Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10656
DC FieldValueLanguage
dc.date.accessioned2017-12-20T12:09:28Zen
dc.date.available2017-12-20T12:09:28Zen
dc.date.issued2017-07en
dc.identifier.urihttp://hdl.handle.net/2122/10656en
dc.description.abstractIn this paper we reply to the criticisms advanced by Narkiewicz (2017) on the paper by Schito et al. (2017). We clarify the issues related to the stratigraphic and thermal maturity constraints used for reconstructing burial and thermal models of the two blocks of the Holy Cross Mountains. We also show how geological evidences brought by Narkiewicz (2017) as a proof of elevated Variscan heat flow are not conclusive or at least suggest the occurence of a localized thermal anomaly only along the area of the Holy Cross Fault. In the end, we performed new burial and thermal models in the Kielce region demonstrating that stratigraphic thickness variations between Schito et al. (2017) and Narkiewicz et al. (2010) produce only negligible differences in levels of thermal maturity of Paleozoic rocks. In addition, we outline that levels of thermal maturity for Silurian rocks can be matched only by using constant heat flow values through the Paleozoic and point to a decisive role for the absence of regional high Variscan heat flow in the area.en
dc.language.isoEnglishen
dc.relation.ispartofMarine and petroleum geologyen
dc.relation.ispartofseries/88(2017)en
dc.rightsCC0 1.0 Universalen
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/en
dc.subjectThermal modellingen
dc.subjectSedimentary basinsen
dc.subjectPaleozoic source rocksen
dc.subjectHoly Cross Mountainsen
dc.titleReply to Narkiewicz (2017) comment on “Thermal evolution of Paleozoic successions of the Holy Cross Mountains (Poland)”en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1114-1122en
dc.subject.INGV04.04. Geologyen
dc.subject.INGVBasin Analysesen
dc.subject.INGVThermal evolutionen
dc.identifier.doi10.1016/j.marpetgeo.2017.07.018en
dc.relation.referencesNarkiewicz, M., 2017. Comment on a paper by Schito et al. (2017) “Thermal evolution of Paleozoic successions of the Holy Cross Mountains (Poland)”. Mar.Petrol. Geol. (in press), Corrected Proof https://doi.org/10.1016/j.marpetgeo.2017.02.016en
dc.description.obiettivoSpecifico1TR. Studi per le Georisorseen
dc.description.journalTypeJCR Journalen
dc.contributor.authorSchito, Andreaen
dc.contributor.authorCorrado, S.en
dc.contributor.authorTrolese, Matteoen
dc.contributor.authorAldega, Lucaen
dc.contributor.authorCaricchi, Chiaraen
dc.contributor.authorCirilli, Simonettaen
dc.contributor.authorGrigo, D.en
dc.contributor.authorGuedes, A.en
dc.contributor.authorSpina, A.en
dc.contributor.authorValentim, B.en
dc.contributor.departmentUniversità degli Studi di Roma Tre, Dipartimento di scienzeen
dc.contributor.departmentUniversità degli Studi di Roma Tre, Dipartimento di scienzeen
dc.contributor.departmentUniversità degli Studi di Roma Tre, Dipartimento di scienzeen
dc.contributor.departmentSapienza Università di Romaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italiaen
dc.contributor.departmentUniversità degli studi di Perugia, Dipartimento di Fisica e Geologiaen
dc.contributor.departmentENI SpA, Exploration and Production Divisionen
dc.contributor.departmentInstituto de Ciencias da Terra (Polo da FCUP) e Departamento de Geocienciasen
dc.contributor.departmentUniversità degli studi di Perugia, Dipartimento di Fisica e Geologiaen
dc.contributor.departmentInstituto de Ciencias da Terra (Polo da FCUP) e Departamento de Geocienciasen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità degli studi di Roma Tre, Dipartimento di Scienze-
crisitem.author.deptUniversità degli studi di Roma Tre, Dipartimento di Scienze-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptUniversità degli Studi di Perugia, Dipartimento di Fisica e geologia-
crisitem.author.deptIstituto de Ciencias della Terra (polo da FCUP), departamento de Geociencia-
crisitem.author.deptUniversità degli studi di Perugia, Dipartimento di Fisica e Geologia-
crisitem.author.deptInstituto de Ciencias da Terra (Polo da FCUP) e Departamento de Geociencias-
crisitem.author.orcid0000-0003-0760-9321-
crisitem.author.orcid0000-0003-4356-4132-
crisitem.author.orcid0000-0001-9391-1484-
crisitem.author.orcid0000-0003-4100-7404-
crisitem.author.orcid0000-0001-6397-3713-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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