Geochemical Characteristics of Jurassic Plume Magmatism in Ahlmannryggen Massif (Queen Maud Land, East Antarctica)


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Resumo

The Mesozoic dykes related to the distribution of Karoo plume on the territory of East Antarctica are studied. It is shown that magnesian high-Ti ferrobasalts are found in the area of Ahlmannryggen massif. Their formation is determined by melting of the mantle that contains pyroxenite. The isotope characteristics of the studied dolerites reflect the composition of a pyroxenite source, i.e., the ancient oceanic lithosphere (EMI) that subsided to the mantle depths of 150–170 km in the paleosubduction zone of the continent of Gondwana and was transformed to the pyroxenite melt 180 Ma ago during the interaction with mantle peridotite of the plume.

Sobre autores

N. Sushchevskaya

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Science

Autor responsável pela correspondência
Email: nadyas@geokhi.ru
Rússia, Moscow, 119991

B. Belyatsky

Karpinsky Russian Geological Research Institute,
Center for Isotopic Research

Autor responsável pela correspondência
Email: bbelyatsky@mail.ru
Rússia, St. Petersburg, 199106

G. Leitchenkov

Gramberg All-Russia Research Institute of Geology
and Mineral Resources of the World Ocean

Email: bbelyatsky@mail.ru
Rússia, St. Petersburg, 190121

V. Batanova

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Science; Université Grenoble Alpes, Institute Science de la Terre (ISTerre)

Email: bbelyatsky@mail.ru
Rússia, Moscow, 119991; Grenoble

A. Sobolev

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Science; Université Grenoble Alpes, Institute Science de la Terre (ISTerre)

Email: bbelyatsky@mail.ru
Rússia, Moscow, 119991; Grenoble

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