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LIANG Shuai, ZHAI Furong, DAI Huimin, ZHANG Yanfei, LIU Kai, ZHONG Mishan, CHEN Yao, LIU Jinqing, YU Xinyang. 2022. Geological structural characteristics and tectonic period in Daguitun area, southern Heilongjiang[J]. Geology in China, 49(2): 631-642. doi: 10.12029/gc20220219
Citation: LIANG Shuai, ZHAI Furong, DAI Huimin, ZHANG Yanfei, LIU Kai, ZHONG Mishan, CHEN Yao, LIU Jinqing, YU Xinyang. 2022. Geological structural characteristics and tectonic period in Daguitun area, southern Heilongjiang[J]. Geology in China, 49(2): 631-642. doi: 10.12029/gc20220219
shu

Geological structural characteristics and tectonic period in Daguitun area, southern Heilongjiang

  • 1.

    Shenyang Center of China Geological Survey, Shenyang 110000, Liaoning, China

  • 2.

    Liaoning Institute of Geology and Mineral Resources Co., Ltd., Shenyang 110000, Liaoning, China

  • 3.

    Liaoning Geological Exploration Institute Co., Ltd., Dalian 116600, Liaoning, China

  • 4.

    Shandong University of Science and Technology, Qingdao 266000 Shandong China

  • 5.

    University of Florida, Homestead 33031, Miami, USA

    • Fund Project: Supported by the project of China Geological Survey "1:250, 000 Land Quality Geochemical Survey of Black Land in Northeast China" (No.121201007000161312) and "Land Quality Geochemical Survey of Xingkai Lake Plain and Western Songliao Plain" (No.DD20190520)
More Information
  • Author Bio: LIANG Shuai, male, born in 1986, doctor, senior engineer, majors in basic geological and land survey research; E-mail: ls476476@163.com
  • Corresponding author: ZHAI Furong, female, born in 1981, master, senior engineer, engages in basic geological and remote sensing in geological research; E-mail: zfr750@163.com 
Received Date:  16 August 2019
Revised Date:  30 December 2019
Publish Date:  25 April 2022
    Abstract

  • This paper is the result of geological survey engineering.

     Object

    Daguitun area in the southern of Heilongjiang Province is located in the eastern part of the Songnen-Zhangguangcailing block, which is the superposition and transformation site of Paleo-Asian oceanic tectonic domain and Pacific tectonic domain, It is of great theoretical significance to further analyze the superposition and transformation background of the two tectonic domains by studying the features of small or micro structures.

     Methods

    Based on systematic field investigation and microscopic identification of mineral deformation characteristics, combined with previous research results, this paper discusses the tectonic evolution history of the study area and the time limit for superposition and transformation of the two tectonic systems.

     Results

    There are three stages of tectonics in the area of Guitun: First, the Early Paleozoic paleo-Asian ocean cracking and expansion, second, the Late Permian-Early Triassic paleo-Asian ocean closing and compression orogeny, third, the Late Triassic-Early Jurassic subduction and compression orogeny of the Pacific plate on the Eurasian plate. The folds formed during the subduction period of the Pacific plate to Eurasia are obviously different from those formed during the closing compression period of the ancient Asian ocean, which not only reflects the significant differences in structural levels, but also reflects the transformation process of regional stress field.

     Conclusion

    During the subduction period of the Pacific plate to Eurasia, not only folds were formed, but also brittle fractures matched with them were formed, which provided an important scientific basis for studying the transformation between the paleo-Asian Ocean and the circum-Pacific tectonic domain, especially the subduction history of the paleo-Pacific plate to Eurasia.
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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