Early Tertiary palaeoenvironments and sedimentation in the NE Main Porcupine Basin (well 35/13–1), offshore western Ireland?evidence for global change in the Tertiary-Reference-Cited by-同舟云学术

Early Tertiary palaeoenvironments and sedimentation in the NE Main Porcupine Basin (well 35/13–1), offshore western Ireland?evidence for global change in the Tertiary

Published:1991-06 Issue:2 Volume:3 Page:99-117
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Research

Author:

Dobson M. R.,Haynes J. R.,Bannister A. D.,Levene D. G.,Petrie H. S.,Woodbridge R. A.

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2117.1991.tb00142.x/fullpdf

Reference59 articles.

1. Foraminifera as indicators of geological events

2. Northwestern European Paleogene magnetostratigraphy, biostratigraphy, and paleogeography: Calcareous nannofossil evidence

3. A. D. Bannister (1989 ) Biostratigraphy and Palaeo-ecotogy of Late Oligocene to early Miocene Foraminifera from Shell?Agip 35j 13-1 exploration well, Porcupine Seabight Basin. Unpubl. MSc thesis, University College Wales, Aberystwyth.

4. Paleogene Tropical Planktonic Foraminiferal Biostratigraphy and Magnetobiochronology

5. Paleocene-Pleistocene benthic foraminiferal evidence of major paleoceanographic events in the eastern South Atlantic (DSDP Site 525, Walvis Ridge)

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