Results 111 to 120 of about 178 (157)

Application of morphological lineages in Australian palynostratigraphy

Review of Palaeobotany and Palynology, 1990
Abstract In terms of biostratigraphic subdivision dorected towards chronostratigraphic correlation, the lineage zone is of major significance. With the application of palynostratigraphy to time correlation however, morphological lineages are little used.
P.L. Price, J. Filatoff
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Palaeogene palynostratigraphy of Simla Hills

Journal of Palaeosciences, 1981
The Palaeogene succession of Simla Hills consists of Subathu, Dagshai and Kasauli formations in ascending order of stratigraphy. The palynostratigraphical information developed from the marine sequence of Subathu sediments throws light on the dating potential of the assemblages and also on the distributional pattern of various palynomorphs.
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Palynostratigraphy in Phanerozoic and Precambrian Metamorphic Rocks

1992
A review is presented on the current state of palynological research in metamorphic rocks. Recent studies have shown that organic-walled microfossils may be structurally preserved in rocks of the greenschist facies and even those of the lower amphibolite facies from where they can be separated by a special maceration procedure.
H. D. Pflug, E. Reitz
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Lower Jurassic palynostratigraphy of Eastern Siberia

Stratigraphy and Geological Correlation, 2017
This paper presents the results of a palynological study of the natural outcrops of the Lower and Middle Jurassic on the Kelimyar River (Outcrops 5, 6, 7, 14, and 16) and two boreholes, Middle-Nakynskaya and Ygyata-Tyungskaya 1, in Eastern Siberia. The Ukugut, Tyung, Motorchuna, Suntar, Kyrin, and Kelimyar formations were studied.
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Lower Toarcian palynostratigraphy of Pozzale, central Italy

Palynology, 1997
Abstract Palynological studies of the Lower Toarcian Pozzale section of central Italy (Tethyan Realm, Mediterranean province) have revealed significant differences between palynomorph assemblages from the Boreal and Tethyan realms and marked similarities between the two bioprovinces of the Tethyan Realm (Mediterranean and Sub‐Mediterranean).
Raffaella Bucefalo Palliani, James B. Riding   +1 more
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Palynostratigraphie des Buntsandsteins in Mitteleuropa

1988
[…] Die Arbeit stellt die Möglichkeiten der palynostratigraphischen Gliederung des Buntsandsteins im Germanischen Becken dar. Charakteristische Sporenzonen ermöglichen eine Unterteilung des Unteren, Mittleren und Oberen Buntsandsteins sowie eine Korrelation mit der alpinen Trias.
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Palynostratigraphy of the Stroud-Gloucester Trough, N.S.W.

Alcheringa: An Australasian Journal of Palaeontology, 1987
An investigation of spore-pollen assemblages from the Permian succession of the Stroud-Gloucester Trough, N.S.W., establishes that sedimentation began at the top of palynological zone Upper Stage 4 in the Dewrang Group. Deposition continued, without major break, through to the Gloucester Coal Measures, which are of lower Upper Stage 5 age.
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Palynostratigraphy, Imperial Adgo F-28

1977
The biostratigraphy on Imperial Adgo F-28 consists of palynostratigraphy and zonation by Dr. Geoffrey Norris and a micropaleontological analysis by Dr. W. Braun. One hundred and six micropaleontological slides and 77 micropaleontological preparations from well cuttings provided by the Geological Survey of Canada were examined in detail.
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Jurassic Palynostratigraphy of Offshore Eastern Canada

1977
Abstract The Scotian Shelf and Grand Banks, offshore southeastern Canada, cover approximately 175,000 square miles and extend over 850 miles from northeast to southwest. More than 100 exploratory wells drilled to date have encountered Lower Paleozoic to Recent sediments, which frequently contain rich and age diagnostic palynomorph assemblages.
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Palynostratigraphy of the Subsurface Carboniferous, Permian, and Triassic in Southern Israel

Proceedings of the Annual Meeting. American Association of Stratigraphic Palynologists, 1974
Abstract Carboniferous, Permian, and Triassic sporomorphs from Zohar 8 and ‘Avdat 1 boreholes (southern Israel) are studied. Three assemblage zones, based on the distribution of sporomorphs, are established: the Punctatosporites minutus Zone, of Westphalian age, overlain unconformably by the Klausipollenites schaubergeri Zone of Thuringian age, and the
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