Volume 24 Issue 4
Aug.  2018
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JIA Limin, LIU Hongzhang, JU Jiaxing, et al., 2018. PROTOLITH RECONSTRUCTION AND GEOTECTONIC ENVIRONMENTAL RESEARCH OF XINGHUADUKOU ROCK GROUP IN LVLIN FORESTRY CENTER, DAXING'ANLING. Journal of Geomechanics, 24 (4): 544-554. DOI: 10.12090/j.issn.1006-6616.2018.24.04.057
Citation: JIA Limin, LIU Hongzhang, JU Jiaxing, et al., 2018. PROTOLITH RECONSTRUCTION AND GEOTECTONIC ENVIRONMENTAL RESEARCH OF XINGHUADUKOU ROCK GROUP IN LVLIN FORESTRY CENTER, DAXING'ANLING. Journal of Geomechanics, 24 (4): 544-554. DOI: 10.12090/j.issn.1006-6616.2018.24.04.057

PROTOLITH RECONSTRUCTION AND GEOTECTONIC ENVIRONMENTAL RESEARCH OF XINGHUADUKOU ROCK GROUP IN LVLIN FORESTRY CENTER, DAXING'ANLING

doi: 10.12090/j.issn.1006-6616.2018.24.04.057
More Information
  • Received: 2017-11-26
  • Revised: 2018-05-12
  • Published: 2018-08-28
  • Xinghuadukou Rock Group, as the basement of Ergun massif, its metamorphic age, protolith types and geotectonic setting has always been a hot spot for geologists. With Xinghuadukou Rock Group in lvlin forestry center, north part of Daxing'anling, as the research object, zircons U-Pb isotopic dating was used to define the metamorphic age of protolith. Protolith reconstruction was carried out combining with the comprehensive analysis methods of petrography and geochemistry, and its geotectonic setting was further discussed. The resarch suggests that Xinghuadukou Rock Group is mainly composed of amphibolite, leptite, granulite and quartzite. The protolith of these four kinds respectively are basic volcanic rock, dacite tuff, pelitic siltstone and pelitic siltstone. Amphibolite is lack of non-active trace elements Ta、Nd、P, and it belongs to the island-arc geotectonic environment. Leptite mainly lacks Ta、Nd、P、Sr、Ti and other elements, and it is formed in the orogenic belt environment of continental margin. The lower limit of metamorphic age of Xinghuadukou Rock Group in Lvlin forestry center is 774.1±3.8 Ma.

     

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