Zobrazeno 1 - 3
of 3
pro vyhledávání: '"enriched primitive magma"'
Publikováno v:
Minerals, Vol 9, Iss 5, p 275 (2019)
The Akechukesai IV mafic−ultramafic complex, located in the western segment of the eastern Kunlun orogenic belt (EKOB), represents a newly-discovered complex, containing Ni ores at grades of up to 0.98% Ni. It is dominated by olivine pyroxenite, py
Externí odkaz:
https://doaj.org/article/1dd5a0532c7841b2a0284387d42a2145
Publikováno v:
Minerals, Vol 9, Iss 5, p 275 (2019)
Minerals
Volume 9
Issue 5
Minerals
Volume 9
Issue 5
The Akechukesai Ⅳ mafic&ndash
ultramafic complex, located in the western segment of the eastern Kunlun orogenic belt (EKOB), represents a newly-discovered complex, containing Ni ores at grades of up to 0.98% Ni. It is dominated by olivine pyro
ultramafic complex, located in the western segment of the eastern Kunlun orogenic belt (EKOB), represents a newly-discovered complex, containing Ni ores at grades of up to 0.98% Ni. It is dominated by olivine pyro
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