The high‐pressure complex of the shackleton range of antarctica

V. S. Semenov; Ye A. Vapnik

doi:10.1080/10889379209377476

The high‐pressure complex of the shackleton range of antarctica

Research output: Contribution to journal › Article › peer-review

Abstract

The study comprises an investigation of the Shackleton Range (which is a part of the East Antarctic craton) by two geologists affiliated with the Russian Academy of Sciences in St. Petersburg. It is focused on thermodynamic conditions of metamorphism and includes an analysis of fluid characteristics based on the cryometric method. The detected presence of slightly mineralized salt‐water inclusions in quartz provided new evidence suggesting a crustal nature of the fluid and an isochemical nature of the metamorphism.

Original language	English
Pages (from-to)	72-85
Number of pages	14
Journal	Polar Geography and Geology
Volume	16
Issue number	1
DOIs	https://doi.org/10.1080/10889379209377476
State	Published - 1 Jan 1992
Externally published	Yes

ASJC Scopus subject areas

Geography, Planning and Development
General Environmental Science
General Agricultural and Biological Sciences
General Earth and Planetary Sciences

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

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10.1080/10889379209377476

Cite this

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AB - The study comprises an investigation of the Shackleton Range (which is a part of the East Antarctic craton) by two geologists affiliated with the Russian Academy of Sciences in St. Petersburg. It is focused on thermodynamic conditions of metamorphism and includes an analysis of fluid characteristics based on the cryometric method. The detected presence of slightly mineralized salt‐water inclusions in quartz provided new evidence suggesting a crustal nature of the fluid and an isochemical nature of the metamorphism.

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The high‐pressure complex of the shackleton range of antarctica

Abstract

ASJC Scopus subject areas

UN SDGs

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