额尔古纳地块早-中三叠世安山岩的发现及其对蒙古-鄂霍茨克洋南向俯冲的指示

李强; 程学芹; 陈伟; 刘洪章; 张涛; 张建珍; 贾立民; 杨宁; 刘腾飞

doi:10.3799/dqkx.2020.319

Volume 46 Issue 8

Aug. 2021

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Article Navigation > Earth Science > 2021 > 46(8): 2768-2785

Li Qiang, Cheng Xueqin, Chen Wei, Liu Hongzhang, Zhang Tao, Zhang Jianzhen, Jia Limin, Yang Ning, Liu Tengfei, 2021. Discovery of Early-Middle Triassic Andesite in Erguna Massif and Its Indication of Southward Subduction of Mongol-Okhotsk Ocean Plate. Earth Science, 46(8): 2768-2785. doi: 10.3799/dqkx.2020.319

Citation:

Li Qiang, Cheng Xueqin, Chen Wei, Liu Hongzhang, Zhang Tao, Zhang Jianzhen, Jia Limin, Yang Ning, Liu Tengfei, 2021. Discovery of Early-Middle Triassic Andesite in Erguna Massif and Its Indication of Southward Subduction of Mongol-Okhotsk Ocean Plate. Earth Science, 46(8): 2768-2785. doi: 10.3799/dqkx.2020.319

Citation:

Li Qiang, Cheng Xueqin, Chen Wei, Liu Hongzhang, Zhang Tao, Zhang Jianzhen, Jia Limin, Yang Ning, Liu Tengfei, 2021. Discovery of Early-Middle Triassic Andesite in Erguna Massif and Its Indication of Southward Subduction of Mongol-Okhotsk Ocean Plate. Earth Science, 46(8): 2768-2785. doi: 10.3799/dqkx.2020.319

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Discovery of Early-Middle Triassic Andesite in Erguna Massif and Its Indication of Southward Subduction of Mongol-Okhotsk Ocean Plate

doi: 10.3799/dqkx.2020.319

1.
Regional Geological Survey Institute of Hebei Province, Langfang 065000, China
2.
MNR Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2020-08-15
Publish Date: 2021-08-01

Abstract

Abstract

The andesite is closely related to the subduction tectonic environment,and the study of andesite can obtain important information about the age of subduction and related subduction processes. In this paper it presents petrographic characteristics,whole-rock geochemical data and zircon U-Pb ages of the Early to Middle Triassic andesites from the Fengshui Mountain area in the Erguna massif in the northern Great Xing'an Range for the purpose of revealing the initial southward subduction of the Mongol-Okhotsk oceanic plate. Most of the zircons from the andesite in the Fengshui Mountain area are euhedral to subhedral in shape,with typical oscillating growth zonation and relatively high Th/U ratios (0.23-1.34),indicative of magmatic zircons. Zircon LA-ICP-MS U-Pb dating yields two ages of 251±2 Ma and 243±2 Ma for andesite in the Fengshui Mountain area,indicative of Early and Middle Triassic ages for the andesites. These Early Mesozoic andesites have typical geochemical characteristics of active continental margin arc magmatite with SiO₂,Al₂O₃,K₂O,Na₂O,Fe₂O₃^T,MgO,TiO₂ and total alkali (K₂O+Na₂O) contents ranging from 53.52% to 60.38%,16.17% to 17.41%,1.60% to 4.60%,3.83% to 4.65%,5.55% to 8.93%,1.96% to 5.97%,0.97% to 1.67%,and 5.60% to 8.05%,respectively. These andesites are high K calc-alkaline with Na₂O/K₂O ratios ranging from 1.23 to 2.51,A/CNK values (aluminum saturation index) from 0.86 to 0.97 and Mg^# values ranging from 47 to 75. These volcanic rocks are enriched in large ionic lithophile elements such as Rb,Ba,U,K,Pb and light rare earth elements,but depleted in high field strength elements such as Nb,Ta,Ti,P and heavy rare earth elements,with weak negative Eu anomaly (δEu=0.74-0.99). These Early Mesozoic andesitic rocks are geochemically similar to the typical andesites in Andean,thus indicating that they are most likely formed in the Andean-type active continental margin environment related to the southward subduction of the Mongol-Okhotsk oceanic plate.
- northern Great Xing'an Range,
- Erguna massif,
- Early to Middle Triassic andesite,
- zircon U-Pb age,
- Mongolia-Okhotsk Ocean,
- petrogenesis,
- geochronology,
- geochemistry

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References(124)

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Discovery of Early-Middle Triassic Andesite in Erguna Massif and Its Indication of Southward Subduction of Mongol-Okhotsk Ocean Plate

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