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all geography including DSDP/ODP Sites and Legs
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Asia
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igneous rocks
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Early and middle Eocene dinoflagellate cysts from the Aktulagay section, Kazakhstan Available to Purchase
Eocene dinoflagellate cyst biostratigraphy of research borehole 011-BP, Omsk Region, southwestern Siberia Available to Purchase
WILSONIDIUM PECHORICUM NEW SPECIES—A NEW DINOFLAGELLATE SPECIES WITH UNUSUAL ASYMMETRY FROM THE PALEOCENE/EOCENE TRANSITION Available to Purchase
DINOFLAGELLATE CYSTS FROM THE MIDDLE EOCENE TO ?LOWERMOST OLIGOCENE SUCCESSION IN THE KYSING RESEARCH BOREHOLE, CENTRAL DANISH BASIN Available to Purchase
The Dababiya Quarry Section: Lithostratigraphy, clay mineralogy, geochemistry and paleontology Available to Purchase
Paleoproductivity of the northwestern Tethyan margin (Anthering section, Austria) across the Paleocene-Eocene transition Available to Purchase
Full article available in PDF version.
A paleoenvironmental reconstruction of the early late Paleocene North Sea from intrashell delta δ 18 O and delta δ 13 C profiles of mollusks Available to Purchase
Full article available in PDF version.
Chronostratigraphic terminology at the Paleocene/Eocene boundary Available to Purchase
Global dinoflagellate event associated with the late Paleocene thermal maximum Available to Purchase
The Paleocene/Eocene-boundary interval of a Tethyan deep-sea section (Austria) and its correlation with the North Sea basin Available to Purchase
Cenozoic Sequence Stratigraphy in the Eastern North Sea Available to Purchase
Abstract The Cenozoic evolution of the epicontinental North Sea Basin is described on the basis of sequence stratigraphy, comprising analyses of seismic sections, petrophysical logs and biostratigraphic studies of foraminifera, dinoflagellates and calcareous nannofossils. Stratigraphic, palaeogeographic and palaeoecological information from the Danish onshore area is integrated in the study. The deposits are subdivided into 21 sequences, which group into seven informal major units. The sequence boundaries are identified by differences in seismic facies and by seismic onlap, toplap and truncation features. The maximum flooding surfaces are placed at internal downlap surfaces which correlate with high values on the gamma-ray logs. The source of sediments and the direction of sediment transport changed several times during Cenozoic deposition. Transport was mainly from the north during the Late Paleocene and Early Eocene, from the west during the Middle and Late Eocene and from the north and northeast during the Oligocene to Quaternary times. The depocenters of the seven major units are generally located marginally, apparently adjoining the source areas. There is only minor evidence for changes in subsidence rates in the basin. A constant rate is assumed from Paleocene to mid Middle Miocene time. For the remaining part of the Cenozoic time an increased rate is indicated. A tentative relative sea-level curve for the North Sea Basin is proposed. The overall trends of the curve are broadly comparable with the global sea-level curve of Haq et al. (1988). Discrepancies may be caused by differences in the biostratigraphic calibrations. The most pronounced Oligocene sea-level fall is dated as latest Oligocene.