Hydrothermal fault zones in the lower oceanic crust: An example from Wadi Gideah, Samail ophiolite, Oman (2018)
Attributed to:
Hydrothermal alteration of an intact section of the upper oceanic crust formed at a superfast spreading rate
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.lithos.2018.09.008
Publication URI: http://dx.doi.org/10.1016/j.lithos.2018.09.008
Type: Journal Article/Review
Parent Publication: Lithos