大兴安岭中段晚石炭世-早二叠世砂岩碎屑锆石LA-ICP-MS U-Pb年龄及地质意义

赵英利; 刘永江; 李伟民; 冯志强; 温泉波; 梁琛岳

doi:10.3799/dqkx.2018.613

Volume 43 Issue 6

Jun. 2018

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Article Navigation > Earth Science > 2018 > 43(6): 2055-2075

Zhao Yingli, Liu Yongjiang, Li Weimin, Feng Zhiqiang, Wen Quanbo, Liang Chenyue, 2018. Detrital Zircon LA-ICP-MS U-Pb Age of Late Carboniferous to Early Permian Sandstones in Central Great Xing'an Range and Its Geological Significance. Earth Science, 43(6): 2055-2075. doi: 10.3799/dqkx.2018.613

Citation:

Zhao Yingli, Liu Yongjiang, Li Weimin, Feng Zhiqiang, Wen Quanbo, Liang Chenyue, 2018. Detrital Zircon LA-ICP-MS U-Pb Age of Late Carboniferous to Early Permian Sandstones in Central Great Xing'an Range and Its Geological Significance. Earth Science, 43(6): 2055-2075. doi: 10.3799/dqkx.2018.613

Citation:

Zhao Yingli, Liu Yongjiang, Li Weimin, Feng Zhiqiang, Wen Quanbo, Liang Chenyue, 2018. Detrital Zircon LA-ICP-MS U-Pb Age of Late Carboniferous to Early Permian Sandstones in Central Great Xing'an Range and Its Geological Significance. Earth Science, 43(6): 2055-2075. doi: 10.3799/dqkx.2018.613

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Detrital Zircon LA-ICP-MS U-Pb Age of Late Carboniferous to Early Permian Sandstones in Central Great Xing'an Range and Its Geological Significance

doi: 10.3799/dqkx.2018.613

1.
Research Center of Paleontology & Stratigraphy, Jilin University, Changchun 130026, China
2.
College of Earth Sciences, Jilin University, Changchun 130061, China
3.
Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Land and Resources, Changchun 130061, China
4.
Department of Earth Science and Engineering, Taiyuan University of Technology, Taiyuan 030024, China

Received Date: 2017-12-21
Publish Date: 2018-06-15

Abstract

Abstract

Northeast China, located in the eastern part of the Central Asian orogenic belt (CAOB), is composed of several micro-blocks (e.g. Erguna block, Xing'an block, Songliao block and Jiamusi block). However the suturing locations, timing and the amalgamation processes among the micro-blocks are still unclear. This study focuses on the systematic study on petrography and detrital zircon LA-ICP-MS U-Pb ages of the Late Carboniferous to Early Permian sandstones from the Baoligaomiao Formation in the Moguqi area, Central Great Xing'an range, in order to reveal the tectonic background of the provenances and constrain the evolution history of the Xing'an and Songliao blocks. Petrographically, detrital compositions show that the investigated sandstones are immature, probably due to rapid erosion, transportation, and diagenetic processes, as well as nearly supplying from the source area. Additionally, the abundance of volcanic lithic reveals that the magmatic provenance dominates. Meanwhile, the cathodoluminescence (CL) images, Th/U ratios and REE pattern of analyzed zircons also imply the igneous origin. Zircon U-Pb ages obtained from the analyzed samples are mainly concentrated in 282-360 Ma (n=134), with the peaks at ca.290 Ma, 305 Ma, 325 Ma and 350 Ma. By combining our new geochronological data with previous regional reports, it is concluded that the provenance of the sandstones is possibly derived from the subduction-and syn-collision-related Paleozoic magmatic arc along the Moguqi-Nenjiang-Heihe areas. Furthermore, the youngest zircon U-Pb ages of 282±4 Ma (sample 15MG10) and 287±4 Ma (sample 15MG11) give the lower limit age of sediments. Comparing the detrital zircon U-Pb concentrations of the Late Carboniferous to Early Triassic sandstones in the Suolun-Moguqi areas, it is found that there is no difference between the Late Carboniferous to Early Permian clastic components in the Xing'an block and the Middle Permian to Early Triassic ones in the Songliao block, indicating the above mentioned two blocks have been amalgamated before Late Carboniferous period along the Hegenshan-Heihe suture zone.
- Central Great Xing'an range,
- Late Carboniferous to Early Permian,
- detrital zircon U-Pb age,
- Hegenshan-Heihe suture zone,
- tectonic evolution,
- petrology

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References(150)

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