Multi-stage serpentinization of ultramafic rocks in the Manlay Ophiolite, southern Mongolia
Serpentinization of ultramafic rocks in ophiolites is key to understanding the global cycle of elements and changes in the physical properties of lithospheric mantle. Mongolia, a central part of the Central Asian Orogenic Belt (CAOB), contains numerous ophiolite complexes, but the metamorphism of ul...
Main Authors: | , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Mongolian University of Science and Technology
2021-12-01
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Series: | Mongolian Geoscientist |
Subjects: | |
Online Access: | https://www.mongoliajol.info/index.php/MGS/article/view/1787 |