| China Geological Survey Chinese Academy of Geological Sciences | Host |
| 科学出版社 | Publish |
| Citation: |
ZHOU Chuanfang, YANG Huaben, CAI Yanlong, ZHANG Yuanhou, JIANG Lili, WEI Xiaoyong, DUAN Mingxin, FENG Jia, WANG Bochao, ZHAO Xidong. 2021. Stratigraphic age of the Mohe Formation in the western margin of Mohe Basin and tectonic environment discrimination of provenance[J]. Geology in China, 48(3): 832-853. doi: 10.12029/gc20210313
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Stratigraphic age of the Mohe Formation in the western margin of Mohe Basin and tectonic environment discrimination of provenance
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Abstract
The Mohe Formation is widely developed in Mohe Basin which is located in the northern part of the Da Hinggan Mountains. Its formation age, provenance characteristics and tectonic background are of great geological significance for the study of the formation and evolution of the basin. Two interbeds of tuff were discovered in the Mohe Formation in the western margin of Mohe basin, Enhe-Hada area. Zircon U-Pb dating by LA-ICP-MS U-Pb method yields the weighted average ages of (158±1) Ma and (157±2) Ma respectively, indicating that the Mohe Formation rocks were formed in early Late Jurassic. The geochemical analysis of Mohe Formation sandstone shows that the content of SiO2 is high (70.20%-76.13%), the value of SiO2/Al2O3 is 4.99-5.87, and the value of K2O/Na2O is 0.59-1.62. In the chondrite-standardized diagram of rare earth elements, the curve is consistent with that of the active continental margin. In the high field strong elements and large-ion lithophile elements, the samples are enriched in Th, Hf, Rb and K, and deficit in Nb, Ta, Ti, P, Ba and Sr. The cobweb curve of trace elements is similar to that of the active continental margin. The geochemical source analysis and tectonic background discrimination show that the parent rocks of the Mohe Formation sandstone were mainly originated from the mixing of the quartzite sedimentary rocks and the acidic volcanic rocks. The ages of the detrital zircons in the sandstone coincide with the ages of the Precambrian basement and granitic rocks in the southern margin of the basin. The formation age, provenance characteristics and tectonic setting of the Mohe Formation, which is widely developed in the Mohe Basin in the north of the Great Hinggan Mountains, are of great significance to the study of the formation and evolution of the basin.
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References
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ZHOU Chuanfang, YANG Huaben, CAI Yanlong, ZHANG Yuanhou, JIANG Lili, WEI Xiaoyong, DUAN Mingxin, FENG Jia, WANG Bochao, ZHAO Xidong. 2021. Stratigraphic age of the Mohe Formation in the western margin of Mohe Basin and tectonic environment discrimination of provenance[J]. Geology in China, 48(3): 832-853. doi: 10.12029/gc20210313
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Figure 1.
Tectonic division of the northern part of the Da Hinggan Mountains (a) and geological map of the western margin of Mohe Basin (b)
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Figure 2.
The measured profile of the Mohe Formation in the western margin of Mohe Basin (PM05-3LT117)
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Figure 3.
Outcrop and microscopic photographs of Mohe Formation tuff in western margin of Mohe Basin (+)
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Figure 4.
Microscopic photographs of sandstone (a-sample WJL082; b-sample WJL083) of Mohe Formation in the western margin of Mohe Basin (+)
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Figure 5.
Typical zircon CL images and surface ages of tuff and mylonitized sandstone in Mohe Formation, western margin of Mohe Basin
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Figure 6.
Zircon U-Pb concordance age (a, c), weighted average age (b, d) and zircon U-Pb concordance age (e) and histogram (f) of mylonitized sandstone of Mohe Formation in the Western Margin of Mohe Basin
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Figure 7.
Standardized REE partition curves of sandstone chondrites (a), global average continental upper crust (b) and standard trace element cobweb maps of the primitive mantle on the western margin of Mohe Basin (c) (a、c after Sun and McDonough, 1989; b after Rudnick and Gao, 2014; d after He Zhengjun et al., 2003)
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Figure 8.
Sandstone La/Th-La/Yb(a, after Shao et al., 2001), F1-F2(b, after Roser et al., 1988), REE-La/Yb(c, after Allègre et al., 1978), Hf-La/Th of Mohe Formation in the western margin of Mohe basin(d, after Floyd et al., 1987)
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Figure 9.
Discriminant diagram of major elements (Fe2O3+MgO)-Al2O3/SiO2 (a)、(Fe2O3+MgO)-TiO2 (b)tectonic environment of the Mohe Formation sandstone in western margin of Mohe basin (after Roser et al., 1985)
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Figure 10.
La-Th-Sc、Th-Sc-Zr/10、Th-Co-Zr/10 diagrams for tectonic environment discriminant of Mohe Formation sandstone, western Margin of Mohe Basin (after Bhatia et al., 1986)