Crustal development in relation to granitic magmatism in regard to D/H partition between coexisting hornblende and biotite in the Svecofennian belt

Crustal development in relation to granitic magmatism in regard to D/H partition between coexisting hornblende and biotite in the Svecofennian belt

Tie-lines in the σD-XFe diagram of hornblende and biotite in Japanese island arc granites give commonly a similar slope to that derived from the equation of Suzuoki-Epstein's experimental work (1976). This indicates that in the process of granite intrusion in the island arc environment, the wat...

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Bibliographic Details
Main Authors: Y. Kuroda, T. Yamada, Y. Yamaguchi, H. Sato, Y. Wake, S. Matsuo
Format: Article
Language:English
Published: Geological Society of Finland 1993-12-01
Series:Bulletin of the Geological Society of Finland
Subjects:
granites
rapakivi
hornblende
geochemistry
D/H
igneous activity
fractional crystallization
Svecofennides
Proterozoic
Finland
Sweden
Online Access:http://www.geologinenseura.fi/bulletin/Volume65/sgs_bt_065_2_pages_091_108.pdf

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http://www.geologinenseura.fi/bulletin/Volume65/sgs_bt_065_2_pages_091_108.pdf

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