Article ID Journal Published Year Pages File Type
6441054 Lithos 2011 11 Pages PDF
Abstract
► Clinopyroxene inclusions were found in chromite of the Gaositai Alaskan-type complex. ► The parent magma was high in Mg# (>90) and CaO, but depleted in Nb and Ti. ► The parent magma was a typical arc ankaramite. ► The Gaositai complex originated from a hydrous-carbonatite fluxed lithospheric mantle above a subduction zone.
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Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Petrology and geochemistry of dunites, chromitites and mineral inclusions from the Gaositai Alaskan-type complex, North China Craton: Implications for mantle source characteristics
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