Evidences that epicenter of ‘Taishan earthquake’ was located in Anqiu area of Tanlu fault zone
ZHANG Banghua1, TIAN Hongshui2, YANG Chuancheng3, ZHANG Shenhe2
1 College of Surveying & Geoinformatics, Shandong Jianzhu University,Jinan 250101, China; 2 School of Civil Engineering, Shandong Jianzhu University, Jinan 250101, China; 3 Earthquake Engineering Research Center of Shandong Province, Jinan 250014, China
Abstract The‘Taishan earthquake’ named after Mount Taishan,occurred in 1831 BC,which was the earliest historical earthquake recorded by writing-materials in China. Bamboo Annals recorded that the strong earthquake occurred,when the emperor named “Fa” was climbing the Mount Taishan in the seventh year of Xia Di Fa(i.e.1831 BC). The earthquake shocked the emperor at that time,so for the first time,it was written and named after Mount Taishan. Apparently,the geographical position that the emperor “Fa” was threatened by the earthquake was at the hillside of the Mount Taishan. However,seismic geologists have been unable to find any seismic-geological records or traces of the historical earthquake in the Taishan area and its surroundings. Therefore,the epicenter and magnitude of the “Taishan earthquake” have been a mystery. By reobserving the discovered seismo-geological remains,combined with a series of tests,experiments and analysis,the paper provides evidences that the “Taishan earthquake” was a strong and historical earthquake with its epicenter located in the Anqiu area within the Tanlu fault zone. First of all,in the Holocene soft soil layers of limnetic facies in the Anqiu-Xiazhuang Basin of the Tanlu fault zone about 200 km away from Mount Taishan,there are macroscopical seismic traces such as seismic-subsidence synclines and co-seismic micro-faults,which recorded epicenter-intensity for degree of IX ,seismic magnitude for M7.0. Second,by means of the results of dating14C isotope,combining with calculating the sedimention time of the related soil layer,the earthquake time(i.e.1827 BC)obtained is very close to 1831 BC. Third,based on seismic intensity attenuation model in North China,the attenuation intensity induced by the earthquake is calculated to the degree of VI near Taishan. The Chinese earthquake intensity table shows that the VI intensity completely makes people stand unstable or escape outdoors,which accords with the historical records that the mountaineering emperor was frightened by the earthquake.
Fund:Co-funded by the Doctoral Fund Program of Shandong Jianzhu University(No.XNBS1708),the National Natural Science Foundation of China(No.41272066)and the National Science and Technology Major Project(No.BAK19B04-01)
About author: ZHANG Banghua,born in 1970,Ph.D.,an associate professor,is engaged in geography and seismic events research. E-mail: banghuazhang@163.com.
Cite this article:
ZHANG Banghua,TIAN Hongshui,YANG Chuancheng et al. Evidences that epicenter of ‘Taishan earthquake’ was located in Anqiu area of Tanlu fault zone[J]. JOPC, 2024, 26(3): 714-724.
ZHANG Banghua,TIAN Hongshui,YANG Chuancheng et al. Evidences that epicenter of ‘Taishan earthquake’ was located in Anqiu area of Tanlu fault zone[J]. JOPC, 2024, 26(3): 714-724.
[1] 晁洪太,李家灵,崔昭文,满洪敏,杜宪宋. 1995. 郯庐活断层与1668年郯城8.5级地震灾害. 海洋地质与第四纪地质, 15(3): 69-80. [Chao H T,Li J L,Cui Z W,Man H M,Du X S.1995. Active faults in Tanlu(Tancheng-Lujiang)fault zone and the hazards produced by the 1668 Tancheng earthquake(M=8.5). Marine Geology & Quaternary Geology, 15(3): 69-80] [2] 晁洪太,李家灵,崔昭文,赵清玉. 1997. 郯庐断裂带潍坊—嘉山段全新世活断层的活动方式与发震模式. 地震研究, 20(2): 218-226. [Chao H T,Li J L,Cui Z W,Zhao Q Y.1997. Mode of motion of the Holocene fault in Weifang-Jiashan segment of the Tanlu fault zone and earthquake-generating model. Journal of Seismological Research, 20(2): 218-226] [3] 晁洪太,王志才,李家灵,崔昭文. 1999. 山东泰安地区断层的最新活动与“泰山震”. 地震地质, 21(2): 105-114. [Chao H T,Wang Z C,Li J L,Cui Z W.1999. The latest activities of faults in the Tai’an region,Shandong Province and the Taishan Mountain earthquake. Seismology and Geology, 21(2): 105-114] [4] 陈希哲,叶菁. 2013. 土力学地基基础. 5版. 北京: 清华大学出版社. [Chen X Z,Ye J.2013. Soil Mechanics and Geotechnical Engineering. 5th Ed. Beijing: Tsinghua University Press] [5] 崔鑫,苗庆杰,王金萍. 2010. 华北地区地震烈度衰减模型的建立. 华北地震科学, 28(2): 18-21. [Cui X,Miao Q J,Wang J P.2010. Model of the seismic intensity attenuation for North China. North China Earthquake Sciences, 28(2): 18-21] [6] 冯增昭(主编). 2013. 中国沉积学·第2版. 北京: 石油工业出版社. [Feng Z Z(ed). 2013. Sedimentology of China. 2nd Ed. Beijing: Petroleum Industry Press] [7] 何碧竹,乔秀夫,田洪水,陈树清,张艳霞. 2011. 山东诸城晚白垩世古地震事件与恐龙化石埋藏. 古地理学报, 13(6): 615-626. [He B Z,Qiao X F,Tian H S,Chen S Q,Zhang Y X.2011. Palaeoearthquake event and dinosaur fossil burial of the Late Cretaceous in Zhucheng of Shandong Province. Journal of Palaeogeography(Chinese Edition), 13(6): 615-626] [8] 何碧竹,乔秀夫,田洪水,张艳霞. 2012. 山东诸城早白垩世莱阳期古地震事件与恐龙迁移. 地质学报, 86(8): 1320-1330. [He B Z,Qiao X F,Tian H S,Zhang Y X.2012. Paleoearthquake events of Early Cretaceous Laiyang stage and dinosaur migration in Zhucheng,Shandong Province,eastern China. Acta Geologica Sinica, 86(8): 1320-1330] [9] 侯万国,孙德军,张春光. 1998. 应用胶体化学. 北京: 科学出版社. [Hou W G,Sun D J,Zhang C G.1998. Applied Colloidal Chemistry. Beijing: Science Press] [10] 李冬,陈培雄,吕小飞,陈小玲. 2011. 软土地震震陷研究现状综述. 工程抗震与加固改造, 33(2): 130-135. [Li D,Chen P X,Lü X F,Chen X L.2011. Research progress summarization of soft soil earthquake subsidence. Earthquake Resistant Engineering and Retrofitting, 33(2): 130-135] [11] 刘恢先. 1986. 唐山大地震震害—第二册. 北京: 地震出版社. [Liu H X.1986. Damage of Tangshan Earthquake: Volume Ⅱ. Beijing: Seismological Press] [12] 吕洪波,王俊,张海春. 2011. 山东灵山岛晚中生代滑塌沉积层的发现及区域构造意义初探. 地质学报, 85(6): 938-946. [Lü H B,Wang J,Zhang H C.2011. Discovery of the late Mesozoic slump beds in Lingshan Island,Shandong,and a pilot research on the regional tectonics. Acta Geologica Sinica, 85(6): 938-946] [13] 乔秀夫,高林志,彭阳. 2001. 古郯庐带新元古界—灾变·层序·生物. 北京: 地质出版社, 1-122. [Qiao X F,Gao L Z,Peng Y.2001. Neoproterozoic in Paleo-Tancheng-Lujiang Fault Zone,Catastrophes-Sequences-Biostratigraphy. Beijing: Geological Publishing House,1-122] [14] 施炜,张岳桥,董树文. 2003. 郯庐断裂带中段第四纪活动及其分段特征. 地球学报, 24(1): 11-18. [Shi W,Zhang Y Q,Dong S W.2003. Quaternary activity and segmentation behavior of the middle portion of the Tan-Lu fault zone. Acta Geosicientia Sinica, 24(1): 11-18] [15] 时振梁,李裕澈. 2001. 中国地震区划. 中国工程科学, 3(6): 65-68. [Shi Z L,Li Y C.2001. Seismic zonation in China. Engineering Science, 3(6): 65-68] [16] 宋明春,王沛成. 2003. 山东省区域地质. 山东济南: 山东省地图出版社. [Song M C,Wang P C.2003. Regional Geology of Shandong Province. Shandong Jinan: Map Press of Shandong Province] [17] 苏德辰,乔秀夫. 2018. 黏性沉积物中的古地震触变流动变形. 古地理学报, 20(4): 609-622. [Su D C,Qiao X F.2018. Thixotropic deformation features of cohesive sediments triggered by palaeoearthquakes. Journal of Palaeogeography(Chinese Edition), 20(4): 609-622] [18] 田洪水,万中杰,王华林. 2003. 鲁中寒武系馒头组震积岩的发现及初步研究. 地质论评, 49(2): 123-131,225. [Tian H S,Wan Z J,Wang H L.2003. Discovery and preliminary study on seismites of the Cambrian Mantou Formation in the central Shandong area. Geological Review, 49(2): 123-131,225] [19] 田洪水,张增奇,张邦花,杜圣贤,郭广军,吕明英. 2006. 山东临朐红丝石层中的古地震事件记录. 中国地质, 33(5): 1137-1143. [Tian H S,Zhang Z Q,Zhang B H,Du S X,Guo G J,Lü M Y.2006. Records of paleoseismic events in the red-silk stone bed in Linqu,Shandong. Geology in China, 33(5): 1137-1143] [20] 田洪水,李洪奎,王金光,郭广军,张增奇. 2007. 沂沭断裂带及其近区的地震成因岩石新认识. 地球学报, 28(5): 496-505. [Tian H S,Li H K,Wang J G,Guo G J,Zhang Z Q.2007. New recognition of seismogenic rocks in the Yishu fault zone and its periphery. Acta Geoscientica Sinica, 28(5): 496-505] [21] 田洪水,张邦花,祝介旺,张增奇,李洪奎. 2011. 早寒武世初期沂沭断裂带地震效应. 古地理学报, 13(6): 645-656. [Tian H S,Zhang B H,Zhu J W,Zhang Z Q,Li H K.2011. Seismic effects from Yishu Fault Zone during the earlier Early Cambrian. Journal of Palaeogeography(Chinese Edition), 13(6): 645-656] [22] 田洪水,王华林,祝介旺,杨传成,吕明英,张慎河. 2015a. 山东安丘地区软土震陷及地震产生的土层构造新启示. 岩土工程学报, 37(4): 734-740,771. [Tian H S,Wang H L,Zhu J W,Yang C C,Lü M Y,Zhang S H.2015a. New revelation from seismic subsidence of soft soils and earthquake-induced soil-layer deformation structures in Anqiu area,Shandong Province. Chinese Journal of Geotechnical Engineering, 37(4): 734-740,771] [23] 田洪水,张爱社,张慎河,张邦花,祝介旺,吕明英. 2015b. 饱和灰泥模拟地震试验与液化变形. 北京: 地震出版社. [Tian H S,Zhang A S,Zhang S H,Zhang B H,Zhu J W,Lü M Y.2015b. Simulation Earthquake Tests and Liquefied Deformations of the Saturated Lime-mud. Beijing: Seismological Press] [24] 田洪水,Van Loon A J,王华林,张慎河,祝介旺. 2016. 大盛群中的震积岩: 郯庐断裂带强构造与地震活动新证据. 中国科学: 地球科学, 46(1): 79-96. [Tian H S,Van Loon A J,Wang H L,Zhang S H,Zhu J W.2016. Seismites in the Dasheng Group: new evidences of strong tectonic and earthquake activities of the Tanlu Fault Zone. Scientia Sinica(Terrae), 46(1): 79-96] [25] 田洪水,祝介旺,王华林,张增奇,张邦花,张慎河. 2017. 沂沭断裂带及其近区地震事件地层的时空分布及意义. 古地理学报, 19(3): 393-417. [Tian H S,Zhu J W,Wang H L,Zhang Z Q,Zhang B H,Zhang S H.2017. Spatio-temporal distribution and significance of seismic event horizon in the Yishu Fault Zone and its adjacent area. Journal of Palaeogeography(Chinese Edition), 19(3): 393-417] [26] 王华林,晁洪太,耿杰. 1992. 鲁西北西向断裂的断层泥及其地震地质意义. 地震地质, 14(3): 265-273,289. [Wang H L,Chao H T,Geng J.1992. Characteristics of fault gouge from the nw-trending faults in West Shandong and its seismo-geological implications. Seismology and Geology, 14(3): 265-273,289] [27] 王志才,贾荣光,孙昭民,石荣会,晁洪太. 2005. 沂沭断裂带安丘—莒县断裂安丘—朱里段几何结构与活动特征. 地震地质, 27(2): 212-220. [Wang Z C,Jia R G,Sun Z M,Shi R H,Chao H T.2005. Geometry and activity of the Anqiu-Zhuli segment of the Anqiu-Juxian fault in theYishu fault zone. Seismology and Geology, 27(2): 212-220] [28] 王志才,王冬雷,许洪泰,葛孚刚,杨传成,李建虎. 2015. 安丘—莒县断裂北段几何结构与最新活动特征. 地震地质, 37(1): 176-191. [Wang Z C,Wang D L,Xu H T,Ge F G,Yang C C,Li J H.2015. Geometric features and latest activities of the north segment of the Anqiu-Juxian fault. Seismology and Geology, 37(1): 176-191] [29] 魏光兴,孙昭民. 2000. 山东省自然灾害史. 北京: 地震出版社. [Wei G X,Sun Z M.2000. History of Natural Disasters in Shandong Province. Beijing: Seismological Press] [30] 郁寿松,石兆吉. 1989. 土壤震陷试验研究. 岩土工程学报, 11(4): 35-44. [Yu S S,Shi Z J.1989. Experimental investigation of soil settlement due to earthquake. Chinese Journal of Geotechnical Engineering, 11(4): 35-44] [31] 杨剑萍,王亚丽,查明,牟雪梅. 2006. 山东惠民凹陷古近系湖泊地震涌浪记录的新发现. 地质学报, 80(11): 1715-1720,1790. [Yang J P,Wang Y L,Zha M,Mu X M.2006. Discovery of the seismic surge wave deposits record of Paleogene in Huimin depression,Shandong Province. Acta Geologica Sinica, 80(11): 1715-1720,1790] [32] 殷秀兰,杨天南. 2005. 胶州—莱阳盆地白垩纪莱阳群中的震积岩及构造意义讨论. 地质论评, 51(5): 502-506. [Yin X L,Yang T N.2005. Seismites in the Laiyang group in the Jiaozhou-Laiyang Basin,Shandong Province,and their tectonic implications. Geological Review, 51(5): 502-506] [33] 袁静. 2004. 山东惠民凹陷古近纪震积岩特征及其地质意义. 沉积学报, 22(1): 41-46. [Yuan J.2004. The property and geological significance of seismites of Paleogene in Huimin sag,Shandong Province. Acta Sedimentologica Sinica, 22(1): 41-46] [34] 张邦花,田洪水,张增奇,杜圣贤. 2012. 地质名山馒头山及其附近早寒武世古地震沉积事件研究. 沉积学报, 30(6): 1021-1031. [Zhang B H,Tian H S,Zhang Z Q,Du S X.2012. Paleoseismic depositional events of the famous geological mountain-Mantoushan and its vicinity in the Early Cambrian. Acta Sedimentologica Sinica, 30(6): 1021-1031] [35] 张邦花,田洪水,祝介旺. 2016. 山东郯城麦坡中更新世地震事件记录. 古地理学报, 18(5): 799-808. [Zhang B H,Tian H S,Zhu J W.2016. Records of the Pleistocene seismic events in Tancheng Maipo,Shandong Province. Journal of Palaeogeography(Chinese Edition), 18(5): 799-808] [36] 张邦花,田洪水,A.J.(Tom)van Loon.2017. 新元古代沂沭海峡地震引发的软沉积物变形及其微量元素信息. 古地理学报, 19(1): 99-116. [Zhang B H,Tian H S,Van Loon A J.2017. Earthquake-induced soft sediment deformations and their trace-element information in the Neoproterozoic Yishu Strait. Journal of Palaeogeography(Chinese Edition), 19(1): 99-116] [37] 张虎臣. 1989. 淤泥地基地震触变研究. 岩土工程学报, 11(3): 78-85. [Zhang H C.1989. Study on seismic thixotropy of silt foundation. Chinese Journal of Geotechnical Engineering, 11(3): 78-85] [38] 张明利,金之钧,吕朋菊,刘国林. 2000. 新生代构造运动与泰山形成. 地质力学学报, 6(2): 23-29. [Zhang M L,Jin Z J,Lü P J,Liu G L.2000. Formation of Taishan Mountain and Cenozoic tectonicism. Journal of Geomechanics, 6(2): 23-29] [39] 张久麒,孙锐,袁晓铭,侯龙清. 2017. 软土残余应变势简化计算公式及参数分析. 地震工程与工程振动, 37(5): 103-108. [Zhang J Q,Sun R,Yuan X M,Hou L Q.2017. The simplified formula for calculating the permanent strain potential of soft soil and parameter analysis. Earthquake Engineering and Engineering Dynamics, 37(5): 103-108] [40] 中华人民共和国国土资源部. 2004. 地质灾害分类分级(DZ0238-2004): 1-179. [Ministry of Land and Resources,PRC.2004. Classification of Geological Disasters(DZ0238-2004): 1-179] [41] 中华人民共和国标准化管理委员会. 2008. 中国地震烈度表(GB/T 17742-2008): 1-6. [Standardization Administration of the People’s Republic of China.2008. The Chinese Seismic Intensity Scale(GB/T 17742-2008): 1-6] [42] Bowman D,Korjenkov A,Porat N.2004. Late-pleistocene seismites from lake issyk-kul,the Tien Shan range,kyrghyzstan. Sedimentary Geology, 163: 211-228. [43] He B Z,Qiao X F.2015a. Advances and overview of the study on paleo-earthquake events: a review of seismites. Acta Geologica Sinica(English Edition), 89: 1702-1746. [44] He B Z,Qiao X F,Zhang Y L,Tian H S,Cai Z H,Chen S Q,Zhang Y X.2015b. Soft-sediment deformation structures in the Cretaceous Zhucheng depression,Shandong Province,East China;their character,deformation timing and tectonic implications. Journal of Asian Earth Sciences, 110: 101-122. [45] Liang L J,Dai F C,Jiang H C,Zhong N.2018. A preliminary study on the soft-sediment deformation structures in the late quaternary lacustrine sediments at tashkorgan,northeastern Pamir,China. Acta Geologica Sinica(English Edition), 92: 1574-1591. [46] Montenat C,Barrier P,Ott d'Estevou P,Hibsch C.2007. Seismites: an attempt at critical analysis and classification. Sedimentary Geology, 196: 5-30. [47] Qiao X F,Song T R,Gao L Z,Peng Y,Li H B,Gao M,Song B,Zhang Q D.1994. Seismic sequence in carbonate rocks by vibrational Liquefaction1. Acta Geologica Sinica-English Edition, 7: 243-265. [48] Tian H S,Zhang Z Q,Zhang B H,Zhu J W,Sang Z X,Li H K.2013. Tectonic taphrogenesis and paleoseismic records from the Yishu fault zone in the initial stage of the Caledonian movement. Acta Geologica Sinica(English Edition), 87: 936-947. [49] Tian H S,Van Loon A J,Zhang Z Q,Zhang S H,Zhang B H,Lü M Y,Li F C,Ma X M.2015. Neogene Paleoseismic events and the Shanwang biota’s burial in the Linqu area,Shandong Province,China. Acta Geologica Sinica(English Edition), 89: 1103-1119.
