Zircon U–Pb geochronology and geochemistry of granitic rocks in central Mongolia

Zircon U–Pb geochronology and geochemistry of granitic rocks in central Mongolia

The Central Asian Orogenic Belt had been formed by amalgamation of voluminous subduction–accretionary complexes during the Late Neoproterozoic to the Mesozoic period. Mongolia is situated in the center of this belt. This study presents new zircon U–Pb geochronological, whole-rock major and trace ele...

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Bibliographic Details
Main Authors: Boldbaatar Dolzodmaa, Yasuhito Osanai, Nobuhiko Nakano, Tatsuro Adachi
Format: Article
Language:English
Published: Mongolian University of Science and Technology 2020-06-01
Series:Mongolian Geoscientist
Subjects:
i-type granite
adakite
a-type granite
central asian orogenic belt
Online Access:https://www.mongoliajol.info/index.php/MGS/article/view/1327

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