{
  "annotation_id": "926fea1d-5331-4a33-be3f-768836c94ae4",
  "date_created": "2026-03-02T18:00:50.270000Z",
  "date_modified": "2026-03-02T18:00:50.270000Z",
  "file_hash": "1d278c3523c3e30fad64af489ce1e0779b698cfeb2094c0b353ed3ed5991ee3a",
  "private": false,
  "record": {
    "abstract": "Recently it has been found by F. Freund that the granite under high pressure\nundergoes a phase transition from insulator to a p-type semiconductor. This\nphase transition is a key concept to understanding pre-earthquake phenomena.\nThis effect accompanies with the radiation of the granite in the mid-infrared\nregion. we were able to predict the recent earthquake in the south of Iran by\nmonitoring this radiation.",
    "arxiv_id": "physics/0403003",
    "authors": [
      "M. Allameh-Zadeh",
      "A. Ansari",
      "A. Bahraminasab",
      "K. Kaviani",
      "A. Mahdavi Ardakani",
      "H. Mehr-nahad",
      "D. Mehr-shahi",
      "M. D. Niry",
      "M. Reza Rahimi Tabar",
      "S. Tabatabai",
      "N. Taghavinia M. Vesaghi",
      "F. Zamani"
    ],
    "categories": [
      "physics.geo-ph",
      "physics.gen-ph"
    ],
    "title": "Mid-Infrared Radiation as a Short-Term Earthquake Precursor",
    "url": "https://arxiv.org/abs/physics/0403003"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "9a8ac64a-aea1-4725-a5b9-a6419c764b7d",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}