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The accretion of lower oceanic crust

2011
The formation of new ocean lithosphere at mid-ocean ridges is a fundamental component of the plate tectonic cycle, and through hydrothermal interactions with seawater is a major control on the composition of the oceans, ocean crust, and upper mantle. Two complementary approaches are used to investigate the thermal implications of endmember theoretical ...
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Hydrothermal alteration in the lower oceanic crust [PDF]

open access: possible, 2019
Hydrothermal circulation is a fundamental process for chemical and isotopic exchange between the solid Earth and oceans and for the extraction of heat from newly accreted crust at mid-ocean ridges. However, due to a dearth of samples from modern oceanic crust and ophiolites, there remain major short-comings in our understanding of hydrothermal ...
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Mobilization of Cu in the continental lower crust: A perspective from Cu isotopes

Geoscience Frontiers, 2023
Chen-Hao Luo, Rui Wang, Noreen Evans
exaly  

lower crust

2014
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