Comparison of correlation between magnetic susceptibility and grain size for lacustrine sediments in eastern Tibetan Plateau and loess deposits in Chinese Loess Plateau
Shi Wei1,2, Jiang Han-Chao1
1 State Key Laboratory of Earthquake Dynamics,Institute of Geology,China Earthquake Administration,Beijing 100029,China; 2 College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100049,China
Abstract:To explore the correlation between magnetic susceptibility(SUS)and grain size of the dust deposits from the tectonically stable and active regions and its implications for environmental events,the grain size and SUS records from the Lantian loess sediments-paleosol of the Chinese Loess Plateau(CLP)were analyzed and compared with that of the lacustrine sediments from the eastern margin of the Tibetan Plateau(TP). Results indicate that the SUS of the loess sediments has the strongest positive correlation with the loess sediments of 2~10 μm grain size in the Chinese Loess Plateau(CLP) and strongest negative in the Tibetan Plateau,respectively,indicating that the 2~10 μm grain size of dust sediments were continuous and stable,which were deposited in the background of the arid to semi-arid regions in the CLP and TP and even in Asia. On the other hand,SUS showed the strongest positive correlation with the 32~63 μm grain size of the loess sediments in the Tibetan Plateau and strongest negative in the Chinese Loess Plateau(CLP),respectively,indicating that the 32~63 μm grain size of the dust sediments were the sensitive indicator not only for the dust storms in the CLP, but also for the seismic events in the eastern margin of the TP. The correlation between SUS and grain size during the beginning period of the seismic event in the eastern part of TP was higher than that of the ending period,indicating that the seismic event brings the fresh sediments in the study area and then decreases due to the gradual recovery of the landscape. The correlation between SUS and grain size is also influenced by the local provenance.
Shi Wei,Jiang Han-Chao. Comparison of correlation between magnetic susceptibility and grain size for lacustrine sediments in eastern Tibetan Plateau and loess deposits in Chinese Loess Plateau[J]. JOPC, 2022, 24(3): 599-610.
[1] 丁海容,马光文,倪师军,施泽明,赵国华,闫亮,颜照坤. 2014. 汶川地震滑坡与强降雨驱动的输沙量增加研究: 以岷江上游为例. 四川大学学报: 工程科学版, 46(3): 49-55. [Ding H R,Ma G W,Ni S J,Shi Z M,Zhao G H,Yan L,Yan Z K.2014. Study on sediment discharge increase caused by Wenchuan earthquake landslide and heavy rainfall in the upper reaches of the Min River. Journal of Sichuan University(Engineering Science Edition), 46(3): 49-55] [2] 李艳豪,蒋汉朝,徐红艳,梁莲姬. 2015. 四川岷江上游滑坡触发因素分析. 地震地质, 37(4): 1147-1161. [Li Y H,Jiang H C,Xu H Y,Liang L J.2015. Analyses on the triggering factors of large quantities of landslides in the upper reaches of the Min River,Sichuan Province. Seismology and Geology, 37(4): 1147-1161] [3] 李勇,曹叔尤,周荣军,Densmore A L,Ellis M A.2005. 晚新生代岷江下蚀速率及其对青藏高原东缘山脉隆升机制和形成时限的定量约束. 地质学报, 79(1): 28-37. [Li Y,Cao S Y,Zhou R J,Densmore A L,Ellis M A.2005. Late Cenozoic Minjiang incision rate and its constraint on the uplift of the eastern margin of the Tibetan Plateau. Acta Geologica Sinica, 79(1): 28-37] [4] 李永昭,郭兵. 2008. 成都平原的晚新生代构造. 成都理工大学学报(自然科学版), 35(4): 371-376. [Li Y Z,Guo B.2008. Cenozoic tectonics of Chengdu plain,Sichuan,China. Journal of Chengdu University of Technology(Science & Technology Edition), 35(4): 371-376] [5] 刘明. 2014. 岷江河谷危石风洞试验研究. 成都理工大学硕士论文. [Liu M.2014. Research on the risk stone under wind loading with wind tunnel test in the Min River Valley. Masteral dissertation of Chengdu University of Technology] [6] 毛雪,蒋汉朝,杨桂芳,徐红艳. 2011. 中国末次冰消期古气候时空演化特征初探. 第四纪研究, 31(1): 59-67. [Mao X,Jiang H C,Yang G F,Xu H Y.2011. Preliminary study on spatial and temporal characteristics of palaeoclimate evolution in China during the last deglaciation. Quaternary Science, 31(1): 59-67] [7] 四川省地质矿产局. 1991. 四川省区域地质志. 北京: 地质出版社,1-680. [Sichuan Provincial Bureau of Geology and Mineral Resources. 1991. Regional Geology of Sichuan Province. Beijing: Geological Publishing House,1-680] [8] 张岳桥,杨农,孟晖. 2005. 岷江上游深切河谷及其对川西高原隆升的响应. 成都理工大学学报(自然科学版), 32(4): 331-339. [Zhang Y Q,Yang N,Meng H.2005. Deep-incised valleys along the Minjiang River upstream and their responses to the uplift of the West Sichuan Plateau,China. Journal of Chengdu University Technology(Science & Technology Edition), 32(4): 331-339] [9] 钟宁,蒋汉朝,李海兵,徐红艳,梁莲姬,时伟. 2020. 岷江上游新磨村湖相沉积物粒度端元反演及其记录的构造和气候事件. 地质学报, 94(3): 968-981. [Zhong N,Jiang H C,Li H B,Xu H Y,Liang L J,Shi W.2020. End member inversion of Xinmocun lacustrine sediments in the upper reaches of the Minjiang River and its recorded tectonic and climate events. Acta Geological Sinica, 94(3): 968-981] [10] Balsam W L,Ellwood B B,Ji J F,Williams E R,Long X Y,Hassani A E.2011. Magnetic susceptibility as a proxy for rainfall: worldwide data from tropical and temperate climate.Quaternary Science Reviews, 30(19-20): 2732-2744. [11] Ding Z,Yu Z,Rutter N W,Liu T.1994. Towards an orbital timescale for Chinese loess deposits.Quaternary Science Reviews, 13(1): 39-70. [12] Hao Q Z,Guo Z T.2005. Spatial variations of magnetic susceptibility of Chinese loess for the last 600 kyr: implications for monsoon evolution. Journal of Geophysical Research(Solid Earth), 110(B12): doi: 10.1029/2005JB003765. [13] Hao Q Z,Oldfield F,Bloemendal J,Guo Z T.2008. Particle size separation and evidence for pedogenesis in samples from the Chinese Loess Plateau spanning the last 22 m.y. Geology, 36(9): 727-730. [14] Heller F,Liu T S.1982. Magnetostratigraphical dating of loess deposits in China. Nature, 300(5891): 431-433. [15] Heller F,Liu T S.1984. Magnetism of Chinese loess deposits. Geophysical Journal International, 77(1): 125-141. [16] Jiang H C,Ding Z L.2005. Temporal and spatial changes of vegetation cover on the Chinese Loess Plateau through the last glacial cycle: evidence from spore-pollen records. Review of Palaeobotany and Palynology, 133(1-2): 23-37. [17] Jiang H C,Mao X,Xu H Y,Yang H L,Ma X L,Zhong N,Li Y H.2014. Provenance and earthquake signature of the last deglacial Xinmocun lacustrine sediments at Diexi,East Tibet. Geomorphology, 204: 518-531. [18] Jiang H C,Shevenell A,Yu S,Xu H Y,Mao X.2015. Decadal-to centennial-scale East Asian summer monsoon variability during the Medieval Climate Anomaly reconstructed from an eastern Tibet lacustrine sequence. Journal of Paleolimnology, 54(2-3): 205-222. [19] Jiang H C,Zhong N,Li Y H,Xu H Y,Yang H L,Peng X N.2016. Soft sediment deformation structures in the Lixian lacustrine sediments,eastern Tibetan Plateau and implications for postglacial seismic activity. Sedimentary Geology, 344: 123-134. [20] Jiang H C,Zhong N,Li Y H,Ma X L,Xu H Y,Shi W,Zhang S Q,Nie G Z.2017. A continuous 13.3-ka record of seismogenic dust events in lacustrine sediments in the eastern Tibetan Plateau. Scientific Reports, 7(1): 15686. doi: 10.1038/s41598-017-16027-8. [21] Kukla G,An Z S.1989. Loess stratigraphy in central China. Palaeogeography, Palaeoclimatology, Palaeoecology, 72(89): 203-225. [22] Kukla G,Heller F,Liu X M,Xu T C,Liu T S,An Z S.1988. Pleistocene climates in China dated by magnetic susceptibility. Geology, 16(9): 811-814. [23] Kukla G,An Z S,Melice J L,Gavin J,Xiao J L.1990. Magneti susceptibility record of Chinese loess.Transactions of the Royal Society of Edinburgh Earth Sciences, 81(4): 263-288. [24] Liang L J,Jiang H C.2017. Geochemical composition of the last deglacial lacustrine sediments in east Tibet and implications for provenance,weathering,and earthquake events.Quaternary International, 430: 41-51. [25] Maher B A,Thompson R.1991. Mineral magnetic record of the Chinese loess and paleosol. Geology, 19(1): 3-6. [26] Meng X M,Derbyshire E,Kemp R A.1997. Origin of the magnetic susceptibility signal in Chinese loess.Quaternary Science Reviews, 16(8): 833-839. [27] Nie J S,Song Y G,King J W,Egli R.2010. Consistent grain size distribution of pedogenic maghemite of surface soils and Miocene loessic soils on the Chinese Loess Plateau. Journal of Quaternary Science, 25(3): 261-266. [28] Shi W,Jiang H C,Mao X,Xu H Y.2020. Pollen record of climate change during the last deglaciation from the eastern Tibetan Plateau. Plos One, 15(5): e0232803. https://doi.org/10.1371/journal.pone.0232803. [29] Sun J M,Liu T S.2000. Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments.Earth and Planetary Science Letters, 180(3-4): 287-296. [30] Tsoar H,Pye K.1987. Dust transport and the question of desert loess formation. Sedimentology, 34(1): 139-153. [31] Verosub K L,Fine P,Singer M J,TenPas J.1993. Pedogenesis and paleoclimate: interpretation of the magnetic susceptibility record of Chinese loess-paleosol sequences. Geology, 21(11): 1011-1014. [32] Wang X,Peng P A,Ding Z L.2005. Black carbon records in Chinese loess plateau over the last two glacial cycles and implications for paleofires.Palaeogeography, Palaeoclimatology, Palaeoecology, 223(1-2): 9-19. [33] Zhang H P,Liu S F,Yang N,Zhang Y Q,Zhang G W.2006. Geomorphic characteristics of the Minjiang drainage basin(eastern Tibetan Plateau)and its tectonic implications: new insights from a DEM study.Island Arc, 15(2): 239-250. [34] Zhang P Z,Deng Q D,Zhang G M,Ma J,Gan W J,Min W,Mao F Y,Wang Q.2003. Active tectonic blocks and strong earthquakes in the continent of China.Science in China(Series D), 46: 13-24. [35] Zhong N,Song X S,Xu H Y,Jiang H C.2017. Influence of a tectonically active mountain belt on its foreland basin: evidence from detrital zircon dating of bedrocks and sediments from the eastern Tibetan Plateau and Sichuan Basin,SW China. Journal of Asian Earth Sciences, 146: 251-264. [36] Zhou L P,Oldfield F,Wintle A G,Robinson S G,Wang J T.1990. Partly pedogenic origin of magnetic variations in Chinese loess.Nature, 346: 737-739.