Hydrothermal alteration of oxygen isotope ratios in quartz phenocrysts, Kidd Creek mine, Ontario: Magmatic values are preserved in zircon

Geology

Volumn 25, Issue 12, 1997, Pages 1079-1082

  King, Elizabeth M ^a   Barrie, C Tucker ^b   Valley, John W ^a  

^a UNIVERSITY OF WISCONSIN MADISON   (United States)

^b GEOLOGICAL SURVEY OF CANADA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

CLAY ALTERATION; COBALT DEPOSITS; GRANITE; ISOTOPES; MAGNETIC SUSCEPTIBILITY; MICROCRACKS; OXYGEN; SILICATE MINERALS; SULFUR COMPOUNDS; VOLCANIC ROCKS; VOLCANOES; ZIRCON;

CATHODOLUMINESCENCE IMAGES; HYDRO-THERMAL EXCHANGES; HYDROTHERMAL ALTERATIONS; MAGMATIC PROCESS; OXYGEN ISOTOPE RATIOS; PARTIAL MELTING; QUARTZ PHENOCRYSTS; VOLCANOGENIC MASSIVE SULFIDE DEPOSITS;

QUARTZ;

HYDROTHERMAL ALTERATION; MAGMATISM; MASSIVE SULFIDE; OXYGEN ISOTOPE; PARTIAL MELTING; PHENOCRYST; QUARTZ; RECRYSTALLIZATION; RHYOLITE; ZIRCON; HYDROTHERMAL PROCESSES;

CANADA; KIDD CREEK; ONTARIO [CANADA]; ONTARIO;

EID: 0031420305     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1997)025<1079:HAOOIR>2.3.CO;2     Document Type: Article

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