Metadata 1798
Relict estuary landform defined as a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it and a free connect to the open sea/ocean. Where know the type of estuary (e.g. fjord, estuary, ria) is included. Chronological information is presented as calendar age BP. Confidence is defined as follows: 1. High: Sampled feature with good age and palaeoenvironmental control. 2. Sampled feature with poor or none age and palaeoenvironmental control. 3. Constructed by rem...
Gyula Maros, Zoltán Püspöki, László Bereczki, Gábor Markos 2015:
In this model, we integrated the interpreted data set of the SAL-X 2D seismic section system, which explores the Nógrád coal basins, including the Zagyva and Etes Grabens, into a 3D model space. The section system delineates the distribution of the near-surface Oligocene formations.
Dataset for classification of rare earth element (REE) deposits in Europe.
Harmonized geo-energy, mineral resource and area management data coming from various countries based on key economic and geological parameters
Harmonized geo-energy, mineral resource and area management data coming from various countries based on key economic and geological parameters
Point map displaying ornamental stone reources in Europe
Spatial distribution of occurrences of Co in European land and sea and respective genetic types.
Spatial distribution of occurrences of Phosphor in European land and sea and respective genetic types.
Within the European wide EUOGA project 82 hydrocarbon bearing shale formations within 21 countries were assessed for their unconventional resource potential. A stochastic volumetric assessment could be carried out for 49 formations, 15 of which are concluded to hold both shale gas and shale oil, 26 only gas and 8 only oil. The total resource estimation for all assessed shale formations in all countries combined amounts to 89.23 tcm of gas and 31.4 billion barrels of oil in place.
Iso-content maps of Europium (Eu), one of the chemical elements.obtained in the Geochemical Atlas of Spain Project, distributed in stream sediments (14,864 samples), superficial soils (0-20 cm.) (13,505 samples) and deeper soils (20-40 cm.) (7,682 samples). The results of the chemical analysis are shown in two types: total dissolution of the sample with 4 acids and partial dissolution with aqua regia. With the analytical results of all the sampled points, an isocontent map is made with adjustment to a squa...
