Journal of Jilin University(Earth Science Edition) ›› 2015, Vol. 45 ›› Issue (1): 61-80.doi: 10.13278/j.cnki.jjuese.201501106

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Provenance-Sedimentary System and Tectonic Setting of First Member of Nantun Formation in Wuerxun Depression of Hailar Basin

Zhao Xiaoqing1,2, Cheng Rihui2, Yu Zhenfeng2,3, Sun Fengxian1, Wang Peng1, Gao Huijun1   

  1. 1. Well Logging Company, Daqing Drilling and Exploration Engineering Corporation, Daqing 163412, Heilongjiang, China;
    2. College of Earth Sciences, Jilin University, Changchun 130061, China;
    3. Key Laboratory of National Energy Coal and Coal Bed Methane Joint Mining Technology, Shanxi Jincheng Anthracite Mining Group Company Limited, Jincheng 048012, Shanxi, China
  • Received:2014-05-06 Published:2015-01-26

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Abstract:

Fracture and volcanism were intensive in First Member of Nantun Formation of Wunan depression in Hailar basin, due to the diversity of detritus. The composition of clastic were metamorphic clastic, pyroclastic and general erosion detrital. The diversity of detritus makes lithology and division have the distinct characteristics. The study of mineral association, cathode luminescence and heavy mineral assemblage shows that the study area can be divided into four single lithology areas and two mixed areas among them. Four single lithology areas are sedimentary rocks area with metamorphic rocks clastics, pyroclastic sedimentary rocks area, welded pyroclastic rocks area and pyroclastic rocks area. According to the contents and components of clastics in rocks, mixed area can be divided into two mixed areas:the area with normal sedimentary clastic was dominant and the area with pyroclastic was dominant. Each single lithology area corresponds with each tectonic unit. The sedimentary rocks area with metamorphic rocks clastics corresponds to Wuxi fault terrace belt, the pyroclastic rocks area correspond to Bayantala structural belt, and pyroclastic sedimentary rocks area is part of Wudong arc structural belt. Geochemical data reveal that magma of source rocks is granitoid magma of crust source, meanwhile be contaminated by magma of mantle-derived, and heavy rare earth elements are enrichment. In Wuxi fault terrace belt, total content of rare earth elements is high and negative anomaly of Eu is not obvious, so the crust-mantle contamination of source rocks magma is heavy. In Bayantala structural belt, total content of rare earth elements is low and negative anomaly of Eu is obvious, so the crust-mantle contamination of source rocks magma is medium. In Wudong arc structural belt, total content of rare earth elements is high and negative anomaly of Eu is obvious, so the crust-mantle contamination of source rocks magma is low. Dickinson graphics of sandstone composition reveal that source regions of Wudong arc structural belt has not deeply cut, and source region of Bayantala structural belt has deeply cut. Noral-slip of Derbgan fault led tectonic gneiss of Chaigang to be developed and Chaigang to uplift relatively, which become erosion area and provided Wuxi fault terrace belt with metamorphic sediments, shaped the sedimentary system of fan delta with metamorphic clastic, meanwhile the fracture provided a channel for the mantle-derived magma rising. Extension slip of Bayantala fault made the rise of mantle-derived magma and volcanic eruption, developed a set of rocks between fusion sintering pyroclastic rock and pyroclastic sedimentary rock, and shaped the sedimentary system of fan delta with pyroclastic. The crust-mantle contamination degree of Bayanshan uplift was low, but underplateing of mantle-derived magma made strong crystallization differentiation, volcanic activity and surface uplift, developed pyroclastic rocks and shaped sedimentary system of delta in Wudong arc structural belt.

Key words: Hailar basin, Wunan depression, First Member of Nantun Formation, provenance, sedimentary system, tectonic setting

CLC Number: 

  • P588.14

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