{"state_type":"pith_open_graph_state","state_version":"1.0","pith_number":"pith:2025:4A2GAT7EQBI3O7YX5374TVKMDB","merge_version":"pith-open-graph-merge-v1","event_count":2,"valid_event_count":2,"invalid_event_count":0,"equivocation_count":0,"current":{"canonical_record":{"metadata":{"abstract_canon_sha256":"51f5faf3267de32097ab9dd6fe0e9e59f82ee9db9a9ba2fbe03f90cc817eb84d","cross_cats_sorted":[],"license":"http://creativecommons.org/licenses/by/4.0/","primary_cat":"physics.geo-ph","submitted_at":"2025-06-02T11:38:59Z","title_canon_sha256":"e8a47a0907c18b6b0e6402cf381e7957756acae8215b0c38de8251636af2a6a4"},"schema_version":"1.0","source":{"id":"2506.04257","kind":"arxiv","version":2}},"source_aliases":[{"alias_kind":"arxiv","alias_value":"2506.04257","created_at":"2026-07-05T11:21:48Z"},{"alias_kind":"arxiv_version","alias_value":"2506.04257v2","created_at":"2026-07-05T11:21:48Z"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.2506.04257","created_at":"2026-07-05T11:21:48Z"},{"alias_kind":"pith_short_12","alias_value":"4A2GAT7EQBI3","created_at":"2026-07-05T11:21:48Z"},{"alias_kind":"pith_short_16","alias_value":"4A2GAT7EQBI3O7YX","created_at":"2026-07-05T11:21:48Z"},{"alias_kind":"pith_short_8","alias_value":"4A2GAT7E","created_at":"2026-07-05T11:21:48Z"}],"graph_snapshots":[{"event_id":"sha256:0fbb26943cc6a9da2852577ffe7ad1d9252d96d0a793f57aa5e3ff1a256d7eb7","target":"graph","created_at":"2026-07-05T11:21:48Z","signer":{"key_id":"pith-v1-2026-05","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54","signer_id":"pith.science","signer_type":"pith_registry"},"payload":{"graph_snapshot":{"author_claims":{"count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57","strong_count":0},"builder_version":"pith-number-builder-2026-05-17-v1","claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"formal_canon":{"evidence_count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"integrity":{"available":true,"clean":true,"detectors_run":[],"endpoint":"/pith/2506.04257/integrity.json","findings":[],"snapshot_sha256":"c28c3603d3b5d939e8dc4c7e95fa8dfce3d595e45f758748cecf8e644a296938","summary":{"advisory":0,"by_detector":{},"critical":0,"informational":0}},"paper":{"abstract_excerpt":"In earthquake-prone regions, the accumulation of geophysical stress during the aseismic period plays a critical role in determining which faults are more likely to be reactivated in future seismic events. In this model, we consider an infinite non-planar fault located in a viscoelastic half-space of a fractional Maxwell medium representing the lithosphere-asthenosphere system comprising three interconnected planar sections. The problem is formulated as a two-dimensional boundary value problem with discontinuities along the fault surface. A numerical solution is obtained using a Laplace transfo","authors_text":"Pabita Mahato, Seema Sarkar (Mondal), Subhash Chandra (Mondal)","cross_cats":[],"headline":"","license":"http://creativecommons.org/licenses/by/4.0/","primary_cat":"physics.geo-ph","submitted_at":"2025-06-02T11:38:59Z","title":"Deformation Due to Non-planar Fault Movement in Fractional Maxwell Medium"},"references":{"count":0,"internal_anchors":0,"resolved_work":0,"sample":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"2506.04257","kind":"arxiv","version":2},"verdict":{"created_at":null,"id":null,"model_set":{},"one_line_summary":"","pipeline_version":null,"pith_extraction_headline":"","strongest_claim":"","weakest_assumption":""}},"verdict_id":null}}],"author_attestations":[],"timestamp_anchors":[],"storage_attestations":[],"citation_signatures":[],"replication_records":[],"corrections":[],"mirror_hints":[],"record_created":{"event_id":"sha256:a8e7c143056dccd67dfcc62205ac6e79f3ace27236dbde3824e5b9d942b8ad0b","target":"record","created_at":"2026-07-05T11:21:48Z","signer":{"key_id":"pith-v1-2026-05","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54","signer_id":"pith.science","signer_type":"pith_registry"},"payload":{"attestation_state":"computed","canonical_record":{"metadata":{"abstract_canon_sha256":"51f5faf3267de32097ab9dd6fe0e9e59f82ee9db9a9ba2fbe03f90cc817eb84d","cross_cats_sorted":[],"license":"http://creativecommons.org/licenses/by/4.0/","primary_cat":"physics.geo-ph","submitted_at":"2025-06-02T11:38:59Z","title_canon_sha256":"e8a47a0907c18b6b0e6402cf381e7957756acae8215b0c38de8251636af2a6a4"},"schema_version":"1.0","source":{"id":"2506.04257","kind":"arxiv","version":2}},"canonical_sha256":"e034604fe48051b77f17eeffc9d54c184fd0a077b3ab9a956d6c612231c7357d","receipt":{"algorithm":"ed25519","builder_version":"pith-number-builder-2026-05-17-v1","canonical_sha256":"e034604fe48051b77f17eeffc9d54c184fd0a077b3ab9a956d6c612231c7357d","first_computed_at":"2026-07-05T11:21:48.130508Z","key_id":"pith-v1-2026-05","kind":"pith_receipt","last_reissued_at":"2026-07-05T11:21:48.130508Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54","receipt_version":"0.3","signature_b64":"21TRJAIUUsMDldAs2LcCdBjg2VzO01zijKVLi80ov6clY3DfneN2oR+dbywFa1hGjD9WGykKA586Wh+P1W8PCA==","signature_status":"signed_v1","signed_at":"2026-07-05T11:21:48.131056Z","signed_message":"canonical_sha256_bytes"},"source_id":"2506.04257","source_kind":"arxiv","source_version":2}}},"equivocations":[],"invalid_events":[],"applied_event_ids":["sha256:a8e7c143056dccd67dfcc62205ac6e79f3ace27236dbde3824e5b9d942b8ad0b","sha256:0fbb26943cc6a9da2852577ffe7ad1d9252d96d0a793f57aa5e3ff1a256d7eb7"],"state_sha256":"df70dde3efa360c798005f2a8f61ad8d75d5e01c8de3ec1db3f45753dbd7e904"}