Oxygen and hydrogen isotope evidence for the origin of plantinum-group element mineralization in Alaskan-type intrusions at Fifield, Australia

被引：13

作者：

Andrew, AS

Hensen, BJ

Dunlop, AC

Agnew, PD

机构：

[1] CSIRO,DIV EXPLORAT GEOSCI,N RYDE,NSW 2113,AUSTRALIA

[2] UNIV NEW S WALES,KENSINGTON,NSW 2033,AUSTRALIA

来源：

ECONOMIC GEOLOGY AND THE BULLETIN OF THE SOCIETY OF ECONOMIC GEOLOGISTS | 1995年 / 90卷 / 06期

关键词：

D O I：

10.2113/gsecongeo.90.6.1831

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：

Platinum-rich midcrustal and zoned intrusive complexes in the Fifield district make up part of a broad zone of Late Ordovician shoshonitic igneous rocks which crop out over a wide area of the eastern Lachlan fold belt. By studying the oxygen isotope fractionation between minerals in the Fifield intrusions, the significance of various magmatic processes is assessed. -from Authors

引用

页码：1831 / 1840

页数：10

共 39 条

[1]

AGNEW PD, 1987, OCT PLAT HOR LAY INT

[2]

AGNEW PD, 1987, THESIS U NEW S WALES

[3]

[Anonymous], [No title captured]

[4] SULFIDE AND PLATINUM MINERALIZATION IN THE MERENSKY REEF - EVIDENCE FROM HYDROUS SILICATES AND FLUID INCLUSIONS [J].