WMS Die Karten „Amplitudenanomalien“ stellen die Verbreitung von Gasindikatoren in Form von Amplitudenanomalien in seismischen Daten dar, wie z.B. bright spots, gas chimneys, seismisch transparente Zonen und velocity pull-downs. Das Untersuchungsgebiet umfasst den deutschen Nordseesektor und den Tiefenbereich der ersten 1.000 m unterhalb des Meeresbodens. Als Datengrundlagen standen verschiedenste seismische Daten zur Verfügung: ca. 30.000 km 2D-Daten und ca. 4.000 km² 3D-Daten. AmplitudenanomalienGeolDGGeologyGPDNGeologieGeopotentialamplitude anomaliesGeopotenzial Deutsche Nordsee BGR Geodatendienste Bundesanstalt für Geowissenschaften und Rohstoffe (BGR) Technischer Ansprechpartner postal

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Hannover DE-NI 30655 DE +49 511 643 - 3433 geodatenmanagement@bgr.de NONE Allgemeine Geschäftsbedingungen, siehe https://www.bgr.bund.de/AGB - General terms and conditions, see https://www.bgr.bund.de/AGB_en. Die bereitgestellten Informationen sind bei Weiterverwendung wie folgt zu zitieren: Datenquelle: BGR, LBEG und BSH, 2023 4096 4096 application/vnd.ogc.wms_xml text/xml image/bmp image/jpeg image/tiff image/png image/png8 image/png24 image/png32 image/gif image/svg+xml application/vnd.esri.wms_raw_xml application/vnd.esri.wms_featureinfo_xml application/vnd.ogc.wms_xml application/geo+json text/xml text/html text/plain application/vnd.ogc.sld+xml application/vnd.ogc.se_xml application/vnd.ogc.se_inimage application/vnd.ogc.se_blank text/xml XML https://geoportal.bgr.de/smartfindersdi-csw/api?request=GetRecordById&service=CSW&version=2.0.2&outputSchema=http://www.isotc211.org/2005/gmd&elementSetName=full&id=8a745de7-ace7-47ea-85a6-a64a240a5eb9application/vnd.ogc.csw.GetRecordByIdResponse_xmlgerger Die Karten „Amplitudenanomalien“ stellen die Verbreitung von Gasindikatoren in Form von Amplitudenanomalien in seismischen Daten dar, wie z.B. bright spots, gas chimneys, seismisch transparente Zonen und velocity pull-downs. Das Untersuchungsgebiet umfasst den deutschen Nordseesektor und den Tiefenbereich der ersten 1.000 m unterhalb des Meeresbodens. Als Datengrundlagen standen verschiedenste seismische Daten zur Verfügung: ca. 30.000 km 2D-Daten und ca. 4.000 km² 3D-Daten. 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