{
  "annotation_id": "00b181d3-d717-45bf-9220-550e59bf0464",
  "date_created": "2026-03-02T18:00:49.860000Z",
  "date_modified": "2026-03-02T18:00:49.860000Z",
  "file_hash": "0b30c391ae259a0b78873ee0f7212abf89fd6b4f1058622b54d5a40aa6210214",
  "private": false,
  "record": {
    "abstract": "The local when earthquake prediction is based on the connection between\ngeomagnetic quakes and the next incoming minimum or maximum of tidal\ngravitational potential. The probability time window for the predicted\nearthquake is for the tidal minimum approximately +/-1 day and for the maximum-\n+/-2 days. The preliminary statistic estimation on the basis of distribution of\nthe time difference between occurred and predicted earthquakes for the period\n2002- 2003 for Sofia region is given. The possibility for creating a local\nwhen, where earthquake research and prediction NETWORK is based on the accurate\nmonitoring of the electromagnetic field with special space and time scales\nunder, on and over the Earth surface. The periodically upgraded information\nfrom seismic hazard maps and other standard geodetic information as well as\nother precursory information is essential.",
    "arxiv_id": "physics/0402112",
    "authors": [
      "S. Cht. Mavrodiev"
    ],
    "categories": [
      "physics.geo-ph",
      "physics.ao-ph"
    ],
    "doi": "10.5194/nhess-4-433-2004",
    "title": "On the Reliability of the Geomagnetic Quake as Short Time Earthquake   Precursor for Sofia Region- 2002, 2003",
    "url": "https://arxiv.org/abs/physics/0402112"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "9542f164-8945-49e6-ba3c-deb4ad53a03c",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}