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

Wilson

书目名称Antarctica影响因子(影响力)




书目名称Antarctica影响因子(影响力)学科排名




书目名称Antarctica网络公开度




书目名称Antarctica网络公开度学科排名




书目名称Antarctica被引频次




书目名称Antarctica被引频次学科排名




书目名称Antarctica年度引用




书目名称Antarctica年度引用学科排名




书目名称Antarctica读者反馈




书目名称Antarctica读者反馈学科排名

贝雷帽

Characteristics of Metamorphosed Banded Iron Formation and Its Relation to the Magnetic Anomaly in tnvestigated in order to understand why a large magnetic anomaly appeared in this region. The study found many meta-BIF layers, consisting of one to nine layers within 30 m thickness in felsic gneiss. The thicknesses of individual layers were usually 0.5–2 m but sometimes varied from zero to 6 m. Alm

尊敬

Experimental Constraints on the Decompressional , Paths of Rundvågshetta Granulites, Lützow-Holm Comgive constraints on the . path of sillimanite-cordierite-sapphirine granulites from Rundvågshetta, Lützow-Holm Complex, East Antarctica. Combining the previous temperature estimates and the present data, we can infer that the Rundvågshetta granulites experienced the peak metamorphism at 925–1039 °C

ABHOR

Sapphirine — Orthopyroxene — Garnet Granulite from Schirmacher Hills, Central Dronning Maud Landciation with orthopyroxene and garnet. Sapphirine occurs as inclusions together with orthopyroxene within garnet and as discrete grains together with spinel, secondary orthopyroxene in cordierite coronas. Orthopyroxene porphyroblasts have the highest Al.O. contents (∼10 wt.-%) so far reported from D

背心

Predigest

justify

Electron Microprobe (EMP) Dating on Monazite from Forefinger Point Granulites, East Antarctica: Implrix 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

fledged

caldron

挣扎

Magnetic Anomalies of the Grove Mountains Region and Their Geological Significancent 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