date: 2020-06-11T05:38:29Z pdf:PDFVersion: 1.6 pdf:docinfo:title: Cooling rates of pyroclastic deposits inferred from mineral magnetic investigations: a case study from the Pleistocene Mętina Maar (Czech Republic) xmp:CreatorTool: Springer access_permission:can_print_degraded: true subject: International Journal of Earth Sciences, https://doi.org/10.1007/s00531-020-01865-1 pdfa:PDFVersion: A-2b xmpMM:History:Action: converted dc:format: application/pdf; version=1.6 pdf:docinfo:custom:robots: noindex pdf:docinfo:creator_tool: Springer access_permission:fill_in_form: true xmpMM:History:When: 2020-06-11T11:04:33Z pdf:encrypted: false dc:title: Cooling rates of pyroclastic deposits inferred from mineral magnetic investigations: a case study from the Pleistocene Mętina Maar (Czech Republic) modified: 2020-06-11T05:38:29Z cp:subject: International Journal of Earth Sciences, https://doi.org/10.1007/s00531-020-01865-1 xmpMM:History:SoftwareAgent: pdfToolbox pdf:docinfo:custom:CrossMarkDomains[1]: springer.com robots: noindex pdf:docinfo:subject: International Journal of Earth Sciences, https://doi.org/10.1007/s00531-020-01865-1 xmpMM:History:InstanceID: uuid:91078ada-ee3e-4a34-9d28-52cd72b581a4 pdf:docinfo:creator: Philipp Lied meta:author: Agnes Kontny meta:creation-date: 2020-05-12T23:01:51Z pdf:docinfo:custom:CrossmarkMajorVersionDate: 2010-04-23 created: Wed May 13 01:01:51 CEST 2020 access_permission:extract_for_accessibility: true Creation-Date: 2020-05-12T23:01:51Z pdfaid:part: 2 pdf:docinfo:custom:CrossMarkDomains[2]: springerlink.com pdf:docinfo:custom:doi: 10.1007/s00531-020-01865-1 pdf:docinfo:custom:CrossmarkDomainExclusive: true Author: Agnes Kontny producer: Acrobat Distiller 10.1.8 (Windows) CrossmarkDomainExclusive: true pdf:docinfo:producer: Acrobat Distiller 10.1.8 (Windows) doi: 10.1007/s00531-020-01865-1 dc:description: International Journal of Earth Sciences, https://doi.org/10.1007/s00531-020-01865-1 Keywords: Eger rift system,Maar-diatreme volcano,Titanomagnetite,Curie temperature,Cation ordering effect,Maghemitization,Pyroclastic emplacement mechanism access_permission:modify_annotations: true dc:creator: Agnes Kontny description: International Journal of Earth Sciences, https://doi.org/10.1007/s00531-020-01865-1 dcterms:created: 2020-05-12T23:01:51Z Last-Modified: 2020-06-11T05:38:29Z dcterms:modified: 2020-06-11T05:38:29Z title: Cooling rates of pyroclastic deposits inferred from mineral magnetic investigations: a case study from the Pleistocene Mętina Maar (Czech Republic) xmpMM:DocumentID: uuid:4c0ac6dd-dfec-4e4f-9cce-7838f005ad2b Last-Save-Date: 2020-06-11T05:38:29Z CrossMarkDomains[1]: springer.com pdf:docinfo:keywords: Eger rift system,Maar-diatreme volcano,Titanomagnetite,Curie temperature,Cation ordering effect,Maghemitization,Pyroclastic emplacement mechanism pdf:docinfo:modified: 2020-06-11T05:38:29Z meta:save-date: 2020-06-11T05:38:29Z Content-Type: application/pdf X-Parsed-By: org.apache.tika.parser.DefaultParser creator: Agnes Kontny pdfaid:conformance: B dc:subject: Eger rift system,Maar-diatreme volcano,Titanomagnetite,Curie temperature,Cation ordering effect,Maghemitization,Pyroclastic emplacement mechanism access_permission:assemble_document: true xmpTPg:NPages: 19 access_permission:extract_content: true access_permission:can_print: true CrossMarkDomains[2]: springerlink.com meta:keyword: Eger rift system,Maar-diatreme volcano,Titanomagnetite,Curie temperature,Cation ordering effect,Maghemitization,Pyroclastic emplacement mechanism access_permission:can_modify: true pdf:docinfo:created: 2020-05-12T23:01:51Z CrossmarkMajorVersionDate: 2010-04-23