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发表于 2025-3-21 16:21:59 | 显示全部楼层 |阅读模式
书目名称Granulites and Crustal Evolution
编辑D. Vielzeuf,Ph. Vidal
视频video
丛书名称Nato Science Series C:
图书封面Titlebook: ;
出版日期Book 1990
版次1
doihttps://doi.org/10.1007/978-94-009-2055-2
isbn_softcover978-94-010-7422-3
isbn_ebook978-94-009-2055-2Series ISSN 1389-2185
issn_series 1389-2185
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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.
发表于 2025-3-22 08:08:31 | 显示全部楼层
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.
发表于 2025-3-22 08:46:26 | 显示全部楼层
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
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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
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