High-grade metamorphic rocks in Instekleppane, Lützow-Holm Complex, east Antarctica: A potential new locality of ultrahigh-temperature (UHT) metamorphic rocks
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引用次数: 0
Abstract
The first comprehensive multi-day geological survey was conducted at Instekleppane in the southern part of the Lützow-Holm Complex, East Antarctica, by the 65th Japanese Antarctic Research Expedition (JARE65). This exposure is predominantly composed of felsic orthopyroxene-biotite gneiss, leucocratic garnet-biotite gneiss, granitic biotite gneiss, and felsic garnet-orthopyroxene-biotite gneiss with intercalations of mafic granulites, meta-ultramafic rocks, and Mg–Al-rich rocks. Several Mg–Al-rich rocks, such as sapphirine-cordierite-biotite gneiss and garnet-sapphirine-orthopyroxene-cordierite gneiss, have reaction textures indicating decompression under ultrahigh-temperature (UHT) conditions. Similar lithological relations and metamorphic signatures have been reported from Rundvågshetta, suggesting a possible geological linkage between these exposures.
期刊介绍:
Polar Science is an international, peer-reviewed quarterly journal. It is dedicated to publishing original research articles for sciences relating to the polar regions of the Earth and other planets. Polar Science aims to cover 15 disciplines which are listed below; they cover most aspects of physical sciences, geosciences and life sciences, together with engineering and social sciences. Articles should attract the interest of broad polar science communities, and not be limited to the interests of those who work under specific research subjects. Polar Science also has an Open Archive whereby published articles are made freely available from ScienceDirect after an embargo period of 24 months from the date of publication.
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