GARNET ZONING AND METAMORPHISM OF THE BARROVIAN TYPE AREA, SCOTLAND

被引：68

作者：

DEMPSTER, TJ ^{[1
]}

机构：

[1] UNIV EDINBURGH,GRANT INST GEOL,EDINBURGH EH9 3JW,MIDLOTHIAN,SCOTLAND

来源：

关键词：

D O I：

10.1007/BF01177588

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：30 / 38

页数：9

共 38 条

[1] STAUROLITE AT ANOMALOUSLY HIGH-GRADE [J].

ASHWORTH, JR .

[2]

ATHERTON M.P., 1968, CONTRIB MINERAL PETR, V18, P347, DOI [10.1007/BF00399696, DOI 10.1007/BF00399696]

[3]

ATHERTON M.P., 1972, SCOTT J GEOLC, V8, P203

[4]

BARROW G., 1912, P GEOL ASS, V23, P268

[5]

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]

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

CHINNER, GA .

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

[7]

De Bethune P., 1975, CONTRIB MINERAL PETR, V50, P197

[8] LOCALIZED UPLIFT IN THE SCOTTISH DALRADIAN [J].

DEMPSTER, TJ .

[9]

DEMPSTER TJ, 1984, J GEOL SOC LOND

[10]

DEMPSTER TJ, 1983, THESIS U EDINBURGH