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dc.contributor.authorNardini, Nicholas
dc.contributor.authorMuñoz-López, Daniel
dc.contributor.authorCruset, David
dc.contributor.authorCantarero, Irene
dc.contributor.authorMartín-Martín, Juan Diego
dc.contributor.authorBenedicto, Antonio
dc.contributor.authorGomez Rivas, Enrique
dc.contributor.authorJohn, Cédric M.
dc.contributor.authorTravé, Anna
dc.date.accessioned2019-02-18T11:20:07Z
dc.date.available2019-02-18T11:20:07Z
dc.date.issued2019-02-16
dc.identifier142128215
dc.identifier089bed30-c493-4527-8e89-3ce9d82436ab
dc.identifier000460799000051
dc.identifier85062851865
dc.identifier.citationNardini , N , Muñoz-López , D , Cruset , D , Cantarero , I , Martín-Martín , J D , Benedicto , A , Gomez Rivas , E , John , C M & Travé , A 2019 , ' From early contraction to post-folding fluid evolution in the frontal part of the Bóixols thrust sheet (Southern Pyrenees) as revealed by the texture and geochemistry of calcite cements ' , Minerals , vol. 9 , no. 2 , 117 , pp. 117 . https://doi.org/10.3390/min9020117en
dc.identifier.issn2075-163X
dc.identifier.otherMendeley: bd64c71c-422c-3660-9c2d-f4f50f367610
dc.identifier.urihttp://hdl.handle.net/2164/11928
dc.descriptionFunding: This research was carried out within the framework of DGICYT Spanish Project CGL2015-66335-C2-1-R and the Grup Consolidat de Recerca “Geologia Sedimentària” (2017-SGR- 824). Acknowledgments: We thank three anonymous referees for their constructive reviews, which helped to improve the quality of the manuscript, together with the editorial guidance of Hairuo Qing. Carbon and oxygen isotopic analyses were performed at “Centre Científics I Tecnològics” of the Universitat de Barcelona. Strontium analyses were carried out at the “CAI de Geocronología y Geoquímica Isotópica (UCM-CEI)” of the Universidad Complutense de Madrid. The clumpled isotope analyses were done in the Qatar Stable isotope Laboratory of Imperial College of London. Elemental and REE composition analyses were performed at the Geochemistry Facility of labGEOTOP of the Institute of Earth Sciences Jaume Almera (ICTJA-CSIC), a cofounded structure by FEDER-UE (Ref. CSIC08-4E-001). EGR acknowledges the support of the Beatriu de Pinós programme of the Government of Catalonia’s Secretariat for Universities and Research of the Department of Economy and Knowledge (2016 BP 00208).en
dc.format.extent29
dc.format.extent18950271
dc.language.isoeng
dc.relation.ispartofMineralsen
dc.subjectSDG 14 - Life Below Wateren
dc.subjectgeochemistry of calcite cementsen
dc.subjectmeteoric and marine fluidsen
dc.subjectfracturesen
dc.subjectBóixols thrust sheeten
dc.subjectsouthern Pyreneesen
dc.subjectBoixols thrust sheeten
dc.subjectFORELAND BASINen
dc.subjectFLOWen
dc.subjectJABAL QUSAYBAH ANTICLINEen
dc.subjectCLUMPED ISOTOPEen
dc.subjectGROWTHen
dc.subjectRARE-EARTH-ELEMENTSen
dc.subjectBELT ALBANIAen
dc.subjectSYSTEMSen
dc.subjectFAULTen
dc.subjectPORE WATERSen
dc.subjectQE Geologyen
dc.subjectSupplementary Dataen
dc.subject.lccQEen
dc.titleFrom early contraction to post-folding fluid evolution in the frontal part of the Bóixols thrust sheet (Southern Pyrenees) as revealed by the texture and geochemistry of calcite cementsen
dc.typeJournal articleen
dc.contributor.institutionUniversity of Aberdeen.Centre for Energy Transitionen
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.description.statusPeer revieweden
dc.identifier.doi10.3390/min9020117
dc.identifier.urlhttp://www.mendeley.com/research/early-contraction-postfolding-fluid-evolution-frontal-part-b%C3%B3ixols-thrust-sheet-southern-pyrenees-reen


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