{"record_type":"pith_number_record","schema_url":"https://pith.science/schemas/pith-number/v1.json","pith_number":"pith:2017:INJ6DBGFY3YESKQFSP343HUX3K","short_pith_number":"pith:INJ6DBGF","schema_version":"1.0","canonical_sha256":"4353e184c5c6f0492a0593f7cd9e97da963eccc5058b92f9779daaad661dd6f5","source":{"kind":"arxiv","id":"1706.10120","version":1},"attestation_state":"computed","paper":{"title":"High spatial resolution trace element determination of geological samples by laser ablation quadrupole plasma mass spectrometry: implications for glass analysis in volcanic products","license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","headline":"","cross_cats":[],"primary_cat":"physics.geo-ph","authors_text":"Diego Perugini, Kathrin Laeger, Maurizio Petrelli","submitted_at":"2017-06-30T11:09:32Z","abstract_excerpt":"Increasing the spatial resolution of Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) is a challenge in microanalysis of geological samples. Smaller sizes for the laser beam will allow for (1) high resolution determination of trace element compositions, (2) accurate estimation of crystal/melt partition coefficients, (3) detailed characterization of diffusion profiles, and (4) analysis of fine volcanic glasses. Here, we report about the figures of merit for LA-ICP Quadrupole MS down to a spatial resolution of 5 {\\mu}m. This study highlights the possibility to achieve suit"},"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":"1706.10120","kind":"arxiv","version":1},"metadata":{"license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","primary_cat":"physics.geo-ph","submitted_at":"2017-06-30T11:09:32Z","cross_cats_sorted":[],"title_canon_sha256":"884289dc5e42fe848e45aaaada422721a1b69cae6a2fcf1e4755287e86489538","abstract_canon_sha256":"b0cdb88a422b14121cf8baa9449c27737dd2346cf6a2e8a3c0856aef053469ab"},"schema_version":"1.0"},"receipt":{"kind":"pith_receipt","key_id":"pith-v1-2026-05","algorithm":"ed25519","signed_at":"2026-05-18T00:41:09.411096Z","signature_b64":"cBjflc+19zyDBiDME9Gihd4vlX3g07ruuAak0wnlstGVTfAa28/KBTTQGPsRD99Cw6RaveNAL2P281nHjwr6DQ==","signed_message":"canonical_sha256_bytes","builder_version":"pith-number-builder-2026-05-17-v1","receipt_version":"0.3","canonical_sha256":"4353e184c5c6f0492a0593f7cd9e97da963eccc5058b92f9779daaad661dd6f5","last_reissued_at":"2026-05-18T00:41:09.410344Z","signature_status":"signed_v1","first_computed_at":"2026-05-18T00:41:09.410344Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54"},"graph_snapshot":{"paper":{"title":"High spatial resolution trace element determination of geological samples by laser ablation quadrupole plasma mass spectrometry: implications for glass analysis in volcanic products","license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","headline":"","cross_cats":[],"primary_cat":"physics.geo-ph","authors_text":"Diego Perugini, Kathrin Laeger, Maurizio Petrelli","submitted_at":"2017-06-30T11:09:32Z","abstract_excerpt":"Increasing the spatial resolution of Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) is a challenge in microanalysis of geological samples. Smaller sizes for the laser beam will allow for (1) high resolution determination of trace element compositions, (2) accurate estimation of crystal/melt partition coefficients, (3) detailed characterization of diffusion profiles, and (4) analysis of fine volcanic glasses. Here, we report about the figures of merit for LA-ICP Quadrupole MS down to a spatial resolution of 5 {\\mu}m. This study highlights the possibility to achieve suit"},"claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"1706.10120","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":""},"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":"1706.10120","created_at":"2026-05-18T00:41:09.410474+00:00"},{"alias_kind":"arxiv_version","alias_value":"1706.10120v1","created_at":"2026-05-18T00:41:09.410474+00:00"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.1706.10120","created_at":"2026-05-18T00:41:09.410474+00:00"},{"alias_kind":"pith_short_12","alias_value":"INJ6DBGFY3YE","created_at":"2026-05-18T12:31:21.493067+00:00"},{"alias_kind":"pith_short_16","alias_value":"INJ6DBGFY3YESKQF","created_at":"2026-05-18T12:31:21.493067+00:00"},{"alias_kind":"pith_short_8","alias_value":"INJ6DBGF","created_at":"2026-05-18T12:31:21.493067+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/INJ6DBGFY3YESKQFSP343HUX3K","json":"https://pith.science/pith/INJ6DBGFY3YESKQFSP343HUX3K.json","graph_json":"https://pith.science/api/pith-number/INJ6DBGFY3YESKQFSP343HUX3K/graph.json","events_json":"https://pith.science/api/pith-number/INJ6DBGFY3YESKQFSP343HUX3K/events.json","paper":"https://pith.science/paper/INJ6DBGF"},"agent_actions":{"view_html":"https://pith.science/pith/INJ6DBGFY3YESKQFSP343HUX3K","download_json":"https://pith.science/pith/INJ6DBGFY3YESKQFSP343HUX3K.json","view_paper":"https://pith.science/paper/INJ6DBGF","resolve_alias":"https://pith.science/api/pith-number/resolve?arxiv=1706.10120&json=true","fetch_graph":"https://pith.science/api/pith-number/INJ6DBGFY3YESKQFSP343HUX3K/graph.json","fetch_events":"https://pith.science/api/pith-number/INJ6DBGFY3YESKQFSP343HUX3K/events.json","actions":{"anchor_timestamp":"https://pith.science/pith/INJ6DBGFY3YESKQFSP343HUX3K/action/timestamp_anchor","attest_storage":"https://pith.science/pith/INJ6DBGFY3YESKQFSP343HUX3K/action/storage_attestation","attest_author":"https://pith.science/pith/INJ6DBGFY3YESKQFSP343HUX3K/action/author_attestation","sign_citation":"https://pith.science/pith/INJ6DBGFY3YESKQFSP343HUX3K/action/citation_signature","submit_replication":"https://pith.science/pith/INJ6DBGFY3YESKQFSP343HUX3K/action/replication_record"}},"created_at":"2026-05-18T00:41:09.410474+00:00","updated_at":"2026-05-18T00:41:09.410474+00:00"}