ASSESSMENT OF GEOMORPHIC PROCESSES AND ACTIVE TECTONICS IN CON VOI MOUNTAIN RANGE AREA (NORTHERN VIETNAM) USING THE HYPSOMETRIC CURVE ANALYSIS METHOD

Ngo Van Liem*, Nguyen Phuc Dat, Bui Tien Dieu, Vu Van Phai, Phan Trong Trinh, Hoang Quang Vinh, Tran Van Phong
Author affiliations

Authors

  • Ngo Van Liem* Institute of Geological Sciences, Vietnam Academy Science and Technology
  • Nguyen Phuc Dat Vietnam Institute of Geosciences and Mineral Resources, Ministry of Natural Resources and Environment
  • Bui Tien Dieu Geographic Information System Group, Department of Business Administration and Computer Science, University College of Southeast Norway; Faculty of Geomatics and Land Administration, Hanoi University of Mining and Geology
  • Vu Van Phai Faculty of Geography, VNU University of Sciences
  • Phan Trong Trinh Institute of Geological Sciences, Vietnam Academy Science and Technology
  • Hoang Quang Vinh Institute of Geological Sciences, Vietnam Academy Science and Technology
  • Tran Van Phong Institute of Geological Sciences, Vietnam Academy Science and Technology

DOI:

https://doi.org/10.15625/0866-7187/38/2/8602

Keywords:

Geomorphic index, Hypsometric curve, Statistical moments, Active tectonics, Red River fault, Day Nui Con Voi

Abstract

the Day Nui Con Voi (DNCV) area of Vietnam. For this purpose, a spatial database was collected and constructed, including DEM (Digital Elevation Model) and a geological map. The hypsometric curve (HC) analysis method and its statistical moments were adopted to use for the assessment. These methods have been widely used for the assessment of geomorphic processes and active tectonics in many areas in the world showing promising results. A total of 44 sub-basins of the Red River and the Chay river were analyzed. The result shows that 3 curve-types such as "straight- shape", "S- shape", and concave were found; with the concave curve being the dominant and widely distributed in the northeast side and in the south of the southwestern side of the study area. The hypsometric integral (HI) values are rather small with the largest value is 0.37 and the smallest one is 0.128. Other statistical moments of the hypsometric curve, i.e. skew (SK), kurtosis (KUR), and the density function (density skew - DSK and density kurtosis-DKUR) show great values, which increased in the south direction of the area study. Accordingly, recent active tectonics (uplift-lower) in the study area is generally weak; however, they are also not completely homogeneous and can be distinguished by different levels. The southwestern side is being lifted higher than the northeastern side. The northern part is being lifted larger than the southern part. In the region, the uplift activities were increased gradually in the Pliocene-Quaternary and could have stopped at certain time in the past. The current geomorphic processes are mainly headward erosion in the upstream.

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Published

09-04-2016

How to Cite

Liem*, N. V., Dat, N. P., Dieu, B. T., Phai, V. V., Trinh, P. T., Vinh, H. Q., & Phong, T. V. (2016). ASSESSMENT OF GEOMORPHIC PROCESSES AND ACTIVE TECTONICS IN CON VOI MOUNTAIN RANGE AREA (NORTHERN VIETNAM) USING THE HYPSOMETRIC CURVE ANALYSIS METHOD. Vietnam Journal of Earth Sciences, 38(2), 202–216. https://doi.org/10.15625/0866-7187/38/2/8602

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