SOME ASPECTS OF MAGNETOSTRATIGRAPHIC CORRELATION

dc.contributor.author	Molostovskii E.A.
dc.date.accessioned	2020-11-30T07:32:07Z
dc.date.available	2020-11-30T07:32:07Z
dc.date.issued	1996
dc.identifier	https://elibrary.ru/item.asp?id=13240881
dc.identifier.citation	Stratigraphy and Geological Correlation, 1996, , 3, 231-237
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19915
dc.description.abstract	The traditional visual comparison of paleomagnetic columns with the consecutive counting of magnetozones of different polarities is liable to many errors. In this approach the following methodical miscalculations are particularly apparent: the loss of an interval, an arbitrary interpolation of paleomagnetic boundaries, comparison of magnetozones of different ranks, and erroneous identification of magnetozones. Paleomagnetic stratigraphic correlation is practically impossible without exact correlation between paleontological, lithological and facies data. Appropriate examples are given to show the procedure of magnetostratigraphic correlation of marine and continental deposits in widely spaced biogeographic provinces.
dc.title	SOME ASPECTS OF MAGNETOSTRATIGRAPHIC CORRELATION
dc.type	Статья

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