3 edition of Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough found in the catalog.
Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough
|Statement||by Claus Heilmann-Clausen ; with a contribution on the gottschei ammonite zone (Hauterivian) in the Adda-2 well by Tove Birkelund.|
|Series||Danmarks geologiske undersøgelse. Serie A,, nr. 17, Danmarks geologiske undersøgelse (Series)., nr. 17.|
|LC Classifications||QE774.D5 H45 1987|
|The Physical Object|
|Pagination||89 p. :|
|Number of Pages||89|
|ISBN 10||8742107490, 8742107466|
|LC Control Number||89198688|
DINOFLAGELLATE CYST STRATIGRAPHY OF THE LOWER CRETACEOUS SEQUENCE AT SITES AND , EXMOUTH PLATEAU, NORTHWEST AUSTRALIA1 Wolfram Brenner2 ABSTRACT Cores from Leg , Sites and , were sampled at intervals of one sample per m section in the Lower Cretaceous sequences. Dinoflagellate cysts and associated aquatic palynomorphs have been recovered from the dinosaur-bearing Tendaguru Beds (Upper Jurassic–Lower Cretaceous) at Tendaguru, a hill in southeast Tanzania. Palynofloras from these beds are generally dominated by pollen grains of Mesozoic conifers (mainly Classopollis), but dinoflagellate cysts occur Cited by:
Regional geothermal aquifer architecture of the fluvial Lower Cretaceous Nieuwerkerk Formation – a palynological analysis - Volume 96 Issue 4 - Cees J.L. Willems, Andrea Vondrak, Dirk K. Munsterman, Marinus E. Donselaar, Harmen F. Mijnlieff Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough. Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough. Danmarks Geologiske Undersøgelse, Serie A, Lefeld, J., Middle-Upper Jurassic and Lower Cretaceous biostratigraphy and sedimentology of the Sub-Tatric succession in the Tatra Mts (Western Carpathians). Acta Geologica Polonica,
The Sten-l, , Nora-l, Elin-l, Bo-l, and ~dda-l wells are located in the Danish part of the Central Trough. All six wells encountered Mesozoic rocks. Based on log-sequence stratigraphy, the Lower Cretaceous deposits (the Cromer Knoll Group) is subdivided into 24 log-sequences. which can be correlated between most well sections. The log sequences. Heilmann-Clausen,C. Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough: details: Late Aptian: England(Isle of Wight) Batten,D.J. et al. Palynomorphs. (In: Cretaceous. In the Isle of Wight in Mesozoic and Cenozoic stratigraphical Micropalaeontology of the Dorset coast and Isle of Wight, Southern England.
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Additional Physical Format: Online version: Heilmann-Clausen, Claus. Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough. The biostratigraphy of the Lower Cretaceous in the Danish Central Trough is based on dinoflagellates (Heilmann-Clausen, ) and calcareous nannofossiis (Thomsen, ).
The ages of the various formations and of the seismic stratigraphic units are compiled in Figure by: 6. Dinocyst biostratigraphy of the Lower Cretaceous succession of central and southeastern Spitsbergen. The Lower Cretaceous succession of Spitsbergen, Svalbard is divided into three lithostratigraphic units: the Rurikfjellet, Helvetiafjellet and Carolinefjellet formations.
A detailed log-stratigraphic study was conducted on the Lower Cretaceous Cromer Knoll Group in the Sten-1, I-1, Nora-1, Elin-1, Bo-1 and Adda-1 wells in the Danish Central Trough. Six major, 24 intermediate and a number of minor log-units Cited by: 6.
albian (lower cretaceous) dinoflagellate cyst biostratigraphy of the lower gearle siltstone, southern carnarvon basin, western australia JOHN BACKHOUSE School of Earth and Geographical Sciences, University of Western Australia, 35 Stirling Highway, Crawley, Western AustraliaAustralia, e-mail: [email protected] by: 9.
Two Danish Geological Survey boreholes in the Lower Cretaceous fine-grained Rødbjerg Member (Jydegård Formation) in the Nyker fault-block on Bornholm have yielded dinoflagellate cysts which can date the sequence as latest Ryazanian to earliest Valanginian.
Two dinoflagellate zones are identified, a. Dinoflagellate cyst biostratigraphy, palynofacies, depositional environment and sequence stratigraphy of the Agardhfjellet Formation (Upper Jurassic–Lower Cretaceous) in central Spitsbergen (Arctic Norway) Introduction Dinoflagellate cysts have proven to be an important tool for dating and correlation of Mesozoic and Cenozoic.
The Cismon drill site is located on the eastward-deepening slope between the Trento Plateau and the Belluno Basin, at an estimated palaeodepth, during the Lower Cretaceous, of – m (Erba and Larson, ).Cited by: Dinocyst biostratigraphy of the Lower Cretaceous in North Siberia Article in Stratigraphy and Geological Correlation 15(6) January with 13 Reads How we measure 'reads'.
Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough. Danmarks Geologiske UndersÝgelse, Serie A, (Albian-Cenomanian, Pieniny Klippen Belt, Carpathians): a new in sight into its foraminiferal assemblages and biostratigraphy.
Studia Geologica Polonica, Heilmann-Clausen C. Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough. Danmarks Geol.
Unders. A17, Heilmann-Clausen C. & Costa L.I. Dinoflagellate zonation of the uppermost Paleocene. to Lower Miocene in the Wursterheide Research Well, NW Germany. Geol.Jurassic-Lower Cretaceous lithostratigraphic nomenclature for the Danish Central Trough. Danmarks Geol. Undersøgelse, Serie A, 12, 65 pp.
Johannessen, P.N., Sedimentology and sequence stratigraphy of paralic and shallow marine Upper Jurassic sandstones in the northern Danish Central Graben. Additional Physical Format: Online version: Thomsen, Erik. Lower Cretaceous calcareous nannofossil biostratigraphy in the Danish Central Trough.
København: I kommission hos C.A. Reitzels forlag, The Lower Cretaceous of Bedfordshire is represented by the Aptian to Albian stages only—any earlier Lower Cretaceous stages, if they were deposited, have been subject to erosion (Eyers, ).
Earlier Lower Cretaceous units may be found to the north and to the south of this region and indicate that the area of Bedfordshire remained a relatively uplifted Cited by: 1. Heilmann-Clausen,C. Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough: details: Kimmeridgian: Volgian: North Sea: Bailey,D.A.
Selected Cribroperidinium species (Dinophyceae) from the Kimmeridgian and Volgian of Northwest Europe: details. Journals & Books; Register Sign in Sign inCited by: 2. Abstract.
This work discusses the complex characteristic of the Upper Cretaceous (Turonian-Lower Maastrichtian) section recovered by two boreholes in the southern part of the Volgograd region (right side of the Volga River) in the Gremyach’e potash by: 8.
Dinoflagellate cysts and microforaminifera of the Lower Cretaceous Yatria River section, Subarctic Ural, NW Siberia (Russia). Biostratigraphy, palaeoenvironmental and palaeogeographic discussion.
Heilmann-Clausen, C () Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough. Danmarks Geologiske Undersøgelse, Series A, 17, 1 – Helby, R () Muderongia and related dinoflagellates of the latest Jurassic to Early Cretaceous of Australasia. Abstract. The ‘Late Jurasic’ stratigraphy of the Dutch Central North Sea Graben is revised.
The sediments, ranging in age from Callovian to Ryazanian, are grouped in two lithological units: the mainly non-marine Central Graben Group (with Lower Graben Sand, Middle Graben Shale, Upper Graben Sand, Puzzle Hole, and Delfland formations) Cited by:.
Book. Full-text available. Lower Cretaceous dinoflagellate biostratigraphy in the Danish Central Trough. Danmarks Geologiske Undersøgelse Serie A, 89 p.
Jan .Central Trough. The northern part of the Danish Central Trough experienced marine inundation from the north at a time when the Sogne Basin and Feda Graben underwent major subsidence (Figure 1) (Damtoft et al., ). Dur- ing the Kimmeridgian, marine connections to the Arctic,File Size: 1MB.subsidence .
Sedimentary deposits near the head of the embayment range from Cretaceous to Quaternary in age [2–4] and in some localities are known to contain the Cretaceous-Paleogene (K-Pg) boundary interval [5–7].
Figure 1. Late Cretaceous shoreline for eastern and central regions of the United States from . ME: Mississippi by: