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中国科技核心期刊

地学领域高质量科技期刊分级T2区（2023）

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Volume 43 Issue 4
Jul.  2024
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Article Contents
Article Navigation >  Bulletin of Geological Science and Technology  > 2024  >  43(4): 273-290
FAN Yu, HUANG Kun, DUAN Huiyu, LIN Yuhang, LUO Mingming, WAN Junwei, WEN Hanhui, QU Jincai, ZHANG Longxuan. Control of tectonic evolution on karstification and karst collapse in the Lianzhou Basin, northwestern Guangdong Province[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 273-290. doi: 10.19509/j.cnki.dzkq.tb20230120
Citation: FAN Yu, HUANG Kun, DUAN Huiyu, LIN Yuhang, LUO Mingming, WAN Junwei, WEN Hanhui, QU Jincai, ZHANG Longxuan. Control of tectonic evolution on karstification and karst collapse in the Lianzhou Basin, northwestern Guangdong Province[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 273-290. doi: 10.19509/j.cnki.dzkq.tb20230120
shu

Control of tectonic evolution on karstification and karst collapse in the Lianzhou Basin, northwestern Guangdong Province

doi: 10.19509/j.cnki.dzkq.tb20230120
  • 1.

    School of Environmental Studies, China University of Geosciences(Wuhan), Wuhan 430078, China

  • 2.

    No. 940 Branch of Geology Bureau for Nonferrous Metals of Guangdong Province, Qingyuan Guangdong 511500, China

More Information
  • Author Bio:

    FAN Yu, E-mail: yufan@cug.edu.cn

  • Corresponding author: WAN Junwei, E-mail: wanjw@cug.edu.cn
  • Received Date: 07 Mar 2023
  • Accepted Date: 01 Sep 2023
  • Rev Recd Date: 28 May 2023
    Abstract
  • Objective

    There is still a lack of systematic understanding of the evolution process of the Lianzhou Basin since the Mesozoic and its response to karstic development.

    Methods

    Based on the comprehensive analysis of the latest field geological investigations, hydrogeological drilling, dissolution experiments, and three-dimensional geological modelling, the tectonic evolution stages of the basin can be divided, and the karstification of each stage can be discussed by considering the existing geological data.

    Results

    Before the Cretaceous, carbonate rocks with strong dissolution were successively deposited under the rise or fall movement of the crust, which laid a material foundation for karstic development. The Indosinian movement caused vertically multilayered strata to form an E-W-trending structure, and the Yanshanian movement made the straddle-oblique superimposed a NE-SW-trending structure. They controlled the geological structures, spatial distribution, and dissolution behaviors of carbonate strata. And the distribution of mountains and river system were established. However, karst generally does not develop. An intracontinental and intermountain faulted confluence lake basin formed from the Cretaceous to the Palaeogene, the slow crustal uplift strengthened the karstification around the basin, and it currently retains the early karst platform. Later, they were buried-filled-consolidated by alluvial deposits; therefore, karst basically stopped developing, generating a thick-covered red strata basin. Since the Neogene, the rapid uplift of the crust has led to the continuous elevation of mountains around the basin, deepening of rivers, and strong development of karst, shaping multilevel karst platforms. When part of the Cretaceous red strata in the basin are denuded or cut through, karstification is reactivated. After many changes and penetrations of water systems, the graben basin formed, with karst strata covered by Quaternary sediments, Tectonic evolution controls karstic development, karstification influences the internal structure of the basin, and soil structure causes karst ground collapse.

    Conclusion

    This study can provide a scientific basis and guidance for understanding karst collapse conditions in covered karst areas.

     

    • The authors declare that no competing interests exist.
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