 | | Report (chapter) | | on March 6, 2015 Geosciences research in East Antarctica (088E – 6088E): present status and future perspectives...palaeoenvironmental and palaeogeographical studies, Antarctica plays a unique role in our understanding of the...of East Antarctica, especially in the Dronning Maud Land and Enderby Land regions. Enderby Land preserves...Mesoproterozoic to Palaeozoic history of Dronning Maud Land is extremely important in understanding the formation...Present understanding of the evolution of East Antarctica in terms of global tectonics allows us to visualize |  | | Report (chapter) | | garnet and kyanite in clinopyroxene – hornblende-bearing adakitic meta-tonalites from Cape Hinode, Prince...Prince Olav Coast, East Antarctica YOSHIKUNI HIROI1, YOICHI MOTOYOSHI2, NAOTO ISHIKAWA3, TOMOKAZU HOKADA2...606-8501, Japan Abstract: Xenocrystic garnet and kyanite, in addition to clinopyroxene and rare orthopyroxene...trondhjemites and tonalites (meta-tonalites) at Cape Hinode on the eastern Prince Olav Coast in the latest Proterozoic...Lützow-Holm Complex, East Antarctica. Textural and compositional features of garnet and kyanite suggest that these |  | | Report (chapter) | | Cambrian crustal evolution of eastern Dronning Maud Land, East Antarctica: a synthesis of SHRIMP U-Pb age...Cambrian crustal evolution of eastern Dronning Maud Land, East Antarctica: a synthesis of SHRIMP U – Pb...456-0002, Japan Abstract: In eastern Dronning Maud Land (DML), East Antarctica, there are several discrete...published data suggests that the main part of eastern Dronning Maud Land, including the SRM, represents juvenile...in this section of East Antarctica. The eastern part of Dronning Maud Land (DML) between 378E and 508E |  | | Report (chapter) | | thermal history of Lützow-Holm Complex, East Antarctica, based on Rb– Sr and Sm –Nd mineral chronology...southwestern part of the Lützow-Holm Complex, Dronning Maud Land, assists in constructing a thermal history after...activity reported from localities throughout East Antarctica. This intracontinental, post-orogenic igneous...locality in the Lützow-Holm Complex (LHC) of East Antarctica, which involved rapid cooling after decompression...SHIRAISHI , K. (eds) Geodynamic Evolution of East Antarctica: A Key to the East– West Gondwana Connection |  | | Report (chapter) | | of metabasites from Lützow-Holm Complex, East Antarctica YOSHIMITSU SUDA1,2, YOSHINOBU KAWANO3, GREG YAXLEY4...Metabasites from the Lützow-Holm Complex, East Antarctica, are the equivalent of metamorphosed ultramafic...suggested that the Lützow-Holm Complex (LHC) of East Antarctica is a high-grade mobile belt with metamorphic...rocks in the LHC are characterized by early formed kyanite that was replaced by sillimanite at peak temperature...SHIRAISHI , K. (eds) Geodynamic Evolution of East Antarctica: A Key to the East– West Gondwana Connection |  | | Journal (article/letter/editorial) | | 特に，石灰珪質岩塊近傍に産出するものについて Kyanitebearing tonalites from Cape Hinode, East Antarctica: with special reference...HIROI) 大和田正明(Masaaki OWADA) The Cape Hinode area in East Antarctica exposes MidProterozoic tonalites...xenocrystic garnet and kyanite. Pinite and carbonate minerals surrounding kyanite inclusions in plagioclase...calcsilicate enclaves carry kyanite fringed by similar anorthite coronas. Such kyanite sometimes encloses quartz...saturation index (0.75) in spite of the occurrence of kyanite, and a nonadakitic geochemistry. The calcsilicate |  | Owada, Masaaki, Kamei, Atsushi, Horie, Kenji, Shimura, Toshiaki, Yuhara, Masaki, Tsukada, Kazuhiro, Osanai, Yasuhito, Baba, Sotaro (2013) Magmatic history and evolution of continental lithosphere of the Sør Rondane Mountains, eastern Dronning Maud Land, East Antarctica. Precambrian Research, 234. 63-84 doi:10.1016/j.precamres.2013.02.007 | Journal (article/letter/editorial) | | of the Sør Rondane Mountains, eastern Dronning Maud Land, East Antarctica Masaaki Owada a,∗ , Atsushi Kamei...Mountains East Antarctica a b s t r a c t The Sør Rondane Mountains, eastern Dronning Maud Land, East Antarctica...02.007 and is recognized as the East-Africa-Antarctica Orogen (EAAO; Jacobs and Thomas, 2002, 2004)...older (c. 1000 Ma) basement rocks of Dronning Maud Land were differentially reworked during the Pan-African...overprint was less intense in western Dronning Maud Land but strongly affected the Mesoproterozoic rocks |  | | Journal (article/letter/editorial) | | Tanzania Craton and its NUMBER 4 APRIL 1998 eastern hinterland. These roughly N–S trending highgrade...limit for Pan-African high-grade metamorphism in eastern Tanzania at 650 Ma. The interpretation of the nature...TANZANIA Fig. 1. Simplified geological map of eastern Tanzania. Modified from Coolen (1980), after the...direction and closely approaches the craton on its eastern flank (Fig. 1). However, this subdivision does... The best exposures in the Mozambique Belt of eastern Tanzania are the granulite complexes, some of which |  | | Journal (article/letter/editorial) | | Granulite-Facies Metamorphism at Molodezhnaya Station, East Antarctica by EDWARD S. GREW Department of Earth and Space...Molodezhnaya Station (670401S, 46OE) in East Antarctica b addition to quartz, K-feldspar, and plagioclase...Earth's crust. In the Precambrian shield of East Antarctica between 40° and 50°E, the 2500 million year (m...regional geology. Precambrian rocks of East Antarctica &tween 67' and 69OS and 40° to 52OE have been...amphibolite facies such as fibrolitic sillimanite, kyanite, staurolite, and amphiboles. The Rayner complex |  | | Report (issue) | | (1982)(English). Microprobe analyses (6) from Cape Hinode, E. Antarctica. AMPHIBOLE. Kanisawa, (Mem. Geol. Soc...Microprobe analyses (9) from basanite-phonolite, Antarctica (kaersutite). 16 AMPHIBOLE. Laird, J. Petrol...117-138 (1981). Probe analyses (1) from basalts, Antarctica. AMPHIBOLE. Likhoidov et al., (Geokhimiia, 1002-1013...(1981). Microprobe analyses (1) from basalts, Antarctica Ridge. ANALCIME. Luhr and Carmichael, Contrib...140, 17-28 (1980)(English). Probe analyses (2), eastern desert, Egypt. ANTIMONY. Halenius and Alinder, |
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