Metadata 1823
Structural geological 3D model of the area of interest was created in the MOVE software, which is suitable for the modelling of complex geological environment of the Bohemian massif crystalline and enables simple import and export of various data formats. The aim of the model is the unified visualisation of the geology and faults below the surface in correlation with the planned routes of the railway. The majority of the modelled area is located in the crystalline rocks of the Erzgebirge mountains which be...
Stratigraphic and structural model of the Neves-Corvo Region produced in the framework of the SMART EXPLORATION Project, based on geological, geophysical and drill hole data. It has three stratigraphic surfaces: Base of Mértola Formation, Top of Phylite Quartzite Formation, and in the Neves-Corvo mine region, the contact between the upper and lower Volcanic Sedimentary Complex is available.
The 3D geological model was created, in the framework of ProMine project, to integrate the geological knowledge of an extensive geophysical and geological research conducted in the Portuguese part of the Iberian Pyrite Belt. It was applied to the 100 x 25 km large Neves Corvo project area. The main purpose of the model was to foresee the existence of other massive sulfide deposits as to the well-known Neves Corvo orebodies.Stratigraphic and structural model based on geological, geophysical and drill hole ...
The Geological Map of the Fennoscandian Shield dataset shows fault and impact structures. This incorporates data from the map of the bedrock of Fennoscandia (2001) and new data on Quaternary geology.
Тhe Study describes all deposits of volcanic rocks, explored to be used as technical stone, as well as their spreading, prospective for detailed explorations. Depending on the structural-textural characteristics, volcanic rocks could be utilazed as broken and profiled stones, crushed stones of different granulation, used for railroads, roads and concrete, as well as architectural (decorative) stones (interiors, exterior, sculptural stone etc.). The most commonly exploited rocks here are diabase and serpent...
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Relict subaerial landslide feature. Where information is available these are subdivided further: 1. Slide deposit; 2. Slide scar (area of missing material on failure surface; 3. Other. Where information on the genesis is available that is also provided: 1. Rotational; 2. Translational; 3. Block; 4. Rockfall; 5. Debris Flow; 6. Creep; 7. Lateral Spread; 8. Debris avalanche; 9. Other. Chronological information is presented as calendar age BP. Confidence is defined as follows: 1. High: Sampled feature with go...
Relict subaerial landslide feature. Where information is available these are subdivided further: 1. Slide deposit; 2. Slide scar (area of missing material on failure surface; 3. Other. Where information on the genesis is available that is also provided: 1. Rotational; 2. Translational; 3. Block; 4. Rockfall; 5. Debris Flow; 6. Creep; 7. Lateral Spread; 8. Debris avalanche; 9. Other. Chronological information is presented as calendar age BP. Confidence is defined as follows: 1. High: Sampled feature with go...
Locations of relevant events delivered by National Partners and not reported on the Seismic Portal (EMSC website: https://www.seismicportal.eu/).