Supplemental Material: Origin of composite Ni-Cu sulfide- and Fe-Ti oxide-bearing mafic-ultramafic intrusions in the Central Asian Orogenic Belt, China: Role of externally derived crustal organic carbon in controlling mineralization of post-collisional mafic magmatism

Abstract

<p>Detailed description of modeling the relationship of olivine Fo versus Ni for rocks of the Kebu intrusion, complete lithogeochemical and mineral chemical data sets, as well as geochemical modeling results.</p>