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LI Chengdong, ZHAO Ligang, XU Yawen, CHANG Qingsong, WANG Shiyan, XU Teng. Chronology of metasedimentary rocks from Kuanping Group Complex in North Qinling Belt and its geological significance[J]. GEOLOGY IN CHINA, 2018, 45(5): 992-1010. DOI: 10.12029/gc20180508
Citation: LI Chengdong, ZHAO Ligang, XU Yawen, CHANG Qingsong, WANG Shiyan, XU Teng. Chronology of metasedimentary rocks from Kuanping Group Complex in North Qinling Belt and its geological significance[J]. GEOLOGY IN CHINA, 2018, 45(5): 992-1010. DOI: 10.12029/gc20180508
shu

Chronology of metasedimentary rocks from Kuanping Group Complex in North Qinling Belt and its geological significance

  • 1.

    Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China

  • 2.

    Henan Institute of Geological Survey, Zhengzhou 450001, Henan, China

Funds: 

China Geological Survey Program DD20160043

China Geological Survey Program 12120113060900

National Natural Science Foundation of China 41272065

More Information
  • Author Bio:

    LI Chengdong, male, born in 1963, senior engineer, mainly engages in the study of orogenic belt and petrotectonics; E-mail:tjlcd99@163.com

  • Received Date: September 19, 2016
  • Revised Date: July 16, 2017
  • Available Online: September 25, 2023
    Graphical Abstract
    • Abstract

  • Kuanping Group Complex is located in North Qinling orogenic belt and consists chiefly of amphibolite of Guangdongping Formation, mica-quartzose schist of Sichakou Formation and marble of Xiewan Formation. According to recent dating of the LA-MC-ICPMS U-Pb zircons from Kuanping Group Complex in Tanghe area of Henan, their ages of detrital zircons of mica-quartzose schist from Xiewan Formation Complex range from 400Ma to 3502 Ma with a group of youngest 206Pb/238U ages between 380 and 418 Ma. Combined with(370.9±2.0) Ma metamorphic age of 40Ar/39Ar of the biotite, it is concluded that Xiewan Formation Complex was formed in the Late Devonian. And the ages of detrital zircons from Sichakou Formation Complex range similarly from 512 Ma to 3598 Ma with a group of youngest 206Pb/238U ages between 512 and 549Ma, and its metamorphic age is (370.4±1.8) Ma from biotite 40Ar/39Ar. It is thus held that Sichakou Formation Complex was formed between Middle Cambrian and Late Devonian of early Paleozoic. So Kuanping Group Complex needs further disintegration due to great difference of stratigraphic ages. The sediments were probably derived from the North China Block, the Qinling orogenic belt and the Yangtze block. The ages of biotite 40Ar/39Ar show that Kuanping Group Complex was deformed in Late Devonian, indicating the end of collision orogeny of the North Qinling Belt during Paleozoic.

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