Results 251 to 260 of about 15,112 (291)
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Weichselian chronostratigraphy and correlations

Boreas, 1981
The glacial history of the Fennoscandian ice cap beyond some 20,000 years B.P. is fairly poorly known because of the absence of a reliable dating control. The Eemian Interglacial of Europe is not dated at all. The Weichselian Glaciation seems to be characterized by three main glaciation maxima separated by two main interstadial periods (of quite ...
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Late Pleistocene-Holocene aeolian loess-paleosol sections in the Yellow River source area on the northeast Tibetan Plateau: chronostratigraphy, sediment provenance, and implications for paleoclimate reconstruction

CATENA, 2022
Yaofeng Jia   +12 more
semanticscholar   +1 more source

Chronostratigraphy

2014
Stephan van Gasselt, Gerhard Neukum
  +5 more sources

Permian chronostratigraphy in Kansas

Geology, 1990
Correlations between the type Permian System of Russia and North American strata have been difficult for decades because of biostratigraphic and nomenclatural confusion. Consequently, a standard Permian section was established in west Texas that is widely accepted throughout North America. Series of the North American standard section are, in ascending
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Chronostratigraphy beyond the GSSP

Stratigraphy, 2007
The introduction of the GSSP concept has been successful to the extent that it has fostered a considerable amount of stratigraphic studies. It has also led to a re-thinking of stratigraphic principles and practices. Chronostratigraphy as practiced today attempts to reconcile two opposite philosophical principles, the rock-time model of Hedberg and the ...
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Chronostratigraphy of Upper Eocene Microspherules

PALAIOS, 1989
Impact-glass microspherules occur at numerous localities in rocks that can be dated as late Eocene. There is debate as to whether the discovered microspherule layers are the result of two or three impact events. Standard biostratigraphic techniques have been employed to date the microspherule layers.
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Chronostratigraphie de l'Europe würmienne

Bulletin de l'Association française pour l'étude du quaternaire, 1968
From recent data, the author strives to justify division of the Würm in three parts: Eowürm (75 000 B P. -55 000 B P.), Mesowürm (55 000 B. P. -27 000 B.P.), , Néowürm (27 000 B.P.-10 300 B P.). He tries to caracteris some great natural domains utilizing particularly mousterian and leptolithic settlements maps, « front pioneer » succeeding positions ...
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