Abstract
Valuable geological and environmental information can be obtained from the 200 m thick lacustrine sediments in the Diexi lake (an ancient landslide-dammed lake) of the Minjiang River. The shaking table test method was employed to study the disturbance phenomena which occurred in the Diexi lake sediments. The results show that the disturbance phenomena were caused by liquefaction-induced flows in the unconsolidated lacustrine sediments, due to triggering by earthquakes. The deformations only occurred in unconsolidated sediment layers and not in consolidated layers. This means that a consolidated layer cannot be liquefied and disturbed again by an earthquake for a second time. The disturbance on one layer corresponds to only one earthquake. The temporal occurrence of earthquakes could be determined by disturbance layers generated at different ages. In total, 10 disturbed layers were found in the lacustrine sediments of the Diexi lake. The experiments showed that there were more than 10 earthquakes between 30 ka B.P. and 15 ka B.P. in the Diexi lake area based on the dating of the disturbed sediment layers.
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References
Audemard F, de Santis F (1991) Survey of liquefaction structures induced by recent moderate earthquakes. Bulletin of Engineering Geology and the Environment 44 (1): 5–16.
Bell KLC (2011) On the origin of submarine sediment features in the southern Aegean Sea. Pro-Quest Dissertations and Theses, University of Rhode Island, Rhode Island, Kingston, RI, USA.
Chen J, Dai FC, Tongyan Lv et al. (2013) Holocene landslidedammed lake deposits in the Upper Jinsha River, SETibetan Plateau and their ages. Quaternary International 298: 107–113.
Chi YL, Zhong JH, Zhou YQet al. (1999) The lime blow in the Nanlinghu limestone of early Triassic period in north Chaohu, Anhui: its genesis and significance. Acta Geologica Sinica 15 (1): 137–144. DOI: 10.3321/j.issn:1000-0569.1999.01.016 (In Chinese)
Du YS (2011) Discussion about studies of earthquake event deposit in China. Journal of Palaeogography 13 (6): 581–586. (In Chinese)
Du YS, Shi G, Gong YMet al. (2007) Permian soft-sediment deformation structures related to earthquake in the southern Sydney Basin, eastern Australia. Acta Geologica Sinica 81 (4): 511–518. DOI: 10.3321/j.issn:0001-5717.2007.04.009 (In Chinese)
He BZ, Qiao XF, Xu ZQ, et al. (2010) Late ordovician paleoseismic records of the Manjia’er Depression and adjacent areas in Tarim Basin, Xinjiang, and its geologic significance. Acta Geologica Sinica, 84 (12): 1805–1816. (In Chinese)
Ji XD, Kajiwara K, Nagae T, et al. (2009) A substructure shaking table test for reproduction of earthquake responses of high-rise buildings. Earthquake Engineering & Structural Dynamics 38 (12): 1381–1399.
Lu HB, Zhang YX, Zhang QL, et al. (2006) The earthquake related soft sediment deformation structure and meaning of basin evolution. Acta Geologica Sinica 30 (10): 1606. (In Chinese)
Magenes G, Penna A, Galasco A (2010) A full-scale shaking table test on a two-storey stone masonry building. 14th European Conference on Earthquake Engineering, 2010.8, Ohrid, Macedonia.
Meng SJ, Yuan XM, Sun R (2002) Study on mechanism of earthquake-induced differential settlement of building by shaking table test. Chinese Journal of Geotechnical Engineering 24 (6): 747–751. DOI: 10.3321/j.issn:1000-4548.2002.06.016. (In Chinese)
Rossetti DF, Bezerra FHR, Goes AM, et al. (2011) Sediment deformation in Miocene and post-Miocene strata, northeastern Brazil: evidence for paleoseismicity in a passive margin. Sedimentary Geology 235 (3): 172–187. DOI: 10.1016/j.sedgeo.2010.02.005
Seilacher A (1969) Fault-graded beds interpreted as seismites. Sedimentology 13: 155–159.
Su DC, Sun AP (2011) Soft-sediment deformation and occurrence frequency of palaeoearthquake in the Mesoproterozoic Wumishan Formation, Yongding River Valley. Beijing Journal of Palaeogeography 13 (6): 591–614. (In Chinese)
Sun R, Yuan XM (2007) Method of simulating seismic ground motion in liquefiable soil layer. Rock and Soil Mechanics 28 (Supp.): 759–764. DOI: 10.3321/j.issn:1000-4548.2007.09.015 (In Chinese)
Tang ZY, Li ZB, Ji JB, et al. (2009) Development in shaking table control system. Journal of Earthquake Engineering and Engineering Vibration 29 (6): 162–169. (In Chinese)
Wang LS, Wang XQ, Xu XN (2012) Significances of studying the Diexi paleo-dammed lake at the upstream of Minjiang River, Sichuan, China. Quaternary Sciences 32 (5): 998–1010. DOI: 10.3321/j.issn:1005-2321.2007.04.020. (In Chinese)
Wang LS, Yang LZ, Wang XQ, et al. (2005) Discovery of huge ancient dammed lake on upstream of Minjiang River in Sichuan, China. Journal of Chengdu University of Technology (Science & Technology Edition) 32 (1): 1–11. DOI: 10.3969/j.issn.1671-9727.2005.01.001 (In Chinese)
Wang PF, Chen J, Dai FC et al. (2014) Chronology of relict lake deposits around the Suwalong paleolandslide in the upper Jinsha River, SETibetan Plateau: Implications to Holocene tectonic perturbations. Geomorphology 217: 193–203.
Wang P, Zhang B, Qiu WL, et al. (2011) Soft-sediment deformation structures from the Diexipaleo-dammed lakes in the upper reaches of the Minjiang River, east Tibet. Journal of Asian Earth Sciences 40 (4): 865–872.
Wang XQ, Wang LS (2013) The pollen and spore characteristics of the Diexi ancient dammed lake on the upstream of Minjiang River. Earth Science—Journal of China University of Geosciences 38 (5): 975–982. DOI: 10.3799/dqkx.2013.095 (In Chinese)
Wang XQ, Li YR, Yuan Y, et al. (2014) Palaeoclimate and palaeoseismic events discovered in Diexi barrier lake on the Minjiang River, China. Nat. Hazards Earth Syst. Sci. 14, 2069–2078. DOI: 10.5194/nhess-14-2069-2014
Wang X, Wang MZ (2012) The discovery and geological preliminary investigation of a slump-slip soft-sediment deformation multilayer complex structure in Neoproterozoic strata in Shouxian County, Anhui Province. Acta Geoscientica Sinica 33 (1): 49–56. (In Chinese)
Wang XQ, Wang LS, Shen JH (2010) Granularity analysis of sediments in Diexi ancient dammed lake on the upstream of Minjiang River and its environmental significance. Journal of Engineering Geology 18 (5): 677–684. DOI: 10.3969/j.issn.1004-9665.2010.05.011 (In Chinese)
Wang YH, Cheng W, Lu F, et al. (2007) Development of the shaking table. Earthquake Resistant Engineering and Retrofitting 29 (5): 53–56. DOI: 10.3969/j.issn.1002-8412.2007.05.011 (In Chinese)
Yang JP, Nie LL, Yang J (2008) Soft-sediment deformation structures of neogene related to earthquake and its geological significance in the southwestern Margin of Qaidam basin. Acta Sedimentologica Sinica 26 (6): 967–974. (In Chinese)
Yang WT, Wang XF, Yang JH et al. (2011) Soft-sediment deformation structures caused by palaeoearthquake in the Middle-Late Triassic in Yima area, western Henan Province. Journal of Palaeogography 13 (6): 635–644. (In Chinese)
Yuan XM, Sun R, Meng JS (2004) Research on mechanism for earthquake-induced differential settlement of building on soft subsoil. China Civil Engineering Journal 37 (2): 68–72. DOI: 10.3321/j.issn:1000-131X.2004.02.012 (In Chinese)
Zhang KG, Liu SY. (2010) Soil mechanics. China Architecture & Building Press: 209–210. (In Chinese)
Zhang CH, Wu ZJ, Gao LZ, et al. (2007) Characteristics of soft sediment deformation structure by earthquake. Science China Press 37 (3): 336–343. DOI: 10.3321/j.issn:1006-9267.2007.03.006 (In Chinese)
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Wei, Yf., Wang, Xq., Sheng, M. et al. Reproduction of the sedimentary disturbance phenomenon of the Diexi ancient landslide-dammed lake under earthquake. J. Mt. Sci. 12, 1181–1188 (2015). https://doi.org/10.1007/s11629-015-3460-7
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DOI: https://doi.org/10.1007/s11629-015-3460-7