Obliquity-dominated glacio-eustatic sea level change in the early Oligocene: evidence from the shallow marine siliciclastic Rupelian stratotype (Boom Formation, Belgium)-Reference-Cited by-同舟云学术

Obliquity-dominated glacio-eustatic sea level change in the early Oligocene: evidence from the shallow marine siliciclastic Rupelian stratotype (Boom Formation, Belgium)

Published:2007-02 Issue:1 Volume:19 Page:65-73
ISSN:0954-4879
Container-title:Terra Nova
language:en
Short-container-title:Terra Nova

Author:

Abels Hemmo A.,Simaeys Stefaan Van,Hilgen Frits J.,Man Ellen De,Vandenberghe Noël

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-3121.2006.00716.x/fullpdf

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1. Long-period orbital control on middle Miocene global cooling: Integrated stratigraphy and astronomical tuning of the Blue Clay Formation on Malta

2. A new Geologic Time Scale, with special reference to Precambrian and Neogene

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