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Serpentinite protrusions in the oceanic crust
Earth and Planetary Science Letters, 1976Abstract Serpentinite may be a significant component of the oceanic crust, not as a continuous layer, but as vertical tectonic protrusions and sills emplaced from the upper mantle into fault zones parallel to the axis of spreading ridges. The diapiric emplacement of serpentinite bodies occurs within 100–200 km of ridge axis, with a rate of ascent on ...
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Morpho-structural, adsorption and electrochemical characteristics of serpentinite
Separation and Purification Technology, 2016Jelena S Đorđević +2 more
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