小兴安岭西北部科洛杂岩的岩石学与年代学

那福超; 付俊彧; 宋维民; 刘英才; 汪岩; 葛锦涛; 孙巍; 杨帆; 张广宇; 钟辉

doi:10.3799/dqkx.2019.083

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3265-3278

Na Fuchao, Fu Junyu, Song Weimin, Liu Yingcai, Wang Yan, Ge Jintao, Sun Wei, Yang Fan, Zhang Guangyu, Zhong Hui, 2019. Petrological and Geochronological Study of Keluo Complex in Northwestern Lesser Xing'an Range. Earth Science, 44(10): 3265-3278. doi: 10.3799/dqkx.2019.083

Citation:

Na Fuchao, Fu Junyu, Song Weimin, Liu Yingcai, Wang Yan, Ge Jintao, Sun Wei, Yang Fan, Zhang Guangyu, Zhong Hui, 2019. Petrological and Geochronological Study of Keluo Complex in Northwestern Lesser Xing'an Range. Earth Science, 44(10): 3265-3278. doi: 10.3799/dqkx.2019.083

Citation:

Na Fuchao, Fu Junyu, Song Weimin, Liu Yingcai, Wang Yan, Ge Jintao, Sun Wei, Yang Fan, Zhang Guangyu, Zhong Hui, 2019. Petrological and Geochronological Study of Keluo Complex in Northwestern Lesser Xing'an Range. Earth Science, 44(10): 3265-3278. doi: 10.3799/dqkx.2019.083

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Petrological and Geochronological Study of Keluo Complex in Northwestern Lesser Xing'an Range

doi: 10.3799/dqkx.2019.083

Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China

Received Date: 2019-04-17
Publish Date: 2019-11-11

Abstract

Abstract

Due to the lack of chronological data to constrain the material composition and protolithic age of the Keluo complex, and the lack of chronological date matching the knowledge of the industry scholars, in this study, based on the systematic analysis of different genesis zircon characteristics, genesis and isotopic chronologic results of metamorphic rocks from Keluo complex in northwestern Lesser Xing'an Range, the protolith and metamorphic period of Keluo complex was studied. The LA-ICP-MS magmatic zircon U-Pb ages of three metamorphic rocks (including weak gneissic amphibolite, biotite plagioclase gneiss and biotite amphibole plagioclase gneiss) show that the youngest clastic zircons ages are 286.3±3.6 Ma, 284.3±3.1 Ma and 345.3±4.8 Ma, respectively, which means they formed in Early Permian and Early Carboniferous instead of the Precambrian. Age data also show that the source of clastic sedimentary rocks in Keluo complex is regional basement debris with widely developed two-stage magmatic rocks. Meanwhile, the LA-ICP-MS U-Pb ages of metamorphic zircons indicate that the protolith of Keluo complex underwent at least two-stage metamorphism after diagenesis, the Early-Middle Triassic(peak age 248.5 Ma) and the Early-Middle Jurassic (peak age 173.1 Ma) respectively. The early metamorphism may be a long-range effect of the southward subduction of the Mongolia-Okhotsk plate, while the late metamorphism was controlled by the superposition of the southward subduction of the Mongolia-Okhotsk Ocean and the westward subduction of the paleo-Pacific Ocean.
- Lesser Xing'an Range,
- Keluo complex,
- chronology,
- metamorphism,
- petrology

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References(63)

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Petrological and Geochronological Study of Keluo Complex in Northwestern Lesser Xing'an Range

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