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

Wilson

書目名稱Antarctica影響因子(影響力)




書目名稱Antarctica影響因子(影響力)學科排名




書目名稱Antarctica網(wǎng)絡(luò)公開度




書目名稱Antarctica網(wǎng)絡(luò)公開度學科排名




書目名稱Antarctica被引頻次




書目名稱Antarctica被引頻次學科排名




書目名稱Antarctica年度引用




書目名稱Antarctica年度引用學科排名




書目名稱Antarctica讀者反饋




書目名稱Antarctica讀者反饋學科排名

貝雷帽

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 Rundv?gshetta Granulites, Lützow-Holm Comgive constraints on the . path of sillimanite-cordierite-sapphirine granulites from Rundv?gshetta, Lützow-Holm Complex, East Antarctica. Combining the previous temperature estimates and the present data, we can infer that the Rundv?gshetta 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

掙扎

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