{"record_type":"pith_number_record","schema_url":"https://pith.science/schemas/pith-number/v1.json","pith_number":"pith:2025:QTSO5DZZTOFBXRFD3B3EGVASET","short_pith_number":"pith:QTSO5DZZ","schema_version":"1.0","canonical_sha256":"84e4ee8f399b8a1bc4a3d87643541224f432fbfce8fb26eabfb7ec32ce53369c","source":{"kind":"arxiv","id":"2501.16934","version":1},"attestation_state":"computed","paper":{"title":"A systematic search for tectonic tremor and low-frequency earthquakes in the Atacama segment of the Chilean subduction zone (24$^\\circ$S-31$^\\circ$S) turns up empty","license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","headline":"","cross_cats":[],"primary_cat":"physics.geo-ph","authors_text":"Anne Socquet, David Marsan, Jannes M\\\"unchmeyer, Sophie Giffard-Roisin, William B. Frank","submitted_at":"2025-01-28T13:27:40Z","abstract_excerpt":"Subduction megathrusts release stress not only seismically through earthquakes, but also through creep and transient slow deformation, called slow slip events (SSEs). Understanding the interplay between fast and slow slip is essential for illuminating the deformation processes on the subduction interface. The Chilean subduction margin, while one of the most seismically active regions worldwide, has few reports of SSEs. Furthermore, there are no comprehensive reports of tectonic tremors or low-frequency earthquakes (LFEs), seismic signals typically accompanying SSEs, tracking deformation at sma"},"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":"2501.16934","kind":"arxiv","version":1},"metadata":{"license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","primary_cat":"physics.geo-ph","submitted_at":"2025-01-28T13:27:40Z","cross_cats_sorted":[],"title_canon_sha256":"620fe0f77c72c4b348631ae7994c90f53a697df4802b9b9e877f7db65cadadfd","abstract_canon_sha256":"70a52415765d3f1c2afae8e9b15e67fe0bad78e75cc19d13f138fdb37b1a612f"},"schema_version":"1.0"},"receipt":{"kind":"pith_receipt","key_id":"pith-v1-2026-05","algorithm":"ed25519","signed_at":"2026-07-05T10:06:20.589305Z","signature_b64":"3O4GIWyD/VQ8fiM8p6xEhgtT0Nz4LtJeLduvjI/M8vjv0X+99a2IA6f/Cf5L0c7DjwgAn3CEiYodMqejEiK/Aw==","signed_message":"canonical_sha256_bytes","builder_version":"pith-number-builder-2026-05-17-v1","receipt_version":"0.3","canonical_sha256":"84e4ee8f399b8a1bc4a3d87643541224f432fbfce8fb26eabfb7ec32ce53369c","last_reissued_at":"2026-07-05T10:06:20.588929Z","signature_status":"signed_v1","first_computed_at":"2026-07-05T10:06:20.588929Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54"},"graph_snapshot":{"paper":{"title":"A systematic search for tectonic tremor and low-frequency earthquakes in the Atacama segment of the Chilean subduction zone (24$^\\circ$S-31$^\\circ$S) turns up empty","license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","headline":"","cross_cats":[],"primary_cat":"physics.geo-ph","authors_text":"Anne Socquet, David Marsan, Jannes M\\\"unchmeyer, Sophie Giffard-Roisin, William B. Frank","submitted_at":"2025-01-28T13:27:40Z","abstract_excerpt":"Subduction megathrusts release stress not only seismically through earthquakes, but also through creep and transient slow deformation, called slow slip events (SSEs). Understanding the interplay between fast and slow slip is essential for illuminating the deformation processes on the subduction interface. The Chilean subduction margin, while one of the most seismically active regions worldwide, has few reports of SSEs. Furthermore, there are no comprehensive reports of tectonic tremors or low-frequency earthquakes (LFEs), seismic signals typically accompanying SSEs, tracking deformation at sma"},"claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"2501.16934","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/2501.16934/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":"2501.16934","created_at":"2026-07-05T10:06:20.588985+00:00"},{"alias_kind":"arxiv_version","alias_value":"2501.16934v1","created_at":"2026-07-05T10:06:20.588985+00:00"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.2501.16934","created_at":"2026-07-05T10:06:20.588985+00:00"},{"alias_kind":"pith_short_12","alias_value":"QTSO5DZZTOFB","created_at":"2026-07-05T10:06:20.588985+00:00"},{"alias_kind":"pith_short_16","alias_value":"QTSO5DZZTOFBXRFD","created_at":"2026-07-05T10:06:20.588985+00:00"},{"alias_kind":"pith_short_8","alias_value":"QTSO5DZZ","created_at":"2026-07-05T10:06:20.588985+00:00"}],"events":[],"event_summary":{},"paper_claims":[],"inbound_citations":{"count":0,"internal_anchor_count":0,"sample":[]},"formal_canon":{"evidence_count":0,"sample":[],"anchors":[]},"links":{"html":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET","json":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET.json","graph_json":"https://pith.science/api/pith-number/QTSO5DZZTOFBXRFD3B3EGVASET/graph.json","events_json":"https://pith.science/api/pith-number/QTSO5DZZTOFBXRFD3B3EGVASET/events.json","paper":"https://pith.science/paper/QTSO5DZZ"},"agent_actions":{"view_html":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET","download_json":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET.json","view_paper":"https://pith.science/paper/QTSO5DZZ","resolve_alias":"https://pith.science/api/pith-number/resolve?arxiv=2501.16934&json=true","fetch_graph":"https://pith.science/api/pith-number/QTSO5DZZTOFBXRFD3B3EGVASET/graph.json","fetch_events":"https://pith.science/api/pith-number/QTSO5DZZTOFBXRFD3B3EGVASET/events.json","actions":{"anchor_timestamp":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET/action/timestamp_anchor","attest_storage":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET/action/storage_attestation","attest_author":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET/action/author_attestation","sign_citation":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET/action/citation_signature","submit_replication":"https://pith.science/pith/QTSO5DZZTOFBXRFD3B3EGVASET/action/replication_record"}},"created_at":"2026-07-05T10:06:20.588985+00:00","updated_at":"2026-07-05T10:06:20.588985+00:00"}