
Otgon-Erdene Davaasuren- Doctor of Philosophy
- PostDoc Position at Korea Institute of Geoscience and Mineral Resources
Otgon-Erdene Davaasuren
- Doctor of Philosophy
- PostDoc Position at Korea Institute of Geoscience and Mineral Resources
About
14
Publications
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17
Citations
Introduction
Current institution
Additional affiliations
July 2009 - February 2015
Mineral Resources Authority of Mongolia
Position
- Officer of Geological Division
Publications
Publications (14)
Small‐ to medium‐sized serpentinized ultramafic blocks have been found in several locations in South Korea. Ultramafic‐hosted serpentinization, described as a major hydrothermal process that affects the lithospheric mantle, is known to play a key role in mass fluxes enhanced by multiple fluid–rock interactions that ultimately lead to the formation...
We investigated the nickel potential and genesis of ultramafic rocks in the Yugu area to secure nickel resources in South Korea. The Yugu ultramafic rocks, located in the southwest of the Gyeonggi Massif, are characterized by spinel peridotite and exhibit strong serpentinization along their boundaries. The serpentinization is observed as olivine tr...
In this review, we attempted to summarize and interpret the Phanerozoic geology and mineralization following the article (vol. 71 in Resource Geology) which reviewed the Precambrian geology and mineralization of North Korea. The basement of the Korean peninsula was built during the Precambrian and gradually became more evolved and complex during th...
The Zogdor Cu occurrences are located in the Gurvansayhan island arc terrane of southern Mongolia, which corresponds to the southern part of the Central Asian Orogenic Belt (CAOB). The major porphyry type copper–gold (molybdenum) mineralized belt including Oyu Tolgoi, Tsagaan Suvarga, Shuteen, and Kharmagtai deposits are located in this terrane and...
We report fluid inclusion study results of copper-bearing quartz veins in Zogdor area, which is located within the Gurvansayhan island arc terrane of Southern Mongolia. At the Zogdor area, structure-controlled copper mineralization is hosted in granodiorite-porphyry, which emplaced in the late Cretaceous formation. Within this granodiorite porphyry...
Tsogttsetsii area, an intrusive complex associated with Cu mineralization, is located in the South Gobi, Mongolia. We performed the cross geochemical and extended exploration survey in Tsogttsetsii area. Cu mineralization in Tsogttsetsii area is porphyry Cu type related with alkali granite intruded in Late Carboniferous to Early Permian. In the con...
Since the 1970s, several prospective areas for copper mineralization have been recognized in Mongolia, stimulating further prospecting activities. The following types of copper ore formations are recognized in Mongolia: volcanic hosted Cu deposit, sediment hosted Cu deposit, skarn Cu deposit, epithermal replacement Cu-Ag and porphyry Cu-Au-Mo depos...
Tsogttsetsii area, an intrusive complex associated with Cu porphyry mineralization, is located in the Gurvansaikhan island arc terrane of the Central Asian Orogenic belt, Southern Mongolia. We performed a reconnaissance survey in Tsogttsetsii area. Cu mineralization in Tsogttsetsii area is porphyry Cu type related with alkali granite intruded in Pe...