scholarly journals High-resolution three-dimensional simulations of mid-ocean ridge hydrothermal systems

Author(s):  
D. Coumou ◽  
T. Driesner ◽  
S. Geiger ◽  
A. Paluszny ◽  
C. A. Heinrich
1995 ◽  
Vol 100 (A12) ◽  
pp. 23779 ◽  
Author(s):  
Zi-Ping Sun ◽  
R. P. Turco ◽  
R. L. Walterscheid ◽  
S. V. Venkateswaran ◽  
P. W. Jones

Eos ◽  
1999 ◽  
Vol 80 (16) ◽  
pp. 181 ◽  
Author(s):  
S. C. Singh ◽  
M. C. Sinha ◽  
A. J. Harding ◽  
G. M. Kent ◽  
P. J. Barton ◽  
...  

2009 ◽  
Vol 10 (5) ◽  
pp. n/a-n/a ◽  
Author(s):  
Fabrice J. Fontaine ◽  
William S. D. Wilcock ◽  
Dionysis E. Foustoukos ◽  
David A. Butterfield

Elements ◽  
2020 ◽  
Vol 16 (6) ◽  
pp. 389-394
Author(s):  
Esther M. Schwarzenbach ◽  
Matthew Steele-MacInnis

Seawater interaction with the oceanic lithosphere crucially impacts on global geochemical cycles, controls ocean chemistry over geologic time, changes the petrophysical properties of the oceanic lithosphere, and regulates the global heat budget. Extensive seawater circulation is expressed near oceanic ridges by the venting of hydrothermal fluids through chimney structures. These vent fluids vary greatly in chemistry, from the metal-rich, acidic fluids that emanate from “black smokers” at temperatures up to 400 °C to the metal-poor, highly alkaline and reducing fluids that issue from the carbonate–brucite chimneys of ultramafic-hosted systems at temperatures below 110 °C. Mid-ocean ridge hydrothermal systems not only generate signifi-cant metal resources but also host unique life forms that may be similar to those of early Earth.


1999 ◽  
Vol 523 (2) ◽  
pp. L125-L128 ◽  
Author(s):  
M. A. Aloy ◽  
J. Ma. Ibáñez ◽  
J. Ma. Martí ◽  
J.-L. Gómez ◽  
E. Müller

Sign in / Sign up

Export Citation Format

Share Document