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  • The WMS InSpEE (INSPIRE) provides information about the areal distribution of salt structures (salt domes and salt pillows) in Northern Germany. Contours of the salt structures can be displayed at horizontal cross-sections at four different depths up to a maximum depth of 2000 m below NN. The geodata have resulted from a BMWi-funded research project “InSpEE” running from the year 2012 to 2015. The acronym stands for "Information system salt structures: planning basis, selection criteria and estimation of the potential for the construction of salt caverns for the storage of renewable energies (hydrogen and compressed air)”. Taking into account the fact that this work was undertaken at a scale for providing an overview and not for investigation of single structures, the scale of display is limited to a minimum of 1:300.000. Additionally four horizontal cross-section maps display the stratigraphical situation at a given depth. In concurrence of maps at different depths areal bedding conditions can be determined, e.g. to generally assess and interpret the spread of different stratigraphic units. Clearly visible are extent and shape of the salt structures within their regional context at the different depths, with extent and boundary of the salt structures having been the main focus of the project. Four horizontal cross-section maps covering the whole onshore area of Northern Germany have been developed at a scale of 1:500.000. The maps cover the depths of -500, -1000, -1500, -2000 m below NN. The four depths are based on typical depth requirements of existing salt caverns in Northern Germany, mainly related to hydrocarbon storage. The shapes of the structures show rudimentary information of their geometry and their change with depths. In addition they form the starting point for rock mechanical calculations necessary for the planning and construction of salt caverns for storage as well as for assessing storage potentials. The maps can be used as a pre-selection tool for subsurface uses. It can also be used to assess coverage and extension of salt structures. Offshore areas were not treated within the project. All horizontal cross-section maps were adjusted with the respective state geological survey organisations. According to the Data Specification on Geology (D2.8.II.4_v3.0) the WMS InSpEE (INSPIRE) provides INSPIRE-compliant data. The WMS InSpEE (INSPIRE) contains two group layers: The first group layer “INSPIRE: Salt structures in Northern Germany“ comprises the layers GE.Geologic.Unit.Salt structure types, GE.GeologicUnit.Salt pillow remnants, GE.GeologicUnit.Structure-building salinar and GE.GeologicUnit.Structural outlines. The layer GE.GeologicUnit.Structural outlines contains according to the four depths four sublayers, e.g. GE.GeologiUnit.Structural outlines 500 m below NN. The second group layer „INSPIRE: Horizontal cross-section maps of Northern Germany“ comprises according to the four depths four layers, e.g. Horizontal cross-section map – 500 m below NN. This layer, in turns, contains two sublayers: GE.GeologicFault.Relevant fault traces and GE.GeologicUnit.Stratigraphic Units. Via the getFeatureInfo request the user obtains additional information on the different geometries. In case of the GE.Geologic.Unit.Salt structure types the user gets access to a data sheet with additional information and further reading in German for the respective salt structure via the getFeatureInfo request.

  • InSpEE (INSPIRE) provides information about the areal distribution of salt structures (salt domes and salt pillows) in Northern Germany. Contours of the salt structures can be displayed at horizontal cross-sections at four different depths up to a maximum depth of 2000 m below NN. The geodata have resulted from a BMWi-funded research project “InSpEE” running from the year 2012 to 2015. The acronym stands for "Information system salt structures: planning basis, selection criteria and estimation of the potential for the construction of salt caverns for the storage of renewable energies (hydrogen and compressed air)”. Additionally four horizontal cross-section maps display the stratigraphical situation at a given depth. In concurrence of maps at different depths areal bedding conditions can be determined, e.g. to generally assess and interpret the spread of different stratigraphic units. Clearly visible are extent and shape of the salt structures within their regional context at the different depths, with extent and boundary of the salt structures having been the main focus of the project. Four horizontal cross-section maps covering the whole onshore area of Northern Germany have been developed at a scale of 1:500.000. The maps cover the depths of -500, -1000, -1500, -2000 m below NN. The four depths are based on typical depth requirements of existing salt caverns in Northern Germany, mainly related to hydrocarbon storage. The shapes of the structures show rudimentary information of their geometry and their change with depths. In addition they form the starting point for rock mechanical calculations necessary for the planning and construction of salt caverns for storage as well as for assessing storage potentials. The maps can be used as a pre-selection tool for subsurface uses. It can also be used to assess coverage and extension of salt structures. Offshore areas were not treated within the project. All horizontal cross-section maps were adjusted with the respective state geological survey organisations. According to the Data Specification on Geology (D2.8.II.4_v3.0) the content of InSpEE (INSPIRE) is stored in 15 INSPIRE-compliant GML files: InSpEE_GeologicUnit_Salt_structure_types.gml contains the salt structure types (salt domes and salt pillows), InSpEE_GeologicUnit_Salt_pillow_remnants.gml comprises the salt pillow remnants, InSpEE_GeologicUnit_Structure_building_salinar.gml represents the structural salinar(s), the four files InSpEE_Structural_outlines_500.gml, InSpEE_Structural_outlines_1000.gml, InSpEE_Structural_outlines_1500.gml and InSpEE_Structural_outlines_2000.gml represent the structural outlines in the corresponding horizontal cross-sections, the four files InSpEE_GeologicUnit_Cross_Section_500, InSpEE_GeologicUnit_Cross_Section_1000, InSpEE_GeologicUnit_Cross_Section_1500 and InSpEE_GeologicUnit_Cross_Section_2000 display the stratigraphical situation in the corresponding horizontal cross-sections and the four files InSpEE_GeologicStructure_500.gml, InSpEE_GeologicStructure_1000.gml, InSpEE_GeologicStructure_1500.gml and InSpEE_GeologicStructure_2000.gml comprise the relevant fault traces in the corresponding horizontal cross-sections. The GML files together with a Readme.txt file are provided in ZIP format (InSpEE-INSPIRE.zip). The Readme.text file (German/English) contains detailed information on the GML files content. Data transformation was proceeded by using the INSPIRE Solution Pack for FME according to the INSPIRE requirements.

  • Neue Karte der Salzstrukturen in Norddeutschland im Maßstab 1:500.000, einschließlich des deutschen Anteils der Nordsee (mit "Entenschnabel"). Die Karte enthält alle Salzstrukturen in diesem Gebiet, unterschieden in Salzstöcke, Salzkissen und Salzintrusionen. Die Salzstöcke zeigen den Maximalumfang und sind differenziert in solche, auf denen die Unterkreidebedeckung oder ältere Sedimente noch erhalten sind und solche, auf denen diese unter jüngeren Sedimenten fehlen. Die Salzkissen werden unterschieden in Zechsteinsalz-, Keupersalz- und Oberjurasalz-Kissen. Zusätzlich dargestellt sind: die Verbreitung der Zechstein-Diapire, die Verbreitung des Zechsteinsalinars, die Verbreitung der Rotliegendsalinar-Strukturen und die Bezeichnung der Strukturen. Vier Schnitte deuten die morphologische Vielfalt der Salzstrukturen an, eine Literaturauswahl gibt Hinweise für weitergehende Recherchen zu verschiedenen wissenschaftlichen Themen über Salzstrukturen. Die Karte basiert auf den Resultaten des in der BGR erstellten Geotektonischen Atlas, dem Geophysikalischen Kartenwerk der DDR bis 1989 sowie davon abgeleiteten Arbeiten. Weiterhin sind aktuell durch BGR erhobene Daten im Bereich der Nordsee berücksichtigt.

  • Horizontal cross-section maps display the geological situation at a given depth. In concurrence of maps at different depths areal bedding conditions can be determined, e.g. to generally assess and interpret the spread of different stratigraphic units. Clearly visible are extent and shape of the salt structures within their regional context at the different depths, with extent and boundary of the salt structures having been the main focus of the project. Four horizontal cross-section maps covering the whole onshore area of Northern Germany have been developed at a scale of 1:500.000. The maps cover the depths of -500, -1000, -1500, -2000 m below NN. The four depths were selected by the project partners and are based on typical depth requirements of existing salt caverns in Northern Germany, mainly related to hydrocarbon storage. The shapes of the structures show rudimentary information of their geometry and their change with depths. In addition they form the starting point for rock mechanical calculations necessary for the planning and construction of salt caverns for storage as well as for assessing storage potentials. The maps can be used as a pre-selection tool for subsurface uses. It can also be used to assess coverage and extension of salt structures. As, at the time of preparation of the maps, energy storage and cavern operation in offshore areas could not be assumed as a priority, such areas were not treated within the project. All horizontal cross-section maps were adjusted with the respective state geological survey organisations.

  • Der Downloaddienst (OAF) Strukturgeologische Übersicht Brandenburg stellt Daten zur Tiefengeologie und dem strukturgeologischen Bauplan Brandenburgs bereit. Diese werden dominiert durch die NW-SE streichende intrakratonale Norddeutsche Senke, deren Basis sich im nördlichen und mittleren Teil des Landesterritoriums auf über 5 000 m Tiefe absenkt und nach Süden und Südosten heraushebt. Das Beckenzentrum setzt sich von Nordwest-Brandenburg in Richtung Unterelbe fort. Dagegen ist die jetzige südliche Begrenzung tektonisch bedingt. Die strukturgeologischen Verhältnisse werden durch die jetzige Tiefenlage der Zechsteinbasis und die strukturelle Modulierung der Zechsteinoberfläche wiedergegeben. Weitere Informationen unter: https://geo.brandenburg.de/karten/htdocs/salinar.pdf. OGC API-Features ist eine Web-API zur vereinfachten Nutzung der Daten in entsprechenden Web-Entwicklungsumgebungen. Die API beinhaltet die folgenden Collections:

  • Der Darstellungsdienst (WMS) Strukturgeologische Übersicht Brandenburg stellt Daten zur Strukturgeologische Übersicht bereit. Dieser wird dominiert durch die NW-SE streichende intrakratonale Norddeutsche Senke, deren Basis sich im nördlichen und mittleren Teil des Landesterritoriums auf über 5 000 m Tiefe absenkt und nach Süden und Südosten heraushebt. Das Beckenzentrum setzt sich von Nordwest-Brandenburg in Richtung Unterelbe fort. Dagegen ist die jetzige südliche Begrenzung tektonisch bedingt. Die strukturgeologischen Verhältnisse werden durch die jetzige Tiefenlage der Zechsteinbasis und die strukturelle Modulierung der Zechsteinoberfläche wiedergegeben. Weitere Informationen unter: https://geo.brandenburg.de/karten/htdocs/salinar.pdf.

  • Der Downloaddienst (WFS) Strukturgeologische Übersicht Brandenburg stellt Daten zur Strukturgeologische Übersicht bereit. Dieser wird dominiert durch die NW-SE streichende intrakratonale Norddeutsche Senke, deren Basis sich im nördlichen und mittleren Teil des Landesterritoriums auf über 5 000 m Tiefe absenkt und nach Süden und Südosten heraushebt. Das Beckenzentrum setzt sich von Nordwest-Brandenburg in Richtung Unterelbe fort. Dagegen ist die jetzige südliche Begrenzung tektonisch bedingt. Die strukturgeologischen Verhältnisse werden durch die jetzige Tiefenlage der Zechsteinbasis und die strukturelle Modulierung der Zechsteinoberfläche wiedergegeben. Weitere Informationen unter: https://geo.brandenburg.de/karten/htdocs/salinar.pdf.

  • Horizontal cross-section maps display the geological situation at a given depth. In concurrence of maps at different depths areal bedding conditions can be determined, e.g. to generally assess and interpret the spread of different stratigraphic units. Clearly visible are extent and shape of the salt structures within their regional context at the different depths, with extent and boundary of the salt structures having been the main focus of the project. Four horizontal cross-section maps covering the whole onshore area of Northern Germany have been developed at a scale of 1:500.000. The maps cover the depths of -500, -1000, -1500, -2000 m below NN. The four depths were selected by the project partners and are based on typical depth requirements of existing salt caverns in Northern Germany, mainly related to hydrocarbon storage. The shapes of the structures show rudimentary information of their geometry and their change with depths. In addition they form the starting point for rock mechanical calculations necessary for the planning and construction of salt caverns for storage as well as for assessing storage potentials. The maps can be used as a pre-selection tool for subsurface uses. It can also be used to assess coverage and extension of salt structures. As, at the time of preparation of the maps, energy storage and cavern operation in offshore areas could not be assumed as a priority, such areas were not treated within the project. All horizontal cross-section maps were adjusted with the respective state geological survey organisations.

  • Der interoperable INSPIRE-WMS ist ein Darstellungsdienst, der Daten im Annex-Schema Geologie (abgeleitet aus dem originären Datensatz: Strukturgeologische Übersicht Brandenburg) bereitstellt. Er gibt einen Überblick zur Tiefengeologie und dem strukturgeologischen Bauplan Brandenburgs. Diese werden dominiert durch die NW-SE streichende intrakratonale Norddeutsche Senke, deren Basis sich im nördlichen und mittleren Teil des Landesterritoriums auf über 5 000 m Tiefe absenkt und nach Süden und Südosten heraushebt. Das Beckenzentrum setzt sich von Nordwest-Brandenburg in Richtung Unterelbe fort. Dagegen ist die jetzige südliche Begrenzung tektonisch bedingt. Die strukturgeologischen Verhältnisse werden durch die jetzige Tiefenlage der Zechsteinbasis und die strukturelle Modulierung der Zechsteinoberfläche wiedergegeben. Gemäß der INSPIRE-Datenspezifikation Geology (D2.8.II.4_v3.2.0) liegen die Inhalte der Karte INSPIRE-konform vor. Der WMS beinhaltet die folgenden Layer: - geologische Einheiten (GE.GeologicUnit) mit Angaben zur petrographischen Bezeichnung (GE.GeologicUnit.Lithology) und Art der geologischen Einheit (GE.GeologicUnit.geologicUnitType) - geologische Störungen (GE.GeologicFault) mit Angaben zur Verwerfungsart (faultType). --- The compliant INSPIRE-WMS Geology / Strukturgeologische Übersicht Brandenburg is a view service that delivers data in the annex schema Geology (derived from the original data set: Structural geology overview Brandenburg). It provides an overview of the deep geology and geostructural setting of Brandenburg. These are dominated by the NW-SE striking intracratonic North German depression, the base of which sinks to a depth of over 5,000 m in the northern and central part of the state territory and rises to the south and southeast. The basin center continues from northwest Brandenburg towards the Lower Elbe. In contrast, the current southern boundary is caused tectonically. The structural geological conditions are reflected by the current depth of the Zechstein base and the structural modulation of the Zechstein surface. The content of the map is compliant to the INSPIRE data specification for the annex theme Geology (D2.8.II.4_v3.2.0). The WMS includes the following layer: - geological units (GE.GeologicUnit) with information on the petrographic name (GE.GeologicUnit.Lithology) and the type of geological unit (GE.GeologicUnit.GeologicUnitType), - geological faults (GE.GeologicFault) with information on the fault type (faultType).

  • Der interoperable INSPIRE-WFS Geology / Strukturgeologische Übersicht Brandenburg ist ein Downloaddienst, der Daten im Annex-Schema Geologie (abgeleitet aus dem originären Datensatz: Strukturgeologische Übersicht Brandenburg) bereitstellt. Er gibt einen Überblick zur Tiefengeologie und dem strukturgeologischen Bauplan Brandenburgs. Diese werden dominiert durch die NW-SE streichende intrakratonale Norddeutsche Senke, deren Basis sich im nördlichen und mittleren Teil des Landesterritoriums auf über 5 000 m Tiefe absenkt und nach Süden und Südosten heraushebt. Das Beckenzentrum setzt sich von Nordwest-Brandenburg in Richtung Unterelbe fort. Dagegen ist die jetzige südliche Begrenzung tektonisch bedingt. Die strukturgeologischen Verhältnisse werden durch die jetzige Tiefenlage der Zechsteinbasis und die strukturelle Modulierung der Zechsteinoberfläche wiedergegeben. Gemäß der INSPIRE-Datenspezifikation Geology (D2.8.II.4_v3.2.0) liegen die Inhalte der Karte INSPIRE-konform vor. Der WFS beinhaltet die folgenden FeatureTypes: - Geologische Einheiten (ge:GeologicUnits) mit Angaben zur petrographischen Bezeichnung und Art der geologischen Einheit (geologicUnitType), - Verwerfungen (ge:ShearDisplacementStructure) mit Angaben zur Art der Verwerfung (faultType), - Charakteristika des kartierten Merkmals (ge:MappedFeature) und - Art der geologische Sammlung (ge:GeologicCollection). --- The compliant INSPIRE-WFS Geology / Strukturgeologische Übersicht Brandenburg is a download service that delivers data in the annex schema Geology (derived from the original data set: Structural geology overview Brandenburg). It provides an overview of the deep geology and geostructural setting of Brandenburg. These are dominated by the NW-SE striking intracratonic North German depression, the base of which sinks to a depth of over 5,000 m in the northern and central part of the state territory and rises to the south and southeast. The basin center continues from northwest Brandenburg towards the Lower Elbe. In contrast, the current southern boundary is caused tectonically. The structural geological conditions are reflected by the current depth of the Zechstein base and the structural modulation of the Zechstein surface. The content of the map is compliant to the INSPIRE data specification for the annex theme Geology (D2.8.II.4_v3.2.0). The WFS includes the following feature types: - geological features (ge:GeologicUnits) with information on the petrographic name and the type of geological unit (geologicUnitType), - shear displacement structures (ge:ShearDisplacementStructure) with information on the fault type (faultType), - characteristics of the mapped feature (ge:MappedFeature) and - type of the geological collection (ge:GeologicCollection).

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