Fluid evolution in an Oceanic Core Complex: A fluid inclusion study from IODP hole U1309 D-Atlantis Massif, 30°N, Mid-Atlantic Ridge (2014)
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/10.1002/2013gc004975
Publication URI: http://dx.doi.org/10.1002/2013gc004975
Type: Journal Article/Review
Parent Publication: Geochemistry, Geophysics, Geosystems
Issue: 4