FE-MG RELATIONSHIPS IN SECTOR-ZONED SUBMARINE BASALT PLAGIOCLASE

被引：43

作者：

BRYAN, WB ^{[1
]}

机构：

[1] WOODS HOLE OCEANOG INST,WOODSHOLE,MA 02543

来源：

关键词：

D O I：

10.1016/0012-821X(74)90092-2

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：157 / 165

页数：9

共 19 条

[1]

APPLEMAN DE, 1971, GEOCHIM COSM SUPPL, V1, P117

[2]

BELL PM, PERSONAL COMMUNICATI

BENCE, AE ;

ALBEE, AL .

[4] MORPHOLOGY OF QUENCH CRYSTALS IN SUBMARINE BASALTS [J].

BRYAN, WB .

JOURNAL OF GEOPHYSICAL RESEARCH, 1972, 77 (29) :5812-+

[5] LOW-POTASH DACITE DRIFT PUMICE FROM CORAL SEA [J].

BRYAN, WB .

[6]

CRAWFORD ML, 1973, GEOCHIM COSM SUPPL, V1, P705

[7]

Deer W.A., 1966, INTRO ROCK FORMING M

[8]

FREY FA, IN PRESS

[9] OXIDATION STATE OF IRON IN PLAGIOCLASE FROM LUNAR BASALTS [J].

HAFNER, SS ;

VIRGO, D ;

WARBURTO.D .

[10]

HOLLISTER LS, 1970, 11 P AP LUN SCI C, V1, P541