{"record_type":"pith_number_record","schema_url":"https://pith.science/schemas/pith-number/v1.json","pith_number":"pith:2025:GR56WGO3GEJHKDWUXVCP4DMVKR","short_pith_number":"pith:GR56WGO3","schema_version":"1.0","canonical_sha256":"347beb19db3112750ed4bd44fe0d95547ccf5ceca8c176bde7e40ced7d4f627e","source":{"kind":"arxiv","id":"2505.10414","version":1},"attestation_state":"computed","paper":{"title":"On the elementary theory of earthquake aftershocks","license":"http://creativecommons.org/licenses/by/4.0/","headline":"","cross_cats":[],"primary_cat":"physics.geo-ph","authors_text":"A.V. Guglielmi, O.D. Zotov","submitted_at":"2025-05-15T15:34:46Z","abstract_excerpt":"The elementary theory of aftershocks, being relatively simple mathematically, belongs to the basics of earthquake physics. The paper briefly outlines the concepts and ideas of the theory, provides equations for the relaxation of the source after the main shock, and emphasizes the effectiveness of the theory in the search for new approaches to the processing and analysis of aftershock observation data. The main attention is paid to the discussion of two new results obtained on the basis of elementary theory. Firstly, a two-stage relaxation mode of the earthquake source was discovered. In the fi"},"verification_status":{"content_addressed":true,"pith_receipt":true,"author_attested":false,"weak_author_claims":0,"strong_author_claims":0,"externally_anchored":false,"storage_verified":false,"citation_signatures":0,"replication_records":0,"graph_snapshot":true,"references_resolved":false,"formal_links_present":false},"canonical_record":{"source":{"id":"2505.10414","kind":"arxiv","version":1},"metadata":{"license":"http://creativecommons.org/licenses/by/4.0/","primary_cat":"physics.geo-ph","submitted_at":"2025-05-15T15:34:46Z","cross_cats_sorted":[],"title_canon_sha256":"090be5b4e9c1c89babee03916342dba44e142878b8746b126df0532615efaf1e","abstract_canon_sha256":"4b20744e2f82712a77722055226ed0c9b12f1fa8fe3acacf0241350344efbe1b"},"schema_version":"1.0"},"receipt":{"kind":"pith_receipt","key_id":"pith-v1-2026-05","algorithm":"ed25519","signed_at":"2026-07-05T11:03:38.073158Z","signature_b64":"WkLhZ2bDpsXpwjujOdMPL5xxl+tWmk95C6HMqUrWMeNc7xPXFqrQA6U2vTP9S6mG97V6/NPWD1qp9j8D2XEXDg==","signed_message":"canonical_sha256_bytes","builder_version":"pith-number-builder-2026-05-17-v1","receipt_version":"0.3","canonical_sha256":"347beb19db3112750ed4bd44fe0d95547ccf5ceca8c176bde7e40ced7d4f627e","last_reissued_at":"2026-07-05T11:03:38.072662Z","signature_status":"signed_v1","first_computed_at":"2026-07-05T11:03:38.072662Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54"},"graph_snapshot":{"paper":{"title":"On the elementary theory of earthquake aftershocks","license":"http://creativecommons.org/licenses/by/4.0/","headline":"","cross_cats":[],"primary_cat":"physics.geo-ph","authors_text":"A.V. Guglielmi, O.D. Zotov","submitted_at":"2025-05-15T15:34:46Z","abstract_excerpt":"The elementary theory of aftershocks, being relatively simple mathematically, belongs to the basics of earthquake physics. The paper briefly outlines the concepts and ideas of the theory, provides equations for the relaxation of the source after the main shock, and emphasizes the effectiveness of the theory in the search for new approaches to the processing and analysis of aftershock observation data. The main attention is paid to the discussion of two new results obtained on the basis of elementary theory. Firstly, a two-stage relaxation mode of the earthquake source was discovered. In the fi"},"claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"2505.10414","kind":"arxiv","version":1},"verdict":{"id":null,"model_set":{},"created_at":null,"strongest_claim":"","one_line_summary":"","pipeline_version":null,"weakest_assumption":"","pith_extraction_headline":""},"integrity":{"clean":true,"summary":{"advisory":0,"critical":0,"by_detector":{},"informational":0},"endpoint":"/pith/2505.10414/integrity.json","findings":[],"available":true,"detectors_run":[],"snapshot_sha256":"c28c3603d3b5d939e8dc4c7e95fa8dfce3d595e45f758748cecf8e644a296938"},"references":{"count":0,"sample":[],"resolved_work":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57","internal_anchors":0},"formal_canon":{"evidence_count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"author_claims":{"count":0,"strong_count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"builder_version":"pith-number-builder-2026-05-17-v1"},"aliases":[{"alias_kind":"arxiv","alias_value":"2505.10414","created_at":"2026-07-05T11:03:38.072720+00:00"},{"alias_kind":"arxiv_version","alias_value":"2505.10414v1","created_at":"2026-07-05T11:03:38.072720+00:00"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.2505.10414","created_at":"2026-07-05T11:03:38.072720+00:00"},{"alias_kind":"pith_short_12","alias_value":"GR56WGO3GEJH","created_at":"2026-07-05T11:03:38.072720+00:00"},{"alias_kind":"pith_short_16","alias_value":"GR56WGO3GEJHKDWU","created_at":"2026-07-05T11:03:38.072720+00:00"},{"alias_kind":"pith_short_8","alias_value":"GR56WGO3","created_at":"2026-07-05T11:03:38.072720+00:00"}],"events":[],"event_summary":{},"paper_claims":[],"inbound_citations":{"count":1,"internal_anchor_count":1,"sample":[{"citing_arxiv_id":"2509.04858","citing_title":"Relativity of Time in Earthquake Physics","ref_index":1,"is_internal_anchor":true}]},"formal_canon":{"evidence_count":0,"sample":[],"anchors":[]},"links":{"html":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR","json":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR.json","graph_json":"https://pith.science/api/pith-number/GR56WGO3GEJHKDWUXVCP4DMVKR/graph.json","events_json":"https://pith.science/api/pith-number/GR56WGO3GEJHKDWUXVCP4DMVKR/events.json","paper":"https://pith.science/paper/GR56WGO3"},"agent_actions":{"view_html":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR","download_json":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR.json","view_paper":"https://pith.science/paper/GR56WGO3","resolve_alias":"https://pith.science/api/pith-number/resolve?arxiv=2505.10414&json=true","fetch_graph":"https://pith.science/api/pith-number/GR56WGO3GEJHKDWUXVCP4DMVKR/graph.json","fetch_events":"https://pith.science/api/pith-number/GR56WGO3GEJHKDWUXVCP4DMVKR/events.json","actions":{"anchor_timestamp":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR/action/timestamp_anchor","attest_storage":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR/action/storage_attestation","attest_author":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR/action/author_attestation","sign_citation":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR/action/citation_signature","submit_replication":"https://pith.science/pith/GR56WGO3GEJHKDWUXVCP4DMVKR/action/replication_record"}},"created_at":"2026-07-05T11:03:38.072720+00:00","updated_at":"2026-07-05T11:03:38.072720+00:00"}