Chlorine-bearing lizardite from metakimberlite of the Udachnaya-East pipe, northern Yakutia

Chlorine-bearing lizardite from metakimberlite of the Udachnaya-East pipe, northern Yakutia

Among serpentinite group minerals (lizardite, chrysotile, and antigorite), lizardite is the lowest temperature, whereas antigorite is the highest temperature. In nature, olivine in ultramafic and mafic rocks of fold areas and platforms is commonly replaced by these minerals. The most abundant ultram...

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Veröffentlicht in:Doklady earth sciences 2010-03, Vol.431 (1), p.403-405
Hauptverfasser: Spiridonov, E. M., Pautov, L. A., Sokolova, E. L., Vorob’ev, E. I., Agakhanov, A. A.
Format: Artikel
Sprache:eng
Schlagworte:
Chlorine
Earth and Environmental Science
Earth Sciences
Geochemistry
Mineralogy
Minerals
Oceanic crust
Petrology
Sea-water
Seawater
Serpentinite
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container_issue 1
container_start_page 403
container_title Doklady earth sciences
container_volume 431
creator Spiridonov, E. M.
Pautov, L. A.
Sokolova, E. L.
Vorob’ev, E. I.
Agakhanov, A. A.
description Among serpentinite group minerals (lizardite, chrysotile, and antigorite), lizardite is the lowest temperature, whereas antigorite is the highest temperature. In nature, olivine in ultramafic and mafic rocks of fold areas and platforms is commonly replaced by these minerals. The most abundant ultramafic serpentinite composes a significant part of oceanic crusts and a substantial part of fold areas of the eugeosyncline (Ural) type. Basically, such serpentinite was formed involving seawater, which in addition to other features is documented by chlorine in lizardite, the major mineral of such serpentinite.
doi_str_mv 10.1134/S1028334X10030293
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source SpringerNature Journals
subjects Chlorine
Earth and Environmental Science
Earth Sciences
Geochemistry
Mineralogy
Minerals
Oceanic crust
Petrology
Sea-water
Seawater
Serpentinite
title Chlorine-bearing lizardite from metakimberlite of the Udachnaya-East pipe, northern Yakutia
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