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Geochemistry of Igneous Oceanic Crust by Felipe Jop is a document available to read on EtoBox.

What is Geochemistry of Igneous Oceanic Crust about?

The oceanic crust consists of four main layers from top to bottom: 1) basaltic lava flows and pillows that make up the upper ocean crust; 2) a sheeted dike complex underneath the lava flows; 3) a thick gabbroic layer below the dikes; and 4) ultramafic rocks of the lower crust and upper mantle. New ocean crust forms as mantle melt is focused toward mid-ocean ridges, forming a shallow melt lens overlying a wider mush zone that extends into the crust. Cooling of the melt lens and mush zone leads to crystalliza

Author
Felipe Jop
Language
EN