{
 "currentVersion": 11.4,
 "cimVersion": "3.4.0",
 "serviceDescription": "<div><div>The cause of the measured earth's magnetic field can be divided into different parts: magnetic field parts of the earth's core or mantle, magnetic field parts of the upper atmosphere and magnetic field parts of the earth's crust. The parts of the earth's crust are particularly important for applied geophysics. These magnetic field components, also known as anomalies in the earth's magnetic field, are caused by the different magnetic properties of the rocks (magnetic susceptibility, magnetic remanence), but also by anthropogenic disturbances (metal pipes, railway tracks, transformers, landfills, etc.).<br /><\/div><div><b><br /><\/b><\/div><div><b>Adresses of Services<\/b><\/div><div>ESRI-REST: https://gis.geosphere.at/maps/rest/services/geophysik/Anomalien_des_Erdmagnetfeldes/MapServer<\/div><div>WMS: https://gis.geosphere.at/maps/services/geophysik/Anomalien_des_Erdmagnetfeldes/MapServer/WMSServer<\/div><div><br /><\/div><div><b>Literature<\/b><\/div><div>Hofmann, T. (Hrsg.) &amp; Schönlaub, H. (Hrsg.) (2007): <a href='https://opac.geologie.ac.at/document/44778' target='_blank'>Geo-Atlas Österreich: Die Vielfalt des geologischen Untergrundes.<\/a> - 111, Ill., Böhlau, Wien.<\/div><\/div><div><br /><\/div><div style='font-size:1.414rem;'>Beschreibung<\/div><div><br /><\/div>Das gemessene Erdmagnetfeld kann in seiner Ursache in verschiedene Anteile aufgeteilt werden: Magnetfeldanteile des Erdkerns bzw. Erdmantels, Magnetfeldanteile der oberen Atmosphäre und Magnetfeldanteile der Erdkruste. Für die angewandte Geophysik sind vor allem die Anteile der Erdkruste von Bedeutung. Diese Magnetfeldanteile, auch als Anomalien des Erdmagnetfeldes bezeichnet, werden hervorgerufen durch die unterschiedlichen magnetischen Eigenschaften der Gesteine (magnetische Suszeptibilität, magnetische Remanenz), aber auch durch anthropogene Störungen (Metallrohre, Eisenbahnschienen, Transformatoren, Deponien usw.).<div><br /><\/div><div><b>Adressen der Services<\/b><\/div><div>ESRI-REST: https://gis.geosphere.at/maps/rest/services/geophysik/Anomalien_des_Erdmagnetfeldes/MapServer<\/div><div>WMS: https://gis.geosphere.at/maps/services/geophysik/Anomalien_des_Erdmagnetfeldes/MapServer/WMSServer<\/div><div><br /><\/div><div><b>Literatur<\/b><\/div><div>Hofmann, T. (Hrsg.) &amp; Schönlaub, H. (Hrsg.) (2007): <a href='https://opac.geologie.ac.at/document/44778' target='_blank'>Geo-Atlas Österreich: Die Vielfalt des geologischen Untergrundes.<\/a> - 111, Ill., Böhlau, Wien.<br /><\/div>",
 "mapName": "anomalien_erdmagnetfeld",
 "description": "The cause of the measured earth's magnetic field can be divided into different parts: magnetic field parts of the earth's core or mantle, magnetic field parts of the upper atmosphere and magnetic field parts of the earth's crust. The parts of the earth's crust are particularly important for applied geophysics. These magnetic field components, also known as anomalies in the earth's magnetic field, are caused by the different magnetic properties of the rocks (magnetic susceptibility, magnetic remanence), but also by anthropogenic disturbances (metal pipes, railway tracks, transformers, landfills, etc.).Adresses of ServicesESRI-REST: https://gis.geosphere.at/maps/rest/services/geophysik/Anomalien_des_Erdmagnetfeldes/MapServerWMS: https://gis.geosphere.at/maps/services/geophysik/Anomalien_des_Erdmagnetfeldes/MapServer/WMSServerLiteratureHofmann, T. (Hrsg.) &amp; Schönlaub, H. (Hrsg.) (2007): Geo-Atlas Österreich: Die Vielfalt des geologischen Untergrundes. - 111, Ill., Böhlau, Wien.BeschreibungDas gemessene Erdmagnetfeld kann in seiner Ursache in verschiedene Anteile aufgeteilt werden: Magnetfeldanteile des Erdkerns bzw. Erdmantels, Magnetfeldanteile der oberen Atmosphäre und Magnetfeldanteile der Erdkruste. Für die angewandte Geophysik sind vor allem die Anteile der Erdkruste von Bedeutung. Diese Magnetfeldanteile, auch als Anomalien des Erdmagnetfeldes bezeichnet, werden hervorgerufen durch die unterschiedlichen magnetischen Eigenschaften der Gesteine (magnetische Suszeptibilität, magnetische Remanenz), aber auch durch anthropogene Störungen (Metallrohre, Eisenbahnschienen, Transformatoren, Deponien usw.).Adressen der ServicesESRI-REST: https://gis.geosphere.at/maps/rest/services/geophysik/Anomalien_des_Erdmagnetfeldes/MapServerWMS: https://gis.geosphere.at/maps/services/geophysik/Anomalien_des_Erdmagnetfeldes/MapServer/WMSServerLiteraturHofmann, T. (Hrsg.) &amp; Schönlaub, H. (Hrsg.) (2007): Geo-Atlas Österreich: Die Vielfalt des geologischen Untergrundes. - 111, Ill., Böhlau, Wien.",
 "copyrightText": "GeoSphere Austria",
 "supportsDynamicLayers": true,
 "layers": [
  {
   "id": 0,
   "name": "Anomalie Magnetfeld Isolinien",
   "parentLayerId": -1,
   "defaultVisibility": true,
   "subLayerIds": null,
   "minScale": 0,
   "maxScale": 0,
   "type": "Feature Layer",
   "geometryType": "esriGeometryPolyline",
   "supportsDynamicLegends": true
  },
  {
   "id": 1,
   "name": "Anomalie Magnetfeld 4000m polreduziert, in Nanotesla (nT)",
   "parentLayerId": -1,
   "defaultVisibility": true,
   "subLayerIds": null,
   "minScale": 0,
   "maxScale": 0,
   "type": "Raster Layer",
   "supportsDynamicLegends": true
  }
 ],
 "tables": [],
 "spatialReference": {
  "wkid": 102100,
  "latestWkid": 3857,
  "xyTolerance": 0.001,
  "zTolerance": 0.001,
  "mTolerance": 0.001,
  "falseX": -20037700,
  "falseY": -30241100,
  "xyUnits": 1.4892314192838538E8,
  "falseZ": -100000,
  "zUnits": 10000,
  "falseM": -100000,
  "mUnits": 10000
 },
 "singleFusedMapCache": false,
 "initialExtent": {
  "xmin": 1032083.433230756,
  "ymin": 5620205.058320924,
  "xmax": 1966644.9799406375,
  "ymax": 6371831.1533344025,
  "spatialReference": {
   "wkid": 102100,
   "latestWkid": 3857,
   "xyTolerance": 0.001,
   "zTolerance": 0.001,
   "mTolerance": 0.001,
   "falseX": -20037700,
   "falseY": -30241100,
   "xyUnits": 1.4892314192838538E8,
   "falseZ": -100000,
   "zUnits": 10000,
   "falseM": -100000,
   "mUnits": 10000
  }
 },
 "fullExtent": {
  "xmin": 1041079.6145180926,
  "ymin": 5828619.773437152,
  "xmax": 1919079.6145180925,
  "ymax": 6281619.773437152,
  "spatialReference": {
   "wkid": 102100,
   "latestWkid": 3857,
   "xyTolerance": 0.001,
   "zTolerance": 0.001,
   "mTolerance": 0.001,
   "falseX": -20037700,
   "falseY": -30241100,
   "xyUnits": 1.4892314192838538E8,
   "falseZ": -100000,
   "zUnits": 10000,
   "falseM": -100000,
   "mUnits": 10000
  }
 },
 "datesInUnknownTimezone": false,
 "minScale": 0,
 "maxScale": 0,
 "units": "esriMeters",
 "supportedImageFormatTypes": "PNG32,PNG24,PNG,JPG,DIB,TIFF,EMF,PS,PDF,GIF,SVG,SVGZ,BMP",
 "documentInfo": {
  "Title": "Geophysik - Magnetik",
  "Author": "",
  "Comments": "",
  "Subject": "",
  "Category": "",
  "Version": "3.2.0",
  "AntialiasingMode": "Fast",
  "TextAntialiasingMode": "Force",
  "Keywords": "Geophysik,Magnetik"
 },
 "supportsQueryDomains": true,
 "capabilities": "Map,Query,Data",
 "supportedQueryFormats": "JSON, geoJSON, PBF",
 "exportTilesAllowed": false,
 "referenceScale": 0.0,
 "datumTransformations": [
  {
   "geoTransforms": [
    {
     "wkid": 1757,
     "latestWkid": 3895,
     "transformForward": false,
     "name": "MGI_Ferro_To_MGI"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 1757,
     "latestWkid": 3895,
     "transformForward": true,
     "name": "MGI_Ferro_To_MGI"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 1618,
     "latestWkid": 1618,
     "transformForward": true,
     "name": "MGI_To_WGS_1984_3"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 1618,
     "latestWkid": 1618,
     "transformForward": false,
     "name": "MGI_To_WGS_1984_3"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 8263,
     "latestWkid": 108094,
     "transformForward": false,
     "name": "MGI_Ferro_To_WGS_1984"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 8263,
     "latestWkid": 108094,
     "transformForward": true,
     "name": "MGI_Ferro_To_WGS_1984"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 1619,
     "latestWkid": 1619,
     "transformForward": true,
     "name": "MGI_To_ETRS_1989_1"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 1619,
     "latestWkid": 1619,
     "transformForward": false,
     "name": "MGI_To_ETRS_1989_1"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 1149,
     "latestWkid": 1149,
     "transformForward": true,
     "name": "ETRS_1989_To_WGS_1984"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 1149,
     "latestWkid": 1149,
     "transformForward": false,
     "name": "ETRS_1989_To_WGS_1984"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 1149,
     "latestWkid": 1149,
     "transformForward": true,
     "name": "ETRS_1989_To_WGS_1984"
    },
    {
     "wkid": 3966,
     "latestWkid": 3966,
     "transformForward": false,
     "name": "MGI_Ferro_To_WGS_1984_1"
    }
   ]
  },
  {
   "geoTransforms": [
    {
     "wkid": 3966,
     "latestWkid": 3966,
     "transformForward": true,
     "name": "MGI_Ferro_To_WGS_1984_1"
    },
    {
     "wkid": 1149,
     "latestWkid": 1149,
     "transformForward": false,
     "name": "ETRS_1989_To_WGS_1984"
    }
   ]
  }
 ],
 "supportsDatumTransformation": true,
 "archivingInfo": {"supportsHistoricMoment": false},
 "supportsClipping": true,
 "supportsSpatialFilter": true,
 "supportsTimeRelation": true,
 "supportsQueryDataElements": true,
 "mapUnits": {"uwkid": 9001},
 "maxSelectionCount": 2000,
 "maxRecordCount": 2000,
 "maxImageHeight": 4096,
 "maxImageWidth": 4096,
 "supportedExtensions": "WMSServer",
 "serviceItemId": "45fca31daba741e7ba5c1ce0d8add71f"
}