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dc.rights.licenseopenen_US
hal.structure.identifierInstitut des Sciences de la Terre [ISTerre]
dc.contributor.authorTRUCHE, Laurent
hal.structure.identifierInstitut des Sciences de la Terre [ISTerre]
dc.contributor.authorDONZÉ, Frédéric-Victor
hal.structure.identifierNational Agency of Natural Resources = Agjencia Kombetare e Burimeve Natyrore [AKBN]
dc.contributor.authorGOSKOLLI, Edmond
hal.structure.identifierPolytechnic University of Tirana
dc.contributor.authorMUCEKU, Bardhyl
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorLOISY, Corinne
IDREF: 155424866
hal.structure.identifierGéosciences Environnement Toulouse [GET]
dc.contributor.authorMONNIN, Christophe
hal.structure.identifierInstitut des Sciences de la Terre [ISTerre]
dc.contributor.authorDUTOIT, Hugo
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCEREPI, Adrian
dc.date.accessioned2025-04-07T09:42:04Z
dc.date.available2025-04-07T09:42:04Z
dc.date.issued2024-02-09
dc.identifier.issn0036-8075en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/206016
dc.description.abstractEnDeep crustal production of hydrogen (H 2 ) is a potential source of primary energy if recoverable accumulations in geological formations are sufficiently large. We report direct measurements of an elevated outgassing rate of 84% (by volume) of H 2 from the deep underground Bulqizë chromite mine in Albania. A minimum of 200 tons of H 2 is vented annually from the mine’s galleries, making it one of the largest recorded H 2 flow rates to date. We cannot attribute the flux solely to the release of paleo-fluids trapped within the rocks or to present-day active and pervasive serpentinization of ultramafic rocks; rather, our results demonstrate the presence of a faulted reservoir deeply rooted in the Jurassic ophiolite massif. This discovery suggests that certain ophiolites may host economically useful accumulations of H 2 gas.
dc.description.sponsorshipSources, distribution et flux d'hydrogène (H2) et des gaz associés dans les complexes alcalins (exemple de Khibiny et Lovozero, péninsule de Kola, Russie): conséquences métallogéniques et environnementales - ANR-20-CE01-0020en_US
dc.language.isoENen_US
dc.title.enA deep reservoir for hydrogen drives intense degassing in the Bulqizë ophiolite
dc.typeArticle de revueen_US
dc.identifier.doi10.1126/science.adk9099en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalScienceen_US
bordeaux.page618-621en_US
bordeaux.volume383en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue6683en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamGEOLSEDen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-04916087
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Science&rft.date=2024-02-09&rft.volume=383&rft.issue=6683&rft.spage=618-621&rft.epage=618-621&rft.eissn=0036-8075&rft.issn=0036-8075&rft.au=TRUCHE,%20Laurent&DONZ%C3%89,%20Fr%C3%A9d%C3%A9ric-Victor&GOSKOLLI,%20Edmond&MUCEKU,%20Bardhyl&LOISY,%20Corinne&rft.genre=article


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