The internal structure of an active sea-floor massive sulphide deposit

[1]  M. Hannington,et al.  Deducing patterns of fluid flow and mixing within the TAG active hydrothermal mound using mineralogical and geochemical data , 1995 .

[2]  P. Rona,et al.  A special issue on sea-floor hydrothermal mineralization; new perspectives; preface , 1993 .

[3]  C. V. Raman,et al.  Active and relict sea-floor hydrothermal mineralization at the TAG hydrothermal field, Mid-Atlantic Ridge , 1993 .

[4]  M. Hannington,et al.  Relict hydrothermal zones in the TAG Hydrothermal Field, Mid‐Atlantic Ridge 26°N, 45°W , 1993 .

[5]  Y. Fouquet,et al.  New age data for Mid‐Atlantic Ridge hydrothermal sites: TAG and Snakepit chronology revisited , 1993 .

[6]  P. Rona,et al.  Geochronology of TAG and Snakepit hydrothermal fields, Mid-Atlantic Ridge: witness to a long and complex hydrothermal history , 1990 .

[7]  A. C. Campbell,et al.  Chemistry of hot springs on the Mid-Atlantic Ridge , 1988, Nature.

[8]  S. Humphris,et al.  Active vents and massive sulfides at 26 degrees N (TAG) and 23 degrees N (Snakepit) on the Mid-Atlantic Ridge , 1988 .

[9]  P. Rona,et al.  Black smokers, massive sulphides and vent biota at the Mid-Atlantic Ridge , 1986, Nature.

[10]  J. Cann,et al.  A fracture-loop thermal balance model of black smoker circulation , 1986 .

[11]  J. Cann,et al.  A model of hydrothermal circulation in fault zones at mid-ocean ridge crests , 1982 .

[12]  L. Parson,et al.  Hydrothermal vents and processes , 1995, Geological Society, London, Special Publications.

[13]  M. Talwani,et al.  Deep Drilling Results in the Atlantic Ocean: Ocean Crust , 1979 .