An Intra-Oceanic Subduction System Influenced by Ridge Subduction in the Diyanmiao Subduction Accretionary Complex of the Xar Moron Area, Eastern Margin of the Central Asian Orogenic Belt

Yang Cheng; Qinghui Xiao; Tingdong Li; Liquan Xu; Yuxu Fan; Yan Li; Lingjun Guo; Jinli Pang; Weiming Yuan

doi:10.1007/s12583-021-1404-4

Volume 32 Issue 1

Mar 2021

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Journal of Earth Science > 2021 > 32(1): 253-266.

Yang Cheng, Qinghui Xiao, Tingdong Li, Liquan Xu, Yuxu Fan, Yan Li, Lingjun Guo, Jinli Pang, Weiming Yuan. An Intra-Oceanic Subduction System Influenced by Ridge Subduction in the Diyanmiao Subduction Accretionary Complex of the Xar Moron Area, Eastern Margin of the Central Asian Orogenic Belt. Journal of Earth Science, 2021, 32(1): 253-266. doi: 10.1007/s12583-021-1404-4

Citation:

Yang Cheng, Qinghui Xiao, Tingdong Li, Liquan Xu, Yuxu Fan, Yan Li, Lingjun Guo, Jinli Pang, Weiming Yuan. An Intra-Oceanic Subduction System Influenced by Ridge Subduction in the Diyanmiao Subduction Accretionary Complex of the Xar Moron Area, Eastern Margin of the Central Asian Orogenic Belt. Journal of Earth Science, 2021, 32(1): 253-266. doi: 10.1007/s12583-021-1404-4

Citation:

Yang Cheng, Qinghui Xiao, Tingdong Li, Liquan Xu, Yuxu Fan, Yan Li, Lingjun Guo, Jinli Pang, Weiming Yuan. An Intra-Oceanic Subduction System Influenced by Ridge Subduction in the Diyanmiao Subduction Accretionary Complex of the Xar Moron Area, Eastern Margin of the Central Asian Orogenic Belt. Journal of Earth Science, 2021, 32(1): 253-266. doi: 10.1007/s12583-021-1404-4

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An Intra-Oceanic Subduction System Influenced by Ridge Subduction in the Diyanmiao Subduction Accretionary Complex of the Xar Moron Area, Eastern Margin of the Central Asian Orogenic Belt

doi: 10.1007/s12583-021-1404-4

1.
Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 101300, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Inner Mongolia Key Laboratory of Magmatic Mineralization and Ore-Prospecting, Hohhot 010020, China
4.
General Prospecting Institute, China National Administration of Coal Geology, Beijing 100039, China

More Information

Corresponding author: Qinghui Xiao, chengyang1104@126.com
Received Date: 09 Sep 2020
Accepted Date: 11 Dec 2020
Publish Date: 01 Feb 2021

Abstract

Abstract

This study focuses on the geology,geochemistry,Sr-Nd isotopes and their tectonic settings of three types of basalts in Diyanmiao ophiolite in the Xar Moron area located on the eastern margin of the Central Asian Orogenic Belt. Type Ⅰ basalts are oceanic tholeiites with a depleted light rare earth element (LREE) pattern,which are similar to the typical N-mid-oceanic ridge basalt (MORB) and suggests that they were formed at a mid-oceanic ridge. The initial ⁸⁷Sr/⁸⁶Sr ratios of Type Ⅰ basalts range from 0.703 966 to 0.705 276 and the ε_Nd(t) values are from 16.49 to 17.15,indicating that they were derived from a depleted mantle source. Type Ⅱ basalts belong to the medium-potassium calc-akaline series and have the geochemical characteristics of Nb-enriched basalt (NEB) with high Nb content (14.5 ppm) and strong enrichment in LREEs,implying that they were created by the partial melting of mantle wedge peridotite that previously metasomatized by slab melts. Type Ⅲ basalts are high-Al basalt (HAB) with high-Al contents (Al₂O₃=16.75 wt.%-18.00 wt.%),distinct Nb depletion and high Th/Yb ratios. Thus they were likely generated in a normal island-arc setting. Therefore,the association of MORB,NEB,and HAB in the study area may be due to the subduction of a mid-oceanic ridge,and the Diyanmiao ophiolite is proposed to be formed in the forearc setting of a mid-oceanic ridge subduction system.
- mid-oceanic ridge basalt,
- Nb-enriched basalt,
- high-Al basalt,
- ridge subduction,
- Diyanmiao ophiolite,
- Inner Mongolia

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References(75)

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