辽宁宽甸地区辽河群里尔峪组基性火山岩锆石U-Pb年代学及其地质意义

陈井胜; 田德欣; 邢德和; 李斌; 刘淼; 杨帆; 杨中柱

doi:10.3799/dqkx.2020.150

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3282-3294

Chen Jingsheng, Tian Dexin, Xing Dehe, Li Bin, Liu Miao, Yang Fan, Yang Zhongzhu, 2020. Zircon U-Pb Geochronology and Its Geological Significance of the Basic Volcanic Rocks from the Li'eryu Formation, Liaohe Group in Kuandian Area, Liaoning Province. Earth Science, 45(9): 3282-3294. doi: 10.3799/dqkx.2020.150

Citation:

Chen Jingsheng, Tian Dexin, Xing Dehe, Li Bin, Liu Miao, Yang Fan, Yang Zhongzhu, 2020. Zircon U-Pb Geochronology and Its Geological Significance of the Basic Volcanic Rocks from the Li'eryu Formation, Liaohe Group in Kuandian Area, Liaoning Province. Earth Science, 45(9): 3282-3294. doi: 10.3799/dqkx.2020.150

Citation:

Chen Jingsheng, Tian Dexin, Xing Dehe, Li Bin, Liu Miao, Yang Fan, Yang Zhongzhu, 2020. Zircon U-Pb Geochronology and Its Geological Significance of the Basic Volcanic Rocks from the Li'eryu Formation, Liaohe Group in Kuandian Area, Liaoning Province. Earth Science, 45(9): 3282-3294. doi: 10.3799/dqkx.2020.150

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Zircon U-Pb Geochronology and Its Geological Significance of the Basic Volcanic Rocks from the Li'eryu Formation, Liaohe Group in Kuandian Area, Liaoning Province

doi: 10.3799/dqkx.2020.150

1.
Shenyang Center of China Geological Survey, Shenyang 110034, China
2.
Non-Ferrous Metals Geological Exploration Bureau of Zhejiang Province, Shaoxing, 312000, China

Received Date: 2020-03-31
Publish Date: 2020-09-15

Abstract

Abstract

The formation age and evolution of the Liaohe Group in the Liao-Ji Paleoproterozoic structural belt have always been a research hotspot. Zircon LA-ICP-MS U-Pb geochronology of basic volcanic rocks intercalated in metamorphic sedimentary rocks of the Li'eryu Formation in Kuandian area is studied. Zircons from seven basic magmatic rocks are divided into magmatic zircons and metamorphic zircons. The dating results show two stages of 2 150－2 130 Ma and 2 050－2 020 Ma, representing the diagenetic age of the rocks. Combined with the acid volcanic rocks exposed in this area, it is considered that the formation age of the Liaohe Group in Kuandian area is at least 2.17－2.03 Ga. The metamorphic ages obtained from five amphibolites show that the metamorphism occurred after 1 900 Ma and lasted from 1 870 to 1 780 Ma, which can be further divided into three phases: 1 870－1 861 Ma, 1 845－1 842 Ma and 1 790－1 780 Ma. The peak period of metamorphism is ~1 850 Ma, which is the second strong metamorphic peak period of Paleoproterozoic in this area. The third stage is consistent with the metamorphic event of ~1 800 Ma. The age of meta diorite (D015) vein is 1 314±24 Ma and metamorphic age of amphibolite (D1465-1) is 1 290±21 Ma. This is the first time that Mesoproterozoic magma and metamorphism events have been identified in eastern Liaoning. Combined with 1 320－1 380 Ma magmatic activity in western Liaoning and northern Hebei, these events are considered as the response of North China Craton to the breakup process of Columbia supercontinent.
- Liaohe Group,
- Li'eryu Formation,
- basic volcanic rocks,
- zircon U-Pb chronology,
- petrology

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