SULFUDE MINERALIZATION IN A BROADLANDS GEOTHERMAL DRILL HOLE, TAUPO VOLCANIC ZONE, NEW-ZEALAND

被引：38

作者：

BROWNE, PRL

机构：

[1] N.Z. Geological Survey, Lower Hutt

来源：

ECONOMIC GEOLOGY | 1969年 / 64卷 / 02期

关键词：

D O I：

10.2113/gsecongeo.64.2.156

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：

Base-metal sulfides have been deposited in rocks penetrated by a Broadland Geothermal drill hole. They occur in a permeable, silicified and fault-brecciated zone where the measured temperature is between 272 and 276° C. Textural evidence suggests that they are in equilibrium with the slightly saline solution of low-metal content now being discharged. © 1969 Society of Economic Geologists, Inc.

引用

页码：156 / &

共 8 条

[1]

ELLIS AJ, 1968, DSIR11812 CHEM DIV

[2]

GRINDLEY GW, 1965, 75 NZ GEOL SURV B

[3]

GRINDLEY GW, 1968, 34 NZ GEOL SURV REP

[4]

HELGESON HC, 1967, RESEARCHES GEOCHEMIS, V2, P362

[5]

Hemley J. J., 1967, GEOCHEMISTRY HYDROTH, P166

[6] SULFUR ISOTOPES IN PYRITE PYRRHOTITE ALUNITE AND ANHYDRITE FROM STEAM WELLS IN TAUPO VOLCANIC ZONE NEW ZEALAND [J].

STEINER, A ;

RAFTER, TA .

ECONOMIC GEOLOGY, 1966, 61 (06) :1115-&

[7]

TATLOCK DB, 1966, 1209 US GEOL SURV B

[8]

White D.E., 1967, GEOCHEMISTRY HYDROTH, P575

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