C
Chimedtseren Anaad
Researcher at Mongolian University of Science and Technology
Publications - 18
Citations - 208
Chimedtseren Anaad is an academic researcher from Mongolian University of Science and Technology. The author has contributed to research in topics: Zircon & Volcanic rock. The author has an hindex of 9, co-authored 15 publications receiving 141 citations. Previous affiliations of Chimedtseren Anaad include American Museum of Natural History.
Papers
More filters
Journal ArticleDOI
SHRIMP zircon U-Pb ages and tectonic implications of igneous events in the Ereendavaa metamorphic terrane in NE Mongolia
TL;DR: In this paper, the Ereendavaa metamorphic terrane in NE Mongolia has been considered as a Pre-Altaid block or a Precambrian cratonic terrane with a Paleoproterozoic basement overlain by NeoproTERozoic-Cambrian rocks, but the idea has not been supported by any isotopic dating.
Journal ArticleDOI
Zircon ages and geochemical compositions of the Manlay ophiolite and coeval island arc: Implications for the tectonic evolution of South Mongolia
Mingshuai Zhu,Munkhtsengel Baatar,Laicheng Miao,Chimedtseren Anaad,Fochin Zhang,Shunhu Yang,Yueming Li +6 more
TL;DR: In this article, the authors conducted detailed studies on the Manlay ophiolitic complex and Huree volcanic rocks south of the Main Mongolian Lineament (MML) to provide some constraints on these rocks and proposed that the Early Paleozoic subduction-accretionary complexes likely constitute the basement of the Late-Paleozoic arc formations and correlate with the Lake Zone in western Mongolia.
Journal ArticleDOI
Geochronology and geochemistry of the Triassic bimodal volcanic rocks and coeval A-type granites of the Olzit area, Middle Mongolia: Implications for the tectonic evolution of Mongol–Okhotsk Ocean
Mingshuai Zhu,Fochin Zhang,Laicheng Miao,Munkhtsengel Baatar,Chimedtseren Anaad,Shunhu Yang,Xingbo Li +6 more
TL;DR: In this paper, the Olzit Late Triassic bimodal volcanic suite was shown to represent a back-arc basin extensional environment, which probably related to the roll-back of Mongol-Okhotsk oceanic plate during the southward subduction under the Central Mongolia microcontinent.
Journal ArticleDOI
Petrogenesis and tectonic implication of the Late Mesozoic volcanic rocks in East Mongolia
Amarjargal Bars,Laicheng Miao,Zhang Fochin,Munkhtsengel Baatar,Chimedtseren Anaad,Khasmaral Togtokh +5 more
TL;DR: In this paper, the authors presented new geochemical and geochronological data of the Late Mesozoic volcanic rocks in East Mongolia and showed that these volcanic rocks belong to high-K calc-alkaline and shoshonitic series and exhibit features of bimodal rocks.
Journal ArticleDOI
Cambrian Kherlen ophiolite in northeastern Mongolia and its tectonic implications: SHRIMP zircon dating and geochemical constraints
TL;DR: In this article, the Kherlen ophiolite complex and a gabbro and a plagiogranite dike intruding from the kherlen terrane were found to have crystallization ages of ca. 440 ± 1.5 million years, which is interpreted to record the minimum age of the tectonic emplacement of the OPHI.