APPLICATION OF FLUVIAL DEPOSITIONAL SYSTEM ANALYSIS DURING THE QUATERNARY GEOLOGICAL SURVEY IN THE SHALLOW COVERED AREA: A CASE STUDY OF 1: 50000 GEOLOGICAL MAPPING IN THE HETAO REGION OF INNER MONGOLIA

LIU Xiao-tong; ZHANG Xu-jiao; YE Pei-sheng; JIA Li-yun; CAI Mao-tang; HE Ze-xin; LI Cheng-lu; WU Ze-qun; ZHOU Qing-shuo

2016 Vol. 22, No. 4

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Article navigation > Journal of Geomechanics > 2016 > 22(4): 868-881

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LIU Xiao-tong, ZHANG Xu-jiao, YE Pei-sheng, JIA Li-yun, CAI Mao-tang, HE Ze-xin, LI Cheng-lu, WU Ze-qun, ZHOU Qing-shuo. APPLICATION OF FLUVIAL DEPOSITIONAL SYSTEM ANALYSIS DURING THE QUATERNARY GEOLOGICAL SURVEY IN THE SHALLOW COVERED AREA: A CASE STUDY OF 1: 50000 GEOLOGICAL MAPPING IN THE HETAO REGION OF INNER MONGOLIA[J]. Journal of Geomechanics, 2016, 22(4): 868-881.

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APPLICATION OF FLUVIAL DEPOSITIONAL SYSTEM ANALYSIS DURING THE QUATERNARY GEOLOGICAL SURVEY IN THE SHALLOW COVERED AREA: A CASE STUDY OF 1: 50000 GEOLOGICAL MAPPING IN THE HETAO REGION OF INNER MONGOLIA

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

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Corresponding author: ZHANG Xu-jiao, zhangxj@cugb.edu.cn

Received Date: 15 September 2016

Publish Date: 25 December 2016

Abstract

Abstract

With the conduction of the national large-scale (1:50000) geological survey in special geological and geomorphic areas, traditional Quaternary mapping methods could not meet the needs of modern geological mapping in the coverage areas. Therefore, "What can we do" and "How can we do" become the key issues for the geological workers during the Quaternary geological mapping. In order to test even find some new geological mapping methods, we select typical coverage area-Hetao plain as our study area. Under the guidance of theories in fluvial sedimentlogy, combined with drilling column, we build the fluvial sedimentary system since the Holocene. Regard these subfacies as the sedimentary frame for the geological sketch frame, we recognize fluvial subfacies, embankments subfacies, and flood plain subfacies. The principle of step by step approximation was applied to determine the geological boundary. Besides that, three periods of fluvial deposits and corresponding sedimentary systems were recognized. Therefore, the problem of lacking geological units during the Quaternary geological survey in covered area might be solved, and a set of feasible scheme could be provided.
- shallow covered area /
- mapping methods /
- fluvial system /
- sedimentary facies analyzation /
- Hetao plain

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References

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