EVOLUTION OF HIGH-TEMPERATURE HYDROTHERMAL FLUIDS ASSOCIATED WITH GREISENIZATION AND FELDSPATHIC ALTERATION OF A TIN-MINERALIZED GRANITE, NORTHEAST QUEENSLAND

被引:36
作者
WITT, WK [1 ]
机构
[1] JAMES COOK UNIV N QUEENSLAND,TOWNSVILLE,QLD 4811,AUSTRALIA
关键词
D O I
10.2113/gsecongeo.83.2.310
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
收藏
页码:310 / 334
页数:25
相关论文
共 91 条
[1]   THE CHARACTER AND EVOLUTION OF HYDROTHERMAL FLUIDS ASSOCIATED WITH THE KAOLINIZED ST-AUSTELL GRANITE, SW ENGLAND [J].
ALDERTON, DHM ;
RANKIN, AH .
JOURNAL OF THE GEOLOGICAL SOCIETY, 1983, 140 (MAR) :297-309
[2]  
Anderson G.M., 1983, AM J SCI A, V283A, P283
[3]  
Anfiligov VN, 1973, GEOKHIMIYA, V1, P44
[4]  
[Anonymous], 1982, GEOCHEMISTRY NATURAL
[5]   FLUORINE IN GRANITIC ROCKS AND MELTS - REVIEW [J].
BAILEY, JC .
CHEMICAL GEOLOGY, 1977, 19 (01) :1-42
[6]  
Barsukov V.L, 1973, GEOCHEM INT+, V10, P363
[7]  
BARSUKOV VL, 1966, GEOCHEM INT, V3, P759
[8]  
BARSUKOV VL, 1969, GEOCHEM INT, V6, P310
[9]  
BARSUKOV VL, 1967, ISRAEL PROGRAM SCI T, V2, P211
[10]   BIOTITE STABILITY IN PORPHYRY COPPER ENVIRONMENT [J].
BEANE, RE .
ECONOMIC GEOLOGY, 1974, 69 (02) :241-256