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只看該作者 · 發(fā)表于 2025-3-21 16:21:59

書(shū)目名稱(chēng)Granulites and Crustal Evolution影響因子(影響力)

書(shū)目名稱(chēng)Granulites and Crustal Evolution影響因子(影響力)學(xué)科排名

書(shū)目名稱(chēng)Granulites and Crustal Evolution網(wǎng)絡(luò)公開(kāi)度

書(shū)目名稱(chēng)Granulites and Crustal Evolution網(wǎng)絡(luò)公開(kāi)度學(xué)科排名

書(shū)目名稱(chēng)Granulites and Crustal Evolution被引頻次

書(shū)目名稱(chēng)Granulites and Crustal Evolution被引頻次學(xué)科排名

書(shū)目名稱(chēng)Granulites and Crustal Evolution年度引用

書(shū)目名稱(chēng)Granulites and Crustal Evolution年度引用學(xué)科排名

書(shū)目名稱(chēng)Granulites and Crustal Evolution讀者反饋

書(shū)目名稱(chēng)Granulites and Crustal Evolution讀者反饋學(xué)科排名

只看該作者 · 發(fā)表于 2025-3-22 00:17:50

只看該作者 · 發(fā)表于 2025-3-22 02:04:58

Susanna B. Park,Matthew C. Kiernana mechanism for producing lowered water activities in these granulites. Lower crustal xenoliths yield a wider range of values, and some are consistent with metamorphism in the presence of a CO.-rich fluid phase. These samples may represent the recrystallized equivalents of underplated basalt magmas that had high CO. contents.

只看該作者 · 發(fā)表于 2025-3-22 08:08:31

Scapolite Phase Equilibria: Additional Constraints on the Role of CO2 in Granulite Genesisa mechanism for producing lowered water activities in these granulites. Lower crustal xenoliths yield a wider range of values, and some are consistent with metamorphism in the presence of a CO.-rich fluid phase. These samples may represent the recrystallized equivalents of underplated basalt magmas that had high CO. contents.

只看該作者 · 發(fā)表于 2025-3-22 08:46:26

The NATO ARW Granulite Conference: A Reportes and Related Rocks. All geoscience disciplines were represented. Session topics at the meeting were chosen according to the major themes of the contributed abstracts. These represent an up-to-date reflection of centres of interest in this field. All abstracts quoted in this report have been publis

只看該作者 · 發(fā)表于 2025-3-22 14:01:10

只看該作者 · 發(fā)表于 2025-3-22 18:52:55

The Granulite — Granite Connexionn reactions, in the presence of a fluid dominated by a species other than H.O (e.g., CO.). Small quantities of H.O-rich fluid may be present at the onset of granulite facies conditions (≥ 650°C). This will promote limited degrees of partial fusion and the formation of granulitic migmatites, but will

只看該作者 · 發(fā)表于 2025-3-23 00:29:35

只看該作者 · 發(fā)表于 2025-3-23 02:29:28

只看該作者 · 發(fā)表于 2025-3-23 07:50:24

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