PETROPHYSICAL PROPERTIES OF QUATERNARY LAVAS OF SPITSBERGEN

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dc.contributor.author Ladygin V.M.
dc.contributor.author Frolova Ju.V.
dc.contributor.author Genshaft Yu.S.
dc.date.accessioned 2021-12-16T08:40:55Z
dc.date.available 2021-12-16T08:40:55Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=21517808
dc.identifier.citation Russian Journal of Earth Sciences, 2003, 5, 4, 291-298
dc.identifier.issn 1681-1208
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/33420
dc.description.abstract The chemical and mineralogical composition, structure and petrophysical properties of volcanic rocks, composing three Quaternary volcanoes of Spitsbergen island - Sverrefjellet, Halvdanpiggen and Sigurdfjellet - have been studied and compared. The sharp tendency of basalts elastic properties' change in a row of volcanism "rejuvenation'' - Sigurdfjellet - Halvdanpiggen - Sverrefjellet has been obtained. The same links between petrophysical characteristics have been defined for all studied volcanoes. This paper reveals the benefits of petrophysical properties - density ( <font face="Symbol">r ), porosity ( P ), velocity of longitudinal waves ( Vp ), strength ( Rc ) - for the definition of lava flows within basaltic outcrops. The petrophysical peculiarities of Spitsbergen basalts have been shown in comparison with basalts from various tectonic unites of the Earth - rifts, island arcs and foldbelts.
dc.subject SPITSBERGEN
dc.subject BASALTS
dc.subject PETROPHYSICAL PROPERTIES
dc.subject Quaternary
dc.title PETROPHYSICAL PROPERTIES OF QUATERNARY LAVAS OF SPITSBERGEN
dc.type Статья
dc.subject.age Cenozoic::Quaternary
dc.subject.age Кайнозой::Четвертичная ru


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