Zobrazeno 1 - 10
of 25
pro vyhledávání: '"Batkhishig Bayaraa"'
Autor:
Batkhishig Bayaraa
Publikováno v:
Mongolian Geoscientist, Vol 28, Iss 56 (2023)
No English abstract
Externí odkaz:
https://doaj.org/article/7690428ad9a14973b773f8da5d383490
Publikováno v:
Mongolian Geoscientist, Vol 27, Iss 55, Pp 18-40 (2022)
The Edren range of the Trans-Altai zone is situated in the central south part of the Central Asian Orogenic Belt. The Edren range is composed primarily of volcano-sedimentary rocks that were weakly metamorphosed during the Devonian to Carboniferous p
Externí odkaz:
https://doaj.org/article/ea49aa97252b400ab9031a366d128bb7
Autor:
Batkhishig Bayaraa
Publikováno v:
Mongolian Geoscientist, Vol 28, Iss 56, Pp i-i (2023)
no abstract in English
Externí odkaz:
https://doaj.org/article/d5792a32851043b991a45a2a3d4017e8
Publikováno v:
Mongolian Geoscientist, Vol 27, Iss 54, Pp i-i (2022)
No abstract in English
Externí odkaz:
https://doaj.org/article/b583fa309e1740d4a724cca858658ca9
Publikováno v:
Mongolian Geoscientist, Iss 47, Pp 5-21 (2018)
The late Paleozoic magmatic rocks are widely distributed in the Mandakh area which is located in the Gurvansaikhan and Manlai terrains, where porphyry Cu deposits occur. In this paper we discuss petrochemical features and mineral assemblages of magma
Externí odkaz:
https://doaj.org/article/a985ff9ec1734b26a2fd311a8eddd1fd
Autor:
Batkhishig Bayaraa
Publikováno v:
Mongolian Geoscientist, Vol 51, Pp i-i (2020)
No abstract in English
Externí odkaz:
https://doaj.org/article/b6bb6d0ec42e473abfe7bac0ec8f93c4
Publikováno v:
Mongolian Geoscientist, Iss 49, Pp 1-1 (2019)
No Abstract in English
Externí odkaz:
https://doaj.org/article/5e49c68dd7414e419b9bbef98354e9a6
Autor:
Batkhishig Bayaraa
Publikováno v:
Mongolian Geoscientist, Iss 47, Pp 4-4 (2018)
No abstract in English
Externí odkaz:
https://doaj.org/article/f981eb4a5c0c42d587aa8ae0d8f0600e
Publikováno v:
In Journal of Asian Earth Sciences 2010 37(5):399-411
Publikováno v:
Mongolian Geoscientist, Iss 47, Pp 5-21 (2018)
The late Paleozoic magmatic rocks are widely distributed in the Mandakh area which is located in the Gurvansaikhan and Manlai terrains, where porphyry Cu deposits occur. In this paper we discuss petrochemical features and mineral assemblages of magma