The Muong Te fault zone is known as the active tectonic area in Northwest Vietnam, proved by earthquakes with the most recent one of Ms 4.9 on June 16, 2020 and hundreds of aftershocks accompanying with landslides. The neotectonic activities of the study area is asssessed by analysing 61 sub-basins in term of geomorphological indices: Ratio of valley floor width to valley height (Vf), Stream-Length gradient index (SL), Hypsometric integral index (HI), Hypsometric curve (HC) and Index of Relative Active Tectonics (IRAT). As a results, this are has: relative lowVf corresponding to the terrain of V-shape valleys; SL in large range from 10 to 7000 (gradient - m); straight – convex H ccurve and HI in the range of 0,422 – 0,51 corresponding to the developing phase of river basins; More than 50% of asymmetric basins (AF) due to tectonic impacts. IRAT ranging from 1.25 to 2.5 divided into 3 classes according to the tectonic levels: (1) – strong uplift with - IRAT < 1.5, (2) moderate uplift with IRAT from 1.5 to 2.0 (strong) and (3) weak uplift with IRAT more than 2. The calculated values of the indices are seemed very consistent with the tectonic-geological features of the Muong Te area.
Published in | American Journal of Environmental and Resource Economics (Volume 9, Issue 3) |
DOI | 10.11648/j.ajere.20240903.12 |
Page(s) | 61-73 |
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Neotectonics, Geomorphological Indices, Morphotectonics, Muong Te, Song Da
[1] | Alireza Habibi, Mohammadreza Gharibreza (2015). Estimation of the relative active tectonics in Shahriary basin (Central Iran) using geomorphic and seismicity indices. Natural Environment Change, Vol. 1, No. 1, Summer & Autumn 2015, pp. 71-83. |
[2] | Le Duy Bach, Ngo Gia Thang (1996). Tectonic setting of Tay Bac Vietnam. Journal of GEOLOGY and Mining, No 5, Hanoi, p 9–105 (Vietnamese). |
[3] | Bull W. B. (2007). Tectonic geomorphology of mountains: A New approach to Paleoseismology. Wiley-Blackwell. Oxford, 328pp. |
[4] | Zuchiewicz W., Cuong N. Q., Bluszcz A. & Michalik M., 2004. Quaternary sediments in the Dien Bien Phu fault zone, NW Vietnam: A record of young tectonic processes in the light of OSL-SAR dating results. Geomorphology, 60 (3-4): 269-302.i. |
[5] | Hamdouni R. E., Irigaray C., Fernández T., Chacón J., Keller E. A. (2008). Assessment of relative active tectonics, southwest border of the Sierra Nevada (Southern Spain). Geomorphology 96, 150–173. |
[6] | Joshi P. N., Maurya D. M., Chamyal L. S. (2013). Morphotectonic segmentation and spatial variability of neotectonic activity along the Narmada–Son Fault, Western India: Remote sensing and GIS analysis. Geomorphology 180–181 (2013) 292–306. |
[7] | Keller E. A., Seaver D. B., Laduzinsky D. L., Johnson D. L., Ku T. L. (2000). Tectonic geomorphology of active folding over buried reverse faults: San Emigdio Mountain front, southern San Joaquin Valley, California. Geological Society of America Bulletin 112, 86–97. |
[8] | Keller E. A., Pinter N. (2002). Active Tectonics. Earthquakes, Uplift and Landscape. Prentice Hall, New Jersey. (362 p.). |
[9] | Ngo Van Liem, Nguyen Phuc Dat, Bui Tien Dieu, Vu Van Phai, Phan Trong Trinh, Hoang Quang Vinh, Tran Van Phong (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 Vol. 38, 1-15, Ha Noi. |
[10] | Nguyen Huu Tuyen, Ph. V. Phach, Renat Shakirov, C. D. Trong, P. N. Hưng, L. D. Anh, 2018. ‘’Geoblocks Delineation and Recognition of Earthquake Prone Areas in the Tuan Giao Area (Northwest Vietnam)’’. Journal of Geotectonics, Vol 52, No 3, Pages 359-381. |
[11] | Nguyen Huu Tuyen (2012). ‘’Study of geo-dynamics condition for Tuan Giao and adjacent area, establish the scientific criteria for earthquakes prediction’’. PhD Dissertation, Hanoi Natural University (Vietnamese). |
[12] | Nguyen Huu Tuyen, Cao Dinh Trieu, Phung Thi Thu Hang (2012). The active Geodynamics Blocks model case study for Tuan Giao Area. Journal of Geology, Vol 331-332 (5-8/2012), p. 145-155, ISSN 0866-7381. |
[13] | Nguyen Huu Tuyen, A. I. Gorshkov, Ngo Thi Lu (2012). Recognition of Earthquake-prone area (M≥ 5.0) applied for North Vietnam and Adjacency. Journal of Earth Science, Vol 34, No3, Ha Noi, p. 251-265. |
[14] | Nguyen Huu Tuyen, Chu Van Ngoi, Cao Dinh Trieu (2012). Forcasting earthquakes with M ≥ 5.0 in the Tuan Giao and Adjacent areas by the application of CORA-3 Algorithm. Journal of Geology, series A No 331-332, 5-8/2012, p 131-144, ISSN 0866-7381. |
[15] |
Nguyen Huu Tuyen, Cao Dinh Trong, Pham Nam Hung, Phung Thi Thu Hang, 2019. The Main Structure of Epicenter Area and Aftershock Ditribution of Large Earthquake (Ms = 6.7). International Journal of Innovative Studies in Sciences and Engineering Technology (IJISSET, ISSN 2455-4863 (Online),
www.ijisset.org Volume 5 Issue 6, 2019. |
[16] | Mahmood S. A., Gloaguen R. (2012). Appraisal of active tectonics in Hindu Kush: Insights from DEM derived geomorphic indices and drainage analysis. Geoscience Frontiers 3(4), 407–428. |
[17] | Pérez-Pena J. V., Azanon J. M. (2009). CalHypso: An ArcGIS extension to calculate hypsometric curves and their statistical moments. Applications to drainage basin analysis in SE Spain. Computers & Geosciences 35, 1214–1223. |
[18] | Pérez-Pena J. V. (2009). GIS-based tools and methods for landscape analysis and active tectonic evaluation. Departamentdo de Geodimámica, Universidad de Granada. |
[19] | Strahler A. N. (1952). Hypsometric (area–altitude) analysis of erosional topography. Geological Society of America Bulletin 63, 1117–1142. |
[20] | Ngo Gia Thang, Le Duy Bach, Nguyen Ngọc Thuy (2007), “The feature of vertical deformation during Pliocene-Quaternary period of the Northwest of Vietnam”, Journal of Earth Science, Vol. 29, No 2, Hanoi, p. 161-170. |
[21] | Nguyen Ngoc Thuy (Investigator) (2005). Seismic zoning for the Northwest of Vietnam. National Project Research KC-08-10, years 2001-2005. |
[22] | Tran Dang Tuyet (ed.) (1976). Geological map of Northwest Vietnam at scale 1/200.000 (geological division). |
[23] | Kuang-Yin Lai, Yue-Gau Chen, Doan Dinh Lam, 2012. Pliocene-to-present morphotectonics of the Dien Bien Phu fault in Northwest Vietnam. Geomorphology 173–174 (2012) 52–68. |
[24] | Vu Van Tich, Tran Trong Thang, 2015. Active Faults and Geothermal Potential in Vietnam: a Case Study in Uva Area, Dien Bien Phu Basin, Along Dien Bien -Lai Chau Fault. Proceedings World Geothermal Congress 2015. Melbourne, Australia, 19-25 April 2015. |
[25] | Bui Phu My (Editor, 1971), revised and edited 2005. Geological and mineral resources map of Việt Nam scale 1: 200.000 sheet Kim Binh - Lao Cai. Department of Geology and Mineral Resources of Vietnam. |
[26] | Tran Dang Tuyet (Editor, 1978), revised and edited 2005a. Geological and mineral resources map of Việt Nam scale 1: 200.000 sheet Khe Su- Muong Te. Published and copyright by Department of Geology and Minerals of Vietnam. |
[27] | Tran Dang Tuyet (Editor, 1984), revised and edited 2005b. Geological and mineral resources map of Việt Nam scale 1: 200.000 sheet Phong Sa Ly - Dien Bien Phu. Published and copyright by Department of Geology and Minerals of Vietnam. |
[28] | Cao Dinh Trong, Nguyen Hoang, Mai Xuan Bach, Nguyen Manh Luc, Le Van Dung, Cao Dinh Trieu, N. S. Syrbu, Dang Thanh Hai, Thai Anh Tuan, Ngo Quang Toan, Duong Van Thanh, 2022. Using Geomorphological Indicators to Predict Earthquake Magnitude (MOb-Max): A case study from Cao Bang Province and Adjasent Areas (Vietnam). ISSN 0016-8521, Journal of Geotectonics, Pages 1-18. |
[29] | Ngo Thi Lu, P. T. T Hang, Nguyen Huu Tuyen, Ha Thi Giang, Nguyen Thanh Hai, 2019. The Characteristics of Aftershock activieties of Dien Bien Eartquake on 19 February 2019 and their relation to the local geomorphological, tectonic feartures. Sciendo Ekologia (Bratislava), Vol 38 No-2, P. 189-200/ |
APA Style
Tuyen, N. H., Hang, P. T. T. (2024). Active Tectonic Features of Muong Te Zone from Geomophological Indicators. American Journal of Environmental and Resource Economics, 9(3), 61-73. https://doi.org/10.11648/j.ajere.20240903.12
ACS Style
Tuyen, N. H.; Hang, P. T. T. Active Tectonic Features of Muong Te Zone from Geomophological Indicators. Am. J. Environ. Resour. Econ. 2024, 9(3), 61-73. doi: 10.11648/j.ajere.20240903.12
@article{10.11648/j.ajere.20240903.12, author = {Nguyen Huu Tuyen and Phung Thi Thu Hang}, title = {Active Tectonic Features of Muong Te Zone from Geomophological Indicators}, journal = {American Journal of Environmental and Resource Economics}, volume = {9}, number = {3}, pages = {61-73}, doi = {10.11648/j.ajere.20240903.12}, url = {https://doi.org/10.11648/j.ajere.20240903.12}, eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ajere.20240903.12}, abstract = {The Muong Te fault zone is known as the active tectonic area in Northwest Vietnam, proved by earthquakes with the most recent one of Ms 4.9 on June 16, 2020 and hundreds of aftershocks accompanying with landslides. The neotectonic activities of the study area is asssessed by analysing 61 sub-basins in term of geomorphological indices: Ratio of valley floor width to valley height (Vf), Stream-Length gradient index (SL), Hypsometric integral index (HI), Hypsometric curve (HC) and Index of Relative Active Tectonics (IRAT). As a results, this are has: relative lowVf corresponding to the terrain of V-shape valleys; SL in large range from 10 to 7000 (gradient - m); straight – convex H ccurve and HI in the range of 0,422 – 0,51 corresponding to the developing phase of river basins; More than 50% of asymmetric basins (AF) due to tectonic impacts. IRAT ranging from 1.25 to 2.5 divided into 3 classes according to the tectonic levels: (1) – strong uplift with - IRAT < 1.5, (2) moderate uplift with IRAT from 1.5 to 2.0 (strong) and (3) weak uplift with IRAT more than 2. The calculated values of the indices are seemed very consistent with the tectonic-geological features of the Muong Te area.}, year = {2024} }
TY - JOUR T1 - Active Tectonic Features of Muong Te Zone from Geomophological Indicators AU - Nguyen Huu Tuyen AU - Phung Thi Thu Hang Y1 - 2024/10/29 PY - 2024 N1 - https://doi.org/10.11648/j.ajere.20240903.12 DO - 10.11648/j.ajere.20240903.12 T2 - American Journal of Environmental and Resource Economics JF - American Journal of Environmental and Resource Economics JO - American Journal of Environmental and Resource Economics SP - 61 EP - 73 PB - Science Publishing Group SN - 2578-787X UR - https://doi.org/10.11648/j.ajere.20240903.12 AB - The Muong Te fault zone is known as the active tectonic area in Northwest Vietnam, proved by earthquakes with the most recent one of Ms 4.9 on June 16, 2020 and hundreds of aftershocks accompanying with landslides. The neotectonic activities of the study area is asssessed by analysing 61 sub-basins in term of geomorphological indices: Ratio of valley floor width to valley height (Vf), Stream-Length gradient index (SL), Hypsometric integral index (HI), Hypsometric curve (HC) and Index of Relative Active Tectonics (IRAT). As a results, this are has: relative lowVf corresponding to the terrain of V-shape valleys; SL in large range from 10 to 7000 (gradient - m); straight – convex H ccurve and HI in the range of 0,422 – 0,51 corresponding to the developing phase of river basins; More than 50% of asymmetric basins (AF) due to tectonic impacts. IRAT ranging from 1.25 to 2.5 divided into 3 classes according to the tectonic levels: (1) – strong uplift with - IRAT < 1.5, (2) moderate uplift with IRAT from 1.5 to 2.0 (strong) and (3) weak uplift with IRAT more than 2. The calculated values of the indices are seemed very consistent with the tectonic-geological features of the Muong Te area. VL - 9 IS - 3 ER -