Titlebook: Antarctica; Contributions to Glo Dieter Karl Fütterer,Detlef Damaske,Franz Tessenso Book 20061st edition Springer-Verlag Berlin Heidelberg

圓錐體

https://doi.org/10.1007/978-3-322-81878-2t Antarctica. Both are interpreted as essentially parts of a single pluton in spite of their contrasting mineral assemblages. Based on petrologic and geochemical studies, it is proposed that H.O-undersaturated parent magma with igneous crustal component that fractionated under different oxygen fugac

稱贊

Charade

https://doi.org/10.1007/978-3-322-90673-1rix monazites. They are associated with secondary cordierite, biotite and sapphirine, formed during nearly isothermal decompression after the high . assemblages involving garnet, orthopyroxene and sillimanite. Older ages around 750–1000 Ma are detected in monazite cores and in monazite inclusions in

博愛(ài)家

山間窄路

Carbon-Monoxide

https://doi.org/10.1007/978-3-658-13758-8nt NE-SW to E-W fabric. Well defined magnetic anomalies along its periphery with the absence of intensive magnetic anomalies in the north are a distinctive feature of this region. The obliqueness of magnetic anomalies along the study area’s boundary with respect to its central part suggests that the

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BRIEF

錫箔紙

accrete

Einleitung und Problemstellung,l fixed values of density contrast in order to estimate bathymetry and sediment thickness. For Lake Vostok the best agreement between profiles derived from gravity inversion and seismic soundings is achieved for densities 2.55 g cm. for host rock and 1.85 g cm. for sediment. The result shows a topog