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...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Mongolian University of Science and Technology
2020-06-01
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| Series: | Mongolian Geoscientist |
| Subjects: | |
| Online Access: | https://www.mongoliajol.info/index.php/MGS/article/view/1327 |