Geology of the Sandercock Nunataks in Enderby Land, East Antarctica (Reports of the Japanese Antarctic Research Expedition)

• Main Authors: Kazuyuki SHIRAISHI, Okitsugu WATANABE, Koshiro KIZAKI
• Format: Article in Journal/Newspaper
• Language: English
• Published: National Institute of Polar Research 1972
• Subjects: geo; Antarctic; Bukt; East Antarctica; Queen Maud Land; Sandercock Nunataks; Antarc*; Antarctica; Enderby Land
• Online Access: https://doi.org/10.15094/00007688; https://doaj.org/article/6c8db63505f14651b9f0831f7b441b18

The Sandercock. Nunataks (68°33'S, 52°07'E) are composed of several small nunataks which are tentatively named A, B, C and D. Nunatak "A" consists mainly of hornblende-biotite gneiss and Nunatak "B" of hypersthene-garnet gneiss and garnet gneiss. Nunatak "C" is composed of hypersthene-hornblende gneiss. They are associated with aplites, pegmatites and metabasites. The petrographic observations under the microscope reveal that the unstable hypersthene signifies the transition of the granulite facies conditions to the amphibolite facies conditions. The transition is not unusual throughout the East Antarctic platform, particularly in the Lutzow-Holm Bukt area and Queen Maud Land.