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Numerical modeling of phase separation at Main Endeavour Field, Juan de Fuca Ridge

Before being disrupted by a magmatic event in 1999, the vent temperatures and salinities along the axis of the Main Endeavour Field on the Juan de Fuca Ridge exhibited a quasi‐steady spatial gradient in which the southern vent fluids were hotter and less saline than the northern vent fluids. We pres...

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Gorde:
Xehetasun bibliografikoak
Egile Nagusiak: Shreya Singh, Robert P. Lowell, Kayla C. Lewis
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: Wiley 2013-10-01
Saila:Geochemistry, Geophysics, Geosystems
Gaiak:
Sarrera elektronikoa:https://doi.org/10.1002/ggge.20249
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