The Study of Deep Mineral Association in Chromitites of the Hegenshan Ophiolite, Inner Mongolia, Chi

• 作 者: HUANG Zhu YANG Jingsui ZHU Yongwang XIONG Fahui LIU Zhao ZHANG Zhongming XU Wei
• 机 构: CARMA,State Key Laboratory of Continental Tectonics and Dynamics,Institute of Geology,Chinese Academ
• 出 处: Acta Geologica Sinica(English Edition)
• 发表日期: 2015年S2期
• 关键词: diamond Paleozoic shallow mantle Russia Polar minerals Tibet zircon Secondary

Previously reported in the Mesozonic Tibet and the early Paleozoic Polar Ural,Russia,diamond and other deep minerals are found in ophiolite mantle peridotite chromite that need to be reconsidered ophiolite and chromite traditional understanding of the causes of shallow.The ophiolitic chromitite can be divided two classes,the high-Cr chromitite and high-Al chromitite.

Previously reported in the Mesozonic Tibet and the early Paleozoic Polar Ural, Russia, diamond and other deep minerals are found in ophiolite mantle peridotite chromite that need to be reconsidered ophiolite and chromite traditional understanding of the causes of shallow. Ophiolitic chromitite can be divided two classes, the high-Cr chromitite and high-Al chromitite.