Deglacial laminated facies on the NW European continental margin: The hydrographic significance of British-Irish Ice Sheet deglaciation and Fleuve Manche paleoriver discharges-Reference-Cited by-同舟云学术

Deglacial laminated facies on the NW European continental margin: The hydrographic significance of British-Irish Ice Sheet deglaciation and Fleuve Manche paleoriver discharges

Published:2007-06 Issue:6 Volume:8 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Eynaud F.¹,Zaragosi S.¹,Scourse J. D.²,Mojtahid M.,Bourillet J. F.³,Hall I. R.⁴,Penaud A.¹,Locascio M.¹,Reijonen A.¹

Affiliation:

1. UniversitéBordeaux I; Talence; UMR 5805 EPOC, Avenue des Facultés,; F-33405; France

2. School of Ocean Sciences; University of Wales (Bangor); Menai Bridge,; LL59 5AB; Anglesey; UK

3. IFREMER; Géosciences Marines, Laboratoire Environnements Sédimentaires; BP70,; F-29280; Plouzané Cedex; France

4. School of Earth, Ocean and Planetary Sciences; Cardiff University; Park Place,; CF10 3YE; Cardiff; UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference109 articles.

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3. Geochemical and geophysical implications of the radiocarbon calibration;Bard;Geochim. Cosmochim. Acta,1998

4. Long-term variations of daily insolation and Quaternary climatic change;Berger;J. Atmos. Sci.,1978

5. Insolation values for the climate of the last 10 millions years;Berger;Quat. Sci. Rev.,1991

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