Unusual, basin-scale, fluid–rock interaction in the Palaeoproterozoic Onega basin from Fennoscandia : Preservation in calcite δ18O of an ancient high geothermal gradient
Contribuinte(s) |
University of Aberdeen, Geosciences, Geology & Petroleum Geology |
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Data(s) |
05/08/2016
05/08/2016
01/08/2016
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Resumo |
Acknowledgements We acknowledge financial support from ICDP for the drilling programme. AEF, ATB and ARP thank NERC for financial support through NE/G00398X/1. VAM thanks the Norwegian Research Council for financial support through 191530/V30. We are grateful for sample preparation and analyses to all the personnel at NGU lab. At SUERC we enjoyed exceptional analytical support from Julie Dougans. Anonymous reviewers and the editor provided comments that improved the final manuscript. Peer reviewed Postprint |
Formato |
12 |
Identificador |
Fallick , A E , Melezhik , V A , Brasier , A T & Prave , A R 2016 , ' Unusual, basin-scale, fluid–rock interaction in the Palaeoproterozoic Onega basin from Fennoscandia : Preservation in calcite δ18O of an ancient high geothermal gradient ' Precambrian Research , vol 281 , pp. 224-235 . , 10.1016/j.precamres.2016.06.001 0301-9268 PURE: 67964215 PURE UUID: 7690b0a5-1e27-4368-8517-754341a8b287 |
Idioma(s) |
eng |
Relação |
Precambrian Research |
Direitos |
© 2016. This manuscript version is made available under the CC-BY 4.0 license http://creativecommons.org/licenses/by/4.0/ |
Palavras-Chave | #palaeoproterozoic #Zaonega Formation #geothermal gradient #oxygen isotope #carbonate diagenesis #QE Geology #Natural Environment Research Council (NERC) #NE/G00398X/1 #QE |
Tipo |
Journal article |