ALUMINOUS ENCLAVES IN GEDRITE-CORDIERITE GNEISS FROM SOUTHWESTERN NEW HAMPSHIRE

被引:57
作者
ROBINSON, P
JAFFE, HW
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D O I
10.2475/ajs.267.3.389
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Gedrite-cordierite gneisses interbedded with other mafic rocks from Middle Ordovician Ammnoosuc Volcanics of Richmond, New Hampshire, contain aluminous enclaves in cordierite composed of kyanite, sillimanite, corundum, staurolite, spinel, and bytownite; original gedrite-kyanite- sillimanite gneisses reacted to form cordierite so that remnant aluminosilicates are nowhere in contact with dedrite; phase analysis using compositional information suggests that enclave assemblages resulted from continuous reactions which formed progressively more Fe-rich cordierite with changing pressures and temperature.
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页码:389 / &
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