CHLORITOID AND ISOCHEMICAL CHARACTER OF BARROWS ZONES

被引：41

作者：

CHINNER, GA

机构：

来源：

关键词：

D O I：

10.1093/petrology/8.2.268

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

引用

页码：268 / &

共 29 条

[1] A PETROGENETIC GRID FOR FE-MG SILICATES OF PELITIC SCHISTS [J].

ALBEE, AL .

[2]

ATHERTON MP, 1964, AM MINERAL, V49, P1331

[3]

Barrow G., 1893, Q J GEOL SOC LOND, V49, P330, DOI [10.1144/GSL.JGS.1893.049.01-04.52, DOI 10.1144/GSL.JGS.1893.049.01-04.52]

[4]

BARROW G, 1898, Q J GEOL SOC LOND, V54, P149

[5] THE ORIGIN OF SILLIMANITE IN GLEN CLOVA, ANGUS [J].

CHINNER, GA .

[6] KYANITE ISOGRAD IN GLEN CLOVA ANGUS SCOTLAND [J].

CHINNER, GA .

MINERALOGICAL MAGAZINE AND JOURNAL OF THE MINERALOGICAL SOCIETY, 1965, 34 (268) :132-&

[7]

CHINNER GA, 1960, J PETROL, V1, P178

[8]

CHINNER GA, 1966, Q J GEOL SOC LOND, V122, P158

[9]

ERNST WG, 1964, AM MINER, V48, P1357

[10]

FAWCETT JJ, 1964, CARNEGIE I WASHINGTO, V63, P137