Unusual, basin-scale, fluid–rock interaction in the Palaeoproterozoic Onega basin from Fennoscandia : Preservation in calcite δ18O of an ancient high geothermal gradient


Autoria(s): Fallick, A.E.; Melezhik, V.A.; Brasier, A.T.; Prave, A.R.
Contribuinte(s)

University of Aberdeen, Geosciences, Geology & Petroleum Geology

Data(s)

05/08/2016

05/08/2016

01/08/2016

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

http://hdl.handle.net/2164/7111

http://dx.doi.org/10.1016/j.precamres.2016.06.001

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