<trans-title>Geological significance of the development characteristics of karst geomorphology and its formation mechanism in Hunan-Guangxi corridor</trans-title>

LUO Shuwen; HE Wei; YANG Tao; DENG Yadong; LV Yong; WU Kehua; MENG Qingxin

doi:10.11932/karst20210502

Volume 40 Issue 5

Oct. 2021

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Article Navigation > CARSOLOGICA SINICA > 2021 > 40(5): 750-759

LUO Shuwen,HE Wei,YANG Tao,et al.Geological significance of the development characteristics of karst geomorphology and its formation mechanism in Hunan-Guangxi corridor[J].Carsologica Sinica,2021,40(05):750-759. doi: 10.11932/karst20210502

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Geological significance of the development characteristics of karst geomorphology and its formation mechanism in Hunan-Guangxi corridor

doi: 10.11932/karst20210502

LUO Shuwen^{1, 2, 4},
HE Wei¹,
YANG Tao³,
DENG Yadong^{2, 4},
LV Yong^{2, 4},
WU Kehua¹,
MENG Qingxin^{2, 4}

1.
Guizhou Institute of Mountain Resources Research，Guiyang， Guizhou 55001， China
2.
Institute of Karst Geology，CAGS，Guilin，Guangxi 541004， China
3.
Guiyang No.12 Middle School ， Guiyang，Guizhou 550002， China
4.
Key Laboratory of Karst Dynamics，MNR & GZAR， Guilin，Guangxi 50002，China

Funds:

2016YFC0502606

[2017]5720

[2016]21

[2019]08

DD20190022

Received Date: 2021-03-30
Publish Date: 2021-10-25

Abstract

Abstract

To explore the karst development characteristics， hydrogeomorphological significance and the causes of formation of peak forest plain in Hunan-Guangxi Corridor，in this paper，the investigation of spatial distribution characteristics of landforms， lithology and landform types in the area are conducted ，and the formation and evolution of hydrogeomorphology are discussed under the guidance of karst hydrogeomorphology theory.The analysis of the spatial distribution characteristics shows that the water system in this area has undergone a reverse seizure process； its regional geomorphic evolution is affected by the uplift of Yuechengling and Haiyangshan mountains， which has led to the narrowing of the Hunan-Guangxi Corridor and diversion of the Xiangjiang river to northeast. The geomorphic evolution has experienced at least three flattening periods， the ancient Xiangjiang period，the Linghe incubation period， and the Linghe period. In addition，the concept model of the karst basin intertidal zone as well as the interactive capture mode of karst basin are put forward for the first time when the formation dynamic mechanism of peak forest plain is analyzed， which enriches the genetic type of peak forest plain and the research methods of karst hydrogeomorphology. The scientific terms put forward here is also of important scientific implications.
- Hunan-Guangxi corridor,
- Ling canal,
- karst basin,
- intertidal zone,
- geomorphic characteristics,
- Guilin karst landform,
- interactive capture mode of karst basin

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References

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