{
  "annotation_id": "d6b1c242-4646-495f-ac34-48bab8451272",
  "date_created": "2026-03-02T18:00:50.492000Z",
  "date_modified": "2026-03-02T18:00:50.492000Z",
  "file_hash": "1a5b2989c83f2f16bba4da1fa1fbd2f85c4ef6ab4e038f224ac4ee7951948dda",
  "private": false,
  "record": {
    "abstract": "This paper presents an analysis of the distribution of the time $\\tau$\nbetween two consecutive events in a stationary point process. The study is\nmotivated by the discovery of a unified scaling law for $\\tau$ for the case of\nseismic events. It is shown that the unified law must necessarily be\nexponential. We discuss the parameterization of the empirical unified law and\nthe physical meaning of the parameters involved.",
    "arxiv_id": "physics/0404111",
    "authors": [
      "G. Molchan"
    ],
    "categories": [
      "physics.geo-ph",
      "physics.data-an"
    ],
    "doi": "10.1007/s00024-004-2664-5",
    "title": "Interevent time distribution in seismicity: a theoretical approach",
    "url": "https://arxiv.org/abs/physics/0404111"
  },
  "schema_id": "dorsal/arxiv",
  "source": {
    "execution_id": "56f1c8ba-949f-4e6c-9512-b99944f219c1",
    "id": "arXiv Dataset IDs",
    "type": "Model",
    "variant": "snapshot-2026-03-01",
    "version": "0.1.0"
  },
  "user_id": 1000002
}