DISCOVERY OF MICRODIAMONDS AND ASSOCIATED MINERALS IN THE MAKHTESH RAMON CANYON (NEGEV DESERT, ISRAEL)

Eppelbaum L.V.; Kuznetsov S.V.; Sazonova L.V.; Korotaeva N.N.; Belovitskaya G.I.; Smirnov S.A.; Surkov A.V.; Bezlepkin B.M.; Katz Yu.I.; Vaksman V.L.

dc.contributor.author	Eppelbaum L.V.
dc.contributor.author	Kuznetsov S.V.
dc.contributor.author	Sazonova L.V.
dc.contributor.author	Korotaeva N.N.
dc.contributor.author	Belovitskaya G.I.
dc.contributor.author	Smirnov S.A.
dc.contributor.author	Surkov A.V.
dc.contributor.author	Bezlepkin B.M.
dc.contributor.author	Katz Yu.I.
dc.contributor.author	Vaksman V.L.
dc.date.accessioned	2024-11-09T08:38:23Z
dc.date.available	2024-11-09T08:38:23Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13529082
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 202-204
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46452
dc.description.abstract	The Makhtesh Ramon erosional–tectonic depression (canyon), 40 km long and approximately 8 km wide, is situated in the Negev Desert (southern Israel), 65 km southwest of the Dead Sea. The canyon rim and center are located at an altitude of 800–1000 and 400–600 m, respectively. In terms of tectonics, this structure represents the southern margin of the Syrian-Sinai block–fold belt. A comprehensive analysis of the available regional geophysical data revealed a collision-related origin of the belt.
dc.title	DISCOVERY OF MICRODIAMONDS AND ASSOCIATED MINERALS IN THE MAKHTESH RAMON CANYON (NEGEV DESERT, ISRAEL)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06020097