FE-NI-CU SULFIDES IN TECTONITE PERIDOTITES FROM THE MAQSAD DISTRICT, SUMAIL OPHIOLITE, SOUTHERN OMAN - IMPLICATIONS FOR THE ORIGIN OF THE SULFIDE COMPONENT IN THE OCEANIC UPPER MANTLE

被引：45

作者：

LORAND, JP

机构：

来源：

关键词：

D O I：

10.1016/0040-1951(88)90240-5

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：57 / 73

页数：17

共 49 条

AHMED, Z ;

HALL, A .

[2]

[Anonymous], 1973, T CANADIAN I MINING, V76, P183

[3]

ASHLEY PM, 1975, J GEOL SOC AUST, V22, P320

[4] NEW DATA ON PHASE RELATIONS IN CU-FE-S SYSTEM [J].

CABRI, LJ .

[5]

CEULENEER G, 1986, THESIS U NANTES NANT

[6] TECTONIC SETTING FOR OPHIOLITE OBDUCTION IN OMAN [J].

COLEMAN, RG .

JOURNAL OF GEOPHYSICAL RESEARCH, 1981, 86 (NB4) :2497-2508

[7]

CZAMANSKE GK, 1977, GEOL SOC AM BULL, V88, P587, DOI 10.1130/0016-7606(1977)88<587:CAPCOS>2.0.CO

[8]

DICK, HJB ;

BULLEN, T .

ECKSTRAND, OR .