A model for the formation of transient event plumes above mid‐ocean ridge hydrothermal systems

E-ISSN： 2156-2202|102|B6|12109-12121

ISSN： 0148-0227

Source： Journal Of Geophysical Research, Vol.102, Iss.B6, 1997-06, pp. : 12109-12121

Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.

Previous Menu Next

Related content

Dynamics and storage of brine in mid‐ocean ridge hydrothermal systems

Journal Of Geophysical Research, Vol. 111, Iss. B6, 2006-06 ,pp. : n/a-n/a

John Wiley & Sons Inc

Access to resources Recommend Favorite

Laboratory studies of high Rayleigh number circulation in an open‐top Hele‐Shaw cell: An analog to mid‐ocean ridge hydrothermal systems

Journal Of Geophysical Research, Vol. 106, Iss. B6, 2001-06 ,pp. : 10983-11000

John Wiley & Sons Inc

Access to resources Recommend Favorite

Interaction of mantle plumes and migrating mid‐ocean ridges: Implications for the Galápagos plume‐ridge system

Journal Of Geophysical Research, Vol. 102, Iss. B7, 1997-07 ,pp. : 15403-15417

John Wiley & Sons Inc

Access to resources Recommend Favorite

Near‐axis subsidence rates, hydrothermal circulation, and thermal structure of mid‐ocean ridge crests

Journal Of Geophysical Research, Vol. 106, Iss. B9, 2001-09 ,pp. : 19233-19258

John Wiley & Sons Inc

Access to resources Recommend Favorite

Cellular convection models of mid‐ocean ridge hydrothermal circulation and the temperatures of black smoker fluids

Journal Of Geophysical Research, Vol. 103, Iss. B2, 1998-02 ,pp. : 2585-2596

John Wiley & Sons Inc

Access to resources Recommend Favorite