Detachment fault control on hydrothermal circulation systems: Interpreting the subsurface beneath the TAG hydrothermal field using the isotopic and geological evolution of oceanic core complexes in the Atlantic
Attributed to:
Mechanisms of fluid penetration into gabbroic crust, IODP Site 1309, mid-Atlantic Ridge.
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1029/2008gm000729
Publication URI: http://dx.doi.org/10.1029/2008gm000729
Type: Book Chapter
Book Title: Diversity of Hydrothermal Systems on Slow Spreading Ocean Ridges (2010)
Page Reference: 207-239
ISBN: 978-0-87590-478-8