Details
| Originalsprache | Englisch |
|---|---|
| Seiten (von - bis) | 527-536 |
| Seitenumfang | 10 |
| Fachzeitschrift | European Journal of Mineralogy |
| Jahrgang | 3 |
| Ausgabenummer | 3 |
| Publikationsstatus | Veröffentlicht - 5 Juni 1991 |
Abstract
Experiments were conducted in order to investigate the influence of tourmaline and the effect of boron (B) on amount and composition of partial melts generated during anatexis. In runs with low fraction of melt the run products were melt, newly crystallized cordierite, residual biotite, plagioclase, quartz and alkali feldspar. With increasing melt fraction, alkali feldspar and finally also quartz participate completely in the melt. Except for Al, which is higher in B-rich melts, the compositions of B-bearing and B-free melts are not significantly different. -from Authors
ASJC Scopus Sachgebiete
- Erdkunde und Planetologie (insg.)
- Geochemie und Petrologie
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in: European Journal of Mineralogy, Jahrgang 3, Nr. 3, 05.06.1991, S. 527-536.
Publikation: Beitrag in Fachzeitschrift › Artikel › Forschung › Peer-Review
}
TY - JOUR
T1 - Effect of tourmaline on melt fraction and composition of first melts in quartzofeldspathic gneiss
AU - Holtz, Francois
AU - Johannes, Wilhelm
N1 - Copyright: Copyright 2018 Elsevier B.V., All rights reserved.
PY - 1991/6/5
Y1 - 1991/6/5
N2 - Experiments were conducted in order to investigate the influence of tourmaline and the effect of boron (B) on amount and composition of partial melts generated during anatexis. In runs with low fraction of melt the run products were melt, newly crystallized cordierite, residual biotite, plagioclase, quartz and alkali feldspar. With increasing melt fraction, alkali feldspar and finally also quartz participate completely in the melt. Except for Al, which is higher in B-rich melts, the compositions of B-bearing and B-free melts are not significantly different. -from Authors
AB - Experiments were conducted in order to investigate the influence of tourmaline and the effect of boron (B) on amount and composition of partial melts generated during anatexis. In runs with low fraction of melt the run products were melt, newly crystallized cordierite, residual biotite, plagioclase, quartz and alkali feldspar. With increasing melt fraction, alkali feldspar and finally also quartz participate completely in the melt. Except for Al, which is higher in B-rich melts, the compositions of B-bearing and B-free melts are not significantly different. -from Authors
UR - http://www.scopus.com/inward/record.url?scp=0026076936&partnerID=8YFLogxK
U2 - 10.1127/ejm/3/3/0527
DO - 10.1127/ejm/3/3/0527
M3 - Article
AN - SCOPUS:0026076936
VL - 3
SP - 527
EP - 536
JO - European Journal of Mineralogy
JF - European Journal of Mineralogy
SN - 0935-1221
IS - 3
ER -