Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? Evidence From the Mid-Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous)-Reference-Cited by-同舟云学术

Sedimentary Mercury Enrichments as a Marker for Submarine Large Igneous Province Volcanism? Evidence From the Mid-Cenomanian Event and Oceanic Anoxic Event 2 (Late Cretaceous)

Published:2017-12 Issue:12 Volume:18 Page:4253-4275
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Scaife J. D.¹^ORCID,Ruhl M.¹^ORCID,Dickson A. J.¹²^ORCID,Mather T. A.¹^ORCID,Jenkyns H. C.¹^ORCID,Percival L. M. E.¹³,Hesselbo S. P.⁴,Cartwright J.¹,Eldrett J. S.⁵,Bergman S. C.⁶^ORCID,Minisini D.⁷

Affiliation:

1. Department of Earth Sciences; University of Oxford; Oxford UK

2. Now at Department of Earth Sciences; Royal Holloway University of London; Egham Surrey UK

3. Now at Institute of Earth Sciences, Géopolis; University of Lausanne; Lausanne Switzerland

4. Camborne School of Mines and Environment and Sustainability Institute; University of Exeter; Penryn UK

5. Shell International Exploration & Production B.V; Rijswijk GS the Netherlands

6. Now at Shell R&D Houston; Vashon WA USA

7. Shell International Exploration and Production Inc.; Houston TX USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017GC007153/fullpdf

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