Problems of lithostratigraphic classification of Holocene deposits in the perimarine area of The Netherlands
Its is concluded that the lithostratigraphic classification of the Holocene sediments in the coastal area has to be disconnected from the genetic concept of a perimarine area. A new system for lithostratigraphic classification in the perimarine area
Terminology and lithostratigraphic division of (surficial) sandy eolian deposits in the Netherlands: an evaluation
homogeneous sand types, have been summarized. A simplified lithostratigraphic division of surficial eolian sediments into three formations is proposed.
Paleoclimatic reconstruction in Belgium and in Greece based on Quaternary lithostratigraphic sequences in Current issues in climate research.
Continental soil-sedimentological lithostratigraphical records from the Eastern Mediterranean and the Southern North Sea prove to be comparable and reveal long term periodicities which allow subdivision of the Pleistocene into four Maxi Cycles
Ecobiostratigraphic, lithostratigraphic, depositional and synthemic setting of Cenozoic units in Southern Sardinia (Italy)
The AA. propose a revision of the nomenclature of the formational units Auct., defining new lithostratigraphic, depositional and synthem units within the Tertiary sedimentary successions cropping out in Southern Sardinia, in particular those
A lithostratigraphic subdivision and a biostratigraphic classification of marine Neogene deposits are presented. The main lithostratigraphic established are the Oosterhout Formation and the older Breda Formation, Five biozones, distinguished mainly
An almost complete Early-Pleistocene sequence of the Tegelen and Kedichem Formation has been studied in the southern Netherlands and northern Belgium. Former Dutch and Belgian lithostratigraphic units are correlated and a new, more detailed
lithostratigraphic framework is proposed. The provenance of the sediments was established by heavy mineral and gravel analysis. Rhine, Meuse and rivers from the Scheldt basin contributed their sediments to the southern North Sea basin during different stages
lithostratigraphic sections have been studied. On the basis of the lithostratigraphic evidence, sedimentary architectures and structures, and paleontological data a paleoenvironmental reconstruction is suggested. Finally, the paleoecological meaning of these species
Levantine Sea-Nile cone lithostratigraphic evolution: quantitative analysis and correlation with paleoclimatic and eustatic oscillations in the late Quaternary
A system for automated correlation of digitized well logs based on lithostratigraphic characters has been developed. Modular in design and concept the system employs a mean value, moving window algorithm for zoning digitized well logs, a stretching
algorithm, a cross-correlation program, and a mapping function that highlights correlations between zones. In an application of this system to the Upper Glen Rose Formation of northeastern Texas, a number of distinct lithostratigraphic zones were detected
The dating is based on new paleomagnetic polarity determinations and on the lithostratigraphic position of the fossils in the loess-paleosol sequence. The results confirm that both localities are older than the first occupation of Zhoukoudian. New
Opinions differ as to whether the true red clays mostly deposited on Upper Pannonian lacustrine sediments are dated as Pliocene or early Quaternary. Biostratigraphic and lithostratigraphic data show that these non-rewashed residual deposits of red
This study deals with litho-and chronostratigraphy of the Holocene in the central and northern part of the Province of North-Holland. The area under discussion can be divided lithostratigraphically into two parts: the area of the beach barriers
The geomorphological, lithostratigraphical, paleontological and paleomagnetic data were considered together for the profile of the Gyongyosvisonta open cast lignite mine pit. (DLO).
the glacial dynamics during the Pomeranian phase in NW Poland, for which two different models exist. Investigations have been carried out at coastal cliffs east of Świnoujście, where it is possible to get good lithostratigraphic control of the Weichselian