Drainage divide stability at Wulashan, northern margin of the Ordos block, China: Evidence from the analysis of <i>χ</i> value

BAI Luanxi; TAN Xibin; ZHOU Chao

doi:10.12090/j.issn.1006-6616.2021128

Volume 28 Issue 4

Aug. 2022

Turn off MathJax

Article Contents

Article Navigation > Journal of Geomechanics > 2022 > 28(4): 513-522

BAI Luanxi, TAN Xibin, ZHOU Chao, 2022. Drainage divide stability at Wulashan, northern margin of the Ordos block, China: Evidence from the analysis of χ value. Journal of Geomechanics, 28 (4): 513-522. DOI: 10.12090/j.issn.1006-6616.2021128

Citation:

PDF( 15417 KB)

Drainage divide stability at Wulashan, northern margin of the Ordos block, China: Evidence from the analysis of χ value

doi: 10.12090/j.issn.1006-6616.2021128

BAI Luanxi^{1, 2, 3
,},
TAN Xibin^{1, 2
,
,},
ZHOU Chao^{1, 2}

1.
Institute of Geology, China Earthquake Administration, Beijing 100029, China
2.
State Key Laboratory of Earthquake Dynamics, Beijing 100029, China
3.
Exploration and Development Research Institute, SINOPEC East China Branch Company, Nanjing 210000, Jiangsu, China

Funds:

the Independent Science and Technology Development Project of the Institute of Geology, China Earthquake Administration F-21-02

More Information

Received: 2021-09-26
Revised: 2022-01-23

Abstract

Abstract

The stability of drainage divides carries important tectonic and climatic information. However, there is still no consensus on the criterion for measuring the stability of drainage divides, which may lead to different conclusions. There are two different views on the stability of the divide at the Wulashan horst, northern margin of the Ordos block: The drainage divide is moving northward, according to the comparison of drainage-basin morphology (such as elbows of capture, knick points); The drainage divide remains stable, according to the comparison of Gilbert metrics. In this study, we used the χ-plot method to check both the stability of the Wulashan drainage divide and the reliability of the above methods. The analysis shows that the χ value at the top of the northern side is higher than that at the same elevation of the southern side if a lower baseline was set (1300 m a.s.l.); If a higher baseline (~1800 m a.s.l.) is set, the χ values on both sides of the divide are the same at the same elevation. Because the tilting has relatively less influence, the χ-plot with a higher baseline is more representative of the drainage divide stability. In summary, the result supports the view that the drainage divide at the Wulashan horst is at a steady state. Moreover, we discussed the limitations of the methods in measuring the stability of drainage divides.
- drainage divide,
- Wulashan horst,
- χ value,
- tilting

Full-text Translaiton by iFLYTEK

The full translation of the current issue may be delayed. If you encounter a 404 page, please try again later.

FullText(HTML)

References(54)

References

CASTELLTORT S, GOREN L, WILLETT S D, et al., 2012. River drainage patterns in the New Zealand Alps primarily controlled by plate tectonic strain[J]. Nature Geoscience, 5(10): 744-748. doi: 10.1038/ngeo1582

CHEN L C, 2002. Paleoearthquakes, the law of strong earthquake recurrence and potential sites for the occurrence of future strong earthquakes in the Hetao fault-depression zone[D]. Beijing: Institute of Geology, China Earthquake Administration. (in Chinese with English abstract)

DENG Q D, CHENG S P, MIN W, et al., 1999. Discussion on Cenozoic tectonics and dynamics of Ordos block[J]. Journal of Geomechanics, 5(3): 13-21. (in Chinese with English abstract)

DENG Q D, LIAO Y H, 1996. Paleoseismology along the range-front fault of Helan Mountains, north central China[J]. Journal of Geophysical Research: Solid Earth, 101(B3): 5873-5893. doi: 10.1029/95JB01814

FORTE A M, WHIPPLE K X, 2018. Criteria and tools for determining drainage divide stability[J]. Earth and Planetary Science Letters, 493: 102-117. doi: 10.1016/j.epsl.2018.04.026

FORTE A M, WHIPPLE K X, 2019. Short communication: The Topographic Analysis Kit (TAK) for TopoToolbox[J]. Earth Surface Dynamics, 7(1): 87-95. doi: 10.5194/esurf-7-87-2019

GILBERT G K, 1877. Geology of the Henry mountains[R]. Washington: Government Printing Office.

GOREN L, WILLETT S D, HERMAN F, et al., 2014. Coupled numerical-analytical approach to landscape evolution modeling[J]. Earth Surface Processes and Landforms, 39(4): 522-545. doi: 10.1002/esp.3514

HE C Q, CHENG Y L, RAO G, et al., 2018. Geomorphological signatures of the evolution of active normal faults along the Langshan Mountains, North China[J]. Geodinamica acta, 30(1): 163-182. doi: 10.1080/09853111.2018.1458935

HE C Q, RAO G, YANG R, et al., 2019. Divide migration in response to asymmetric uplift: Insights from the Wula Shan horst, North China[J]. Geomorphology, 339: 44-57. doi: 10.1016/j.geomorph.2019.04.024

HE C Q, YANG C J, TUROWSKI J M, et al., 2021. Constraining tectonic uplift and advection from the main drainage divide of a mountain belt[J]. Nature communications, 12(1): 544. doi: 10.1038/s41467-020-20748-2

HE Z T, MA B Q, HAO Y J, et al., 2020. Surface rupture geomorphology and vertical slip rates constrained by terraces along the Wulashan piedmont fault in the Hetao Basin, China[J]. Geomorphology, 358: 107116. doi: 10.1016/j.geomorph.2020.107116

BEESON H W, MCCOY S W, KEEN-ZEBERT A, 2017. Geometric disequilibrium of river basins produces long-lived transient landscapes[J]. Earth and Planetary Science Letters, 475: 34-43. doi: 10.1016/j.epsl.2017.07.010

HOWARD A D, 1994. A detachment-limited model of drainage basin evolution[J]. Water resources research, 30(7), 2261-2285. doi: 10.1029/94WR00757

KIRBY E, WHIPPLE K, 2001. Quantifying differential rock-uplift rates via stream profile analysis[J]. Geology, 29(5): 415-418. doi: 10.1130/0091-7613(2001)029<0415:QDRURV>2.0.CO;2

KIRBY E, WHIPPLE K X, 2012. Expression of active tectonics in erosional landscapes[J]. Journal of Structural Geology, 44: 54-75. doi: 10.1016/j.jsg.2012.07.009

KIRBY J R, PARRILA R K, PFEIFFER S L, 2003. Naming speed and phonological awareness as predictors of reading development[J]. Journal of Educational Psychology, 95(3): 453-464. doi: 10.1037/0022-0663.95.3.453

LI J B, RAN Y K, GUO W S, 2007. Division of Quaternary beds and environment evolution in Hubao basin in China[J]. Quaternary Sciences, 27(4): 632-644. (in Chinese with English abstract)

LI Y B, RAN Y K, CHEN L C, et al., 2015. The latest surface rupture events on the major active faults and great historical earthquakes in Hetao fault-depression zone[J]. Seismology and Geology, 37(1): 110-125. (in Chinese with English abstract)

LIN L L, LI X M, ZHANG H P, et al., 2021. River capture and divide migration of the Zhuozishan area in the northwestern margin of the Ordos Block[J]. Journal of Geomechanics, 27 (2): 294-303. (in Chinese with English abstract)

LIU Y D, TAN X B, YE Y J, et al., 2020. Role of erosion in creating thrust recesses in a critical-taper wedge: An example from Eastern Tibet[J]. Earth and Planetary Science Letters, 540: 116270. doi: 10.1016/j.epsl.2020.116270

PERRON J T, ROYDEN L, 2013. An integral approach to bedrock river profile analysis[J]. Earth Surface Processes and Landforms, 38(6): 570-576. doi: 10.1002/esp.3302

RAN Y K, CHEN L C, YANG X P, et al., 2003. Recurrence characteristics of late Quaternary strong earthquakes on the major active faults along the northern border of Ordos Block[J]. Science in China (Series D): Earth Sciences, 46(2): 189-200. . (in Chinese with English abstract)

RAO G, LIN A M, YAN B, et al., 2014. Tectonic activity and structural features of active intracontinental normal faults in the Weihe Graben, central China[J]. Tectonophysics, 636: 270-285. doi: 10.1016/j.tecto.2014.08.019

RAO G, LIN A M, YAN B, 2015. Paleoseismic study on active normal faults in the southeastern Weihe Graben, central China[J]. Journal of Asian Earth Sciences, 114: 212-225. doi: 10.1016/j.jseaes.2015.04.031

RAO G, CHEN P, HU J M, et al., 2016. Timing of Holocene paleo-earthquakes along the Langshan Piedmont Fault in the western Hetao Graben, North China: Implications for seismic risk[J]. Tectonophysics, 677-678: 115-124. doi: 10.1016/j.tecto.2016.03.035

RAO G, HE C Q, CHENG Y L, et al., 2018. Active normal faulting along the Langshan Piedmont Fault, North China: Implications for slip partitioning in the western Hetao Graben[J]. The Journal of Geology, 126(1): 99-118. doi: 10.1086/694748

SCHWANGHART W, SCHERLER D, 2014. Short Communication: TopoToolbox 2-MATLAB-based software for topographic analysis and modeling in Earth surface sciences[J]. Earth Surface Dynamics, 2 (1): 1-7. doi: 10.5194/esurf-2-1-2014

SHI F, TAN X B, ZHOU C, et al., 2021. Impact of asymmetric uplift on mountain asymmetry: Analytical solution, numerical modeling, and natural examples[J]. Geomorphology, 389: 107862. doi: 10.1016/j.geomorph.2021.107862

SU Q, WANG X Y, LU H Y, et al., 2020. Dynamic Divide Migration as a Response to Asymmetric Uplift: An Example from the Zhongtiao Shan, North China[J]. Remote Sensing, 12(24): 4188. doi: 10.3390/rs12244188

STOKES M F, GOLDBERG S L, PERRON J T, 2018. Ongoing river capture in the Amazon[J]. Geophysical Research Letters, 45(11): 5545-5552. doi: 10.1029/2018GL078129

STRUTH L, GARCIA-CASTELLANOS D, VIAPLANA-MUZAS M, et al., 2019. Drainage network dynamics and knickpoint evolution in the Ebro and Duero basins: From endorheism to exorheism[J]. Geomorphology, 327: 554-571. doi: 10.1016/j.geomorph.2018.11.033

The Research Group on Active Fault System around Ordos Massif, State Seismological Bureau (RGAFSO), 1988. Active fault system Around Ordos Massif[M], Beijing, China: Seismological Press: 1-335. (in Chinese)

TUCKER G E, SLINGERLAND R, 1997. Drainage basin responses to climate change[J]. Water Resources Research, 33(8): 2031-2047. doi: 10.1029/97WR00409

VACHERAT A, BONNET S, MOUTHEREAU F, 2018. Drainage reorganization and divide migration induced by the excavation of the Ebro basin (NE Spain)[J]. Earth Surface Dynamics, 6(2): 369-387. doi: 10.5194/esurf-6-369-2018

WHIPPLE K X, FORTE A M, DIBIASE R A, et al., 2017. Timescales of landscape response to divide migration and drainage capture: Implications for the role of divide mobility in landscape evolution[J]. Journal of Geophysical Research: Earth Surface, 122(1): 248-273. doi: 10.1002/2016JF003973

WHIPPLE K X, TUCKER G E, 1999. Dynamics of the stream-power river incision model: Implications for height limits of mountain ranges, landscape response timescales, and research needs[J]. Journal of Geophysical Research: Solid Earth, 104(B8): 17661-17674. doi: 10.1029/1999JB900120

WILLETT S D, MCCOY S W, PERRON J T, et al., 2014. Dynamic reorganization of river basins[J]. Science, 343(6175): 1248765. doi: 10.1126/science.1248765

WOBUS C, WHIPPLE K X, KIRBY E, et al., 2006. Tectonics from topography: Procedures, promise, and pitfalls[M]//WILLETT S D, HOVIUS N, BRANDON M T, et al. Tectonics, Climate, and Landscape Evolution. Boulder: geological society of America, 55-74.

WU L J, SHI J S, ZHANG Y, L et al., 2020. Ostracod characteristics of the eastern Hetao Basin and its sedimentary environmental significance during the Middle and Late Quaternary. Journal of Geomechanics, 26 (1): 125-134. (in Chinese with English abstract)

XU Y R, HE H L, DENG Q D, et al., 2018. The CE 1303 Hongdong earthquake and the Huoshan Piedmont fault, Shanxi graben: Implications for magnitude limits of normal fault earthquakes[J]. Journal of Geophysical Research: Solid Earth, 123(4): 3098-3121. doi: 10.1002/2017JB014928

YANITES B J, EHLERS T A, BECKER J K, et al., 2013. High magnitude and rapid incision from river capture: Rhine River, Switzerland[J]. Journal of Geophysical Research: Earth Surface, 118(2): 1060-1084. doi: 10.1002/jgrf.20056

ZHENG W J, ZHANG P Z, YUAN D Y, et al., 2019. Basic characteristics of active tectonics and associated geodynamic processes in continental China[J]. Journal of Geomechanics, 25(5): 699-721. (in Chinese with English abstract)

ZHOU C, TAN X B, LIU Y D, et al., 2022a. A cross-divide contrast index (C) for assessing controls on the main drainage divide stability of a mountain belt[J]. Geomorphology, 398: 108071. doi: 10.1016/j.geomorph.2021.108071

ZHOU C, TAN X B, LIU Y D, et al., 2022b. Ongoing Westward Migration of Drainage Divides in Eastern Tibet, Quantified from Topographic Analysis[J]. Geomorphology, 402: 108123. doi: 10.1016/j.geomorph.2022.108123

陈立春, 2002. 河套断陷带的古地震、强震复发规律和未来可能强震地点[D]. 北京: 中国地震局地质研究所.

邓起东, 程绍平, 闵伟, 等, 1999. 鄂尔多斯块体新生代构造活动和动力学的讨论[J]. 地质力学学报, 5(3): 13-21. doi: 10.3969/j.issn.1006-6616.1999.03.003

国家地震局《鄂尔多斯周缘断裂系》课题组, 1988. 鄂尔多斯周缘活动断裂系[M]. 北京: 地震出版社: 1-335.

李建彪, 冉勇康, 郭文生, 2007. 呼包盆地第四纪地层与环境演化[J]. 第四纪研究, 27(4): 632-644. doi: 10.3321/j.issn:1001-7410.2007.04.020

李彦宝, 冉勇康, 陈立春, 等, 2015. 河套断陷带主要活动断裂最新地表破裂事件与历史大地震[J]. 地震地质, 37(1): 110-125. doi: 10.3969/j.issn.0253-4967.2015.01.009

林玲玲, 李雪梅, 张会平, 等, 2021. 鄂尔多斯西北缘桌子山地区河流袭夺和分水岭迁移研究[J]. 地质力学学报, 27(2): 294-303. doi: 10.12090/j.issn.1006-6616.2021.27.02.027

冉勇康, 陈立春, 杨晓平, 等, 2003. 鄂尔多斯地块北缘主要活动断裂晚第四纪强震复发特征[J]. 中国科学(D辑), 33(S1): 135-143. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2003S1014.htm

吴利杰, 石建省, 张翼龙, 等, 2020. 河套盆地东部第四纪中晚期介形类特征及其沉积环境意义[J]. 地质力学学报, 26(1): 125-134. doi: 10.12090/j.issn.1006-6616.2020.26.01.013

郑文俊, 张培震, 袁道阳, 等, 2019. 中国大陆活动构造基本特征及其对区域动力过程的控制[J]. 地质力学学报, 25(5): 699-721. doi: 10.12090/j.issn.1006-6616.2019.25.05.062

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

Figures(6)

Get Citation

PDF

XML

Article Metrics

Article views (553) PDF downloads(64)