AN INTRODUCTION TO GROUND PENETRATING RADAR (GPR) IN SEDIMENTS

dc.contributor.author	Bristow C.S.
dc.contributor.author	Jol H.M.
dc.date.accessioned	2022-02-06T10:21:35Z
dc.date.available	2022-02-06T10:21:35Z
dc.date.issued	2003
dc.identifier	https://elibrary.ru/item.asp?id=14248780
dc.identifier.citation	Geological Society Special Publication, 2003, 211, 1-7
dc.identifier.issn	0305-8719
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/35017
dc.description.abstract	In sedimentary geology, ground penetrating radar (GPR) is used primarily for stratigraphic studies where near-continuous, high-resolution profiles aid in determining: (1) stratigraphic architecture, (2) sand-body geometry, and (3) correlation and quantification of sedimentary structures. In the past, to investigate lateral continuity and variability of sediments, we had to infer the correlation between boreholes, outcrops or shallow trenches.
dc.title	AN INTRODUCTION TO GROUND PENETRATING RADAR (GPR) IN SEDIMENTS
dc.type	Статья

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