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Development of large‐scale sand bodies in a fault‐bounded lake basin: Pleistocene-Holocene Poyang Lake, Southern China

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Abstract

In fault-bounded lacustrine basins, the lake basement may be exposed due to tilting of crustal blocks, forming islands of varying size. Such islands are commonly associated with sandy facies that may serve as important reservoirs for oil and gas accumulation. The present study investigated large sand bodies of Pleistocene-Holocene age on Songmenshan Island in the center of Poyang Lake, Jiangxi Province, southern China. The relationship of sedimentation on Songmenshan Island to its formation history was analyzed by means of Google satellite observations and field studies combined with scanning electron microscope, grain size, and 14 C dating analyses. The area of Songmenshan Island (39 km2) represents 8% of the total lake area (500 km2), and its height (81 m) is several times greater than that of the depth of the surrounding lake (13 m). The island has been uplifted since ~ 5 Ma at a rate of ~ 16 m Myr− 1 as a consequence of intrabasinal block faulting. The surficial deposits of the island consist of wave-controlled beach-bars in the lower part (< 36 m elevation) and wind-controlled eolian dunes in the upper part. Sedimentary characteristics were different between beach bars and sand dunes in terms of bedding, sedimentary structures, and grain size and texture. The beach bars are characterized by low-angle cross-bedding, fan-shaped conchoidal, and disciform fractures, and small V-shaped impact craters on quartz grain surfaces. The eolian dunes are characterized by large-scale high-angle cross-bedding, dish-, crescent-, and V-shaped impact craters on quartz grain surfaces. Whereas sand movement in the beach-bar facies was dominantly through traction, saltation was the major process in the eolian dune environment. The depositional history of Songmenshan Island can be divided into 3 stages: (1) deltaic sedimentation from the Ganjiang and **ushui rivers, which are connected to the Yangtze River via a channel; (2) wave reworking of deltaic sediments in shoreline beach-bar facies after initial uplift; and (3) wind reworking of sands in eolian dune facies following further uplift. Later in its history, Songmenshan Island was reduced through wind and wave erosion into two subequal parts (19.6 km2 and 19.8 km2), producing its present configuration. The large sand bodies comprising this island may eventually be buried in a cocoon of organic-rich lacustrine muds, yielding an exploration target. Songmenshan Island may thus serve as a model for development of sand-rich reservoir facies in fault-bounded lacustrine basins.

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Acknowledgements

We thank Wenfeng Wang, **abin Wang, Junjie Li, Shengqian Liu, Zhen Wang, and Yiming Bai for their help in fieldwork and data analysis. This study was supported by the Natural Science Foundation of **njiang Uygur Autonomous Region (2020D01C064), National Science and Technology Major Project of China (2017ZX05009-002), Tianshan Innovation Team Program (2020D14023), Doctoral Research Startup Foundation of **njiang University (BS190237), and Tianchi Doctoral Project of **njiang (TCBS201929). Thanks are also extended to JOPL Editors Thomas J. Whitmore and Maria Isabel Velez Caicedo and two anonymous reviewers for their constructive comments.

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  1. School of Energy Resources, China University of Geosciences (Bei**g), Bei**g, 100083, China

    Chenlin Hu, Yuanfu Zhang & Zaixing Jiang

  2. Institute of Geology and Mining Engineering, **njiang University, Urumqi, 830047, China

    Chenlin Hu

  3. PetroChina Research Institute of Petroleum Exploration and Development, Bei**g, 100083, China

    Min Wang

  4. College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, 266590, China

    Chao Han

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Hu, C., Zhang, Y., Jiang, Z. et al. Development of large‐scale sand bodies in a fault‐bounded lake basin: Pleistocene-Holocene Poyang Lake, Southern China. J Paleolimnol 65, 407–428 (2021). https://doi.org/10.1007/s10933-021-00179-9

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