Mineralogy, Geochemistry, and Geochronology of the Yehe-Shigna Ophiolitic Massif, Tuva-Mongolian Microcontinent, Southern Siberia: Evidence for a Back-Arc Origin and Geodynamic Implications – Vide Leaf

Minerals: Technology and Advances

Mineralogy, Geochemistry, and Geochronology of the Yehe-Shigna Ophiolitic Massif, Tuva-Mongolian Microcontinent, Southern Siberia Evidence for a Back-Arc Origin and GeodynamDownload

Mineralogy-Geochemistry-and-Geochronology-of-the-Yehe-Shigna-Ophiolitic-Massif-Tuva-Mongolian-Microcontinent-Southern-Siberia-Evidence-for-a-Back-Arc-Origin-and-Geodynam