Oceanic crust is the uppermost layer of the oceanic portion of the tectonic plates. It is composed of the upper oceanic crust, with pillow lavas and a dike complex, and the lower oceanic crust, composed of troctolite, gabbro and ultramafic cumulates. The crust overlies the rigid uppermost layer of the mantle. The crust and the rigid upper mantle layer together constitute oceanic lithosphere.
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Boostlane is a media platform that aims to revolutionize how we research, discover, and learn about our favorite topics
Boostlane relies on the power of Artificial Intelligence and a Community of Researchers to curate and deliver reliable, insightful, and purposeful knowledge
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