Multi-stage fluid infiltration and metasomatism in supra-subduction zone mantle: evidence from halogens and noble gases in the Leka Ophiolite Complex, Norway (2021)
Attributed to:
Scales of preservation and root causes of mantle heterogeneities in the Iapetan Ocean convecting upper mantle
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1016/j.gca.2021.04.028
Publication URI: http://dx.doi.org/10.1016/j.gca.2021.04.028
Type: Journal Article/Review
Parent Publication: Geochimica et Cosmochimica Acta