The Study of Deep Mineral Association in Chromitites of the Hegenshan Ophiolite, Inner Mongolia, China
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 c...
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| Veröffentlicht in: | Acta geologica Sinica (Beijing) 2015-12, Vol.89 (s2), p.30-31 |
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| container_title | Acta geologica Sinica (Beijing) |
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| creator | HUANG, Zhu YANG, Jingsui ZHU, Yongwang XIONG, Fahui LIU, Zhao ZHANG, Zhongming XU, Wei |
| description | 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. |
| doi_str_mv | 10.1111/1755-6724.12308_21 |
| format | Article |
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| source | Wiley Online Library Journals Frontfile Complete; Alma/SFX Local Collection |
| title | The Study of Deep Mineral Association in Chromitites of the Hegenshan Ophiolite, Inner Mongolia, China |
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