White Island, New Zealand, volcanic-hydrothermal system represents the geochemical environment of high-sulfidation Cu and Au ore deposition

Geology ◽  
1993 ◽  
Vol 21 (8) ◽  
pp. 731 ◽  
Author(s):  
Jeffrey W. Hedenquist ◽  
Stuart F. Simmons ◽  
Werner F. Giggenbach ◽  
C. Stewart Eldridge
2005 ◽  
Vol 114 (6) ◽  
pp. 1044-1047
Author(s):  
Yuji NISHI ◽  
Nobuo MATSUSHIMA ◽  
Tsuneo ISHIDO

Eos ◽  
1989 ◽  
Vol 70 (7) ◽  
pp. 98 ◽  
Author(s):  
Werner F. Giggenbach ◽  
Jeffrey W. Hendenquist ◽  
Bruce F. Houghton ◽  
Peter M. Otway ◽  
Richard G. Allis

2015 ◽  
Vol 295 ◽  
pp. 26-42 ◽  
Author(s):  
Michael J. Heap ◽  
Ben M. Kennedy ◽  
Noémie Pernin ◽  
Laura Jacquemard ◽  
Patrick Baud ◽  
...  

2004 ◽  
Vol 25 (1) ◽  
pp. 28 ◽  
Author(s):  
Philip Butterworth

White Island (Whakaari) is New Zealand?s most active volcano. The sulphur-rich hydrothermal environment of the island is considered an analogue for early terrestrial ecosystems that supported sulphur-metabolising microorganisms.


2005 ◽  
Vol 114 (6) ◽  
pp. Plate5-Plate5
Author(s):  
Yuji NISHI ◽  
Nobuo MATSUSHIMA ◽  
Tsuneo ISHIDO

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