Sedimentary characteristics analysis and paleoenvironmental restoration of the ground substrate in Baiquan County, Qiqihar area, Songnen Plain

SHAO Xingkun; HOU Hongxing; REN Bingzhang; SHI Lingfeng; ZHAN Zedong; XI Guangyue; LI Junhua; CAO Longyu; GAO Yuan

doi:10.12097/gbc.2023.08.039

2024 Vol. 43, No. 9

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SHAO Xingkun, HOU Hongxing, REN Bingzhang, SHI Lingfeng, ZHAN Zedong, XI Guangyue, LI Junhua, CAO Longyu, GAO Yuan. 2024. Sedimentary characteristics analysis and paleoenvironmental restoration of the ground substrate in Baiquan County, Qiqihar area, Songnen Plain. Geological Bulletin of China, 43(9): 1498-1514. doi: 10.12097/gbc.2023.08.039

Citation:

SHAO Xingkun, HOU Hongxing, REN Bingzhang, SHI Lingfeng, ZHAN Zedong, XI Guangyue, LI Junhua, CAO Longyu, GAO Yuan. 2024. Sedimentary characteristics analysis and paleoenvironmental restoration of the ground substrate in Baiquan County, Qiqihar area, Songnen Plain. Geological Bulletin of China, 43(9): 1498-1514. doi: 10.12097/gbc.2023.08.039

Sedimentary characteristics analysis and paleoenvironmental restoration of the ground substrate in Baiquan County, Qiqihar area, Songnen Plain

Langfang Natural Resources Comprehensive Survey Center, CGS, Langfang 065000, Hebei, China

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Corresponding author: HOU Hongxing, wjhjhhx@163.com

Received Date: 27 August 2023

Revised Date: 10 December 2023

Publish Date: 15 September 2024

Abstract

Abstract

Ground substrate is a new concept in natural resource management, which is the fundamental material supporting the breeding of various natural resources. Strengthening the analysis of ground substrate sedimentary environment and the restoration of paleoenvironment is of great significance for studying its formation mechanism. This article analyzes the sedimentary characteristics and the sedimentary environment of a 50 m shallow ground substrate, based on the data of full core clay minerals, carbonates, magnetic susceptibility, and carbon elements. The research results indicate that there are 16 layers of soil substrate vertically distributed in the study area, exhibiting a transitional sedimentary evolution from deep to shallow, characterized by lacustrine sedimentation → continental eolian facies → meadow facies.The deep lakeside facies and embankment sediments are formed in cold and extremely dry environments, the middle deep lake sediments are formed in warm and humid environments, and the shallow surface meadow and aeolian sediments are formed in relatively dry and cold environments. Based on previous data and ¹⁴C, photoluminescence and ESR dating results, the sedimentary evolution stage of the study area is divided into the late Early Pleistocene to early Middle Pleistocene dry cold sedimentary stage, the warm lacustrine sedimentary stage in the middle and late Middle Pleistocene, the Late Pleistocene to Early Holocene eolian loess sedimentary stage and the black soil sedimentary stage in the Middle and Late Holocene.
- Songnen Plain /
- ground substrate /
- Baiquan area /
- sedimentary environment /
- paleoenvironmental restoration

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References

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