The Norwegian Research Council grant 191530/V30 to V.A. Melezhik fully funded the work of AEC, VAM and AL. ATB was supported by NERC grant NE/G00398X/1 to AEF and ARP. We are grateful for sample preparation and analyses to all the personnel at NGU lab. We appreciate the work on carbon and oxygen isotope analyses by Julie Dougans and Chris Taylor. Bojan Otoničar organized and helped with the CL work at the Karst Research Institute at Postojna. Arrangement of TOC, IC, and TC analyses at University of Münster is acknowledged to Harald Strauss.Peer reviewedPostprin
ABSTRACT: Diagenetic carbonate deposits (concretions, cementation bodies and cement− stone bands) co...
Authigenic carbonates from cold seeps are unique archives for studying environmental conditions, inc...
The exceptionally organic-rich rocks of the 1.98 Ga Zaonega Formation deposited in the Onega Basin,...
The ca. 2.0 Ga Zaonega Formation in the Onega Basin of NW Russia represents a deep-water, mixed sili...
This study was supported by Estonian Science Agency project PUT696 and PRG447, and Estonian Centre o...
This study was supported by Estonian Research Council project PRG447, and the Estonian Centre of Ana...
The c. 2.0 Ga Zaonega Formation of the Onega Basin (NW Russia) has been central in efforts to unders...
This paper addresses potential application of data on stable carbon and oxygen isotope composition o...
Date of Acceptance: 08/05/2015 Date of online publication: 16/05/2015 Acknowledgements Elemental and...
Samples from the Kola Superdeep Drillhole (12 262 m), a deep drillhole (1060 m), and from the surfac...
A. L. Z. acknowledges support from a Natural Environment Council Standard Grant NE/J023485/2. G.The ...
Funding: supported by the Research Council of Norway project number 269842/F50 . OH and AL are grate...
The authors acknowledge financial support from ICDP for the drilling programme. AEF, ATB and ARP tha...
The 150-m-thick Kuetsjärvi Sedimentary Formation (KSF) from the Pechenga Greenstone Belt, NW Russia,...
A variety of carbonates of different geneses, as indicated by petrography and geochemistry, are foun...
ABSTRACT: Diagenetic carbonate deposits (concretions, cementation bodies and cement− stone bands) co...
Authigenic carbonates from cold seeps are unique archives for studying environmental conditions, inc...
The exceptionally organic-rich rocks of the 1.98 Ga Zaonega Formation deposited in the Onega Basin,...
The ca. 2.0 Ga Zaonega Formation in the Onega Basin of NW Russia represents a deep-water, mixed sili...
This study was supported by Estonian Science Agency project PUT696 and PRG447, and Estonian Centre o...
This study was supported by Estonian Research Council project PRG447, and the Estonian Centre of Ana...
The c. 2.0 Ga Zaonega Formation of the Onega Basin (NW Russia) has been central in efforts to unders...
This paper addresses potential application of data on stable carbon and oxygen isotope composition o...
Date of Acceptance: 08/05/2015 Date of online publication: 16/05/2015 Acknowledgements Elemental and...
Samples from the Kola Superdeep Drillhole (12 262 m), a deep drillhole (1060 m), and from the surfac...
A. L. Z. acknowledges support from a Natural Environment Council Standard Grant NE/J023485/2. G.The ...
Funding: supported by the Research Council of Norway project number 269842/F50 . OH and AL are grate...
The authors acknowledge financial support from ICDP for the drilling programme. AEF, ATB and ARP tha...
The 150-m-thick Kuetsjärvi Sedimentary Formation (KSF) from the Pechenga Greenstone Belt, NW Russia,...
A variety of carbonates of different geneses, as indicated by petrography and geochemistry, are foun...
ABSTRACT: Diagenetic carbonate deposits (concretions, cementation bodies and cement− stone bands) co...
Authigenic carbonates from cold seeps are unique archives for studying environmental conditions, inc...
The exceptionally organic-rich rocks of the 1.98 Ga Zaonega Formation deposited in the Onega Basin,...