Kharin, G. S. (1997): Volcanoclastic rocks with subsilicic-ultrabasite inclusions in the transition zone of the Reykjanes Ridge

Leg/Site/Hole:
Identifier:
1999-044108
georefid

Creator:
Kharin, G. S.
Russian Academy of Sciences, Shirshov Institute of Oceanology, Atlantic Branch, Kaliningrad, Russian Federation
author

Identification:
Volcanoclastic rocks with subsilicic-ultrabasite inclusions in the transition zone of the Reykjanes Ridge
1997
Oceanology
MAIK Nauka/Interperiodica, Birmingham, AL, United States
37
1
114-120
Investigations of petrography, mineralogy, and chemical composition of gases and fluids in tuffs and lavas were carried out on the samples dredged in the transition zone from the shelf and slope of Iceland to the Reykjanes Ridge. The samples were collected from the depths of 950-720 m during different expeditions of the R/V Akademik Kurchatov and Mikhail Lomonosov. Mantle ultrabasite inclusions were first recognized in the region of Iceland. It can be assumed that they are related to eruptive structures formed on the ocean floor during the Pliocene and are associated with the Iceland "hot" spot.
English
Serial
Coverage:Geographic coordinates:
North:63.3000
West:-24.3000East: -24.0000
South:63.0000

Oceanography; Igneous and metamorphic petrology; Atlantic Ocean; Cenozoic; chemical composition; Deep Sea Drilling Project; Europe; hot spots; Iceland; igneous rocks; inclusions; lava; mantle; marine geology; mineral composition; Neogene; North Atlantic; ocean floors; petrography; plate tectonics; Pliocene; pyroclastics; research vessels; Reykjanes Ridge; samples; shelf-slope break; Tertiary; tuff; volcanic rocks; Western Europe;

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