of Atalanti 1:50.000 HSGME).
A layer represents aquifer media with direct of assignment of A index values for each aquifer delimitated.Higher values of “A” factor correspond to alluvial quaternary aquifers and Miocene sedimentary formations (sands and gravels). Smaller values represent areas with metamorphic and igneous rocks.
The aquifer media layer is created by direct assignment of aquifers to A index values from 1-10. The metamorphic and igneous rocks were given the lowest ‘A’-value of 3 and the karstified limestone is given the highest value of 10. The majority of the catchment can be grouped into bedded sedimentary rocks and given a value of 6.
The aquifer media layer is created by direct assignment of aquifers to A index values from 1-10. The majority of the catchment is underlain by karst and the karstified limestone is given the highest value of 10. The remainder of the catchment is considered bedded sedimentary rocks and given a value of 6.
The 3D depth model of the Entenschnabel region has been built during July 2018 to March 2019, as part of WP3 of the 3DGEO-EU project. It is a preliminary, generalized model that has been used as input for burial studies within the GARAH-project. The study area covers the Entenschnabel in the northwestern part of the German North Sea sector and the adjacent areas in Denmark and the Netherlands. The model is based on 8 seismically interpreted horizons.