1 School of Civil Engineering,Shandong Jianzhu University,Jinan 250101,Shandong; 2 Earthquake Engineering Research Center of Shandong Province,Jinan 250014,Shandong; 3 Shandong Institute of Geological Science,Jinan 250013,Shandong
Abstract：The Yishu Fault Zone cut through the central part of Shandong Province and it belongs to the middle segment of the Tanlu Fault Zone. So far,25 seismic event horizons have been identified from Neoproterozoic-Cenozoic strata within the Yishu Fault Zone and its adjacent area . Names of these seismic event horizons are derived from some lithostrata with seismic records of different times or ages. Most of seismic records are seismites,but a small quantity of records are seismic volcanic rocks in these horizons. Spatio-temporal distribution features of seismic event horizons support that the history of generating,activity and development of the fault zone is divided into two stages: The Palaeo-Tanlu Fault Zone stage (from Neoproterozoic to Paleozoic) and the Mesozoic-Cenozoic stage. The formation of the ductile-shear zone with the NNE trending from the central part of Shandong to the northern part of Jiangsu-Anhui linked up the transform faults with the NEE trending between the Qinling-Dabie Ocean and the Sulu Ocean in the initial Neoproterozoic,which may be the origin mechanism of the Yishu Fault Zone or the Palaeo-Tanlu Fault Zone. In the vertical,8 seismic event horizons were formed during the Palaeo-Tanlu Fault Zone stage,therein,5 seismic event horizons densely distributed in Nanhuain to Lower-Middle Cambrian;however,17 seismic event horizons were formed in the Mesozoic-Cenozoic stage,in which 12 horizons densely distributed in Cretaceous-Paleogene. Therefore,the Nanhuain to the Early-Middle Cambrian and the Cretaceous to the Paleogene were the two time intervals of frequent respectively and strong seismic events developed during the two stage. In the two different development stages,tectonic-dynamic sources of seismic activity of the fault zone were different: The dynamic source mainly came from the opposite movement or collision between the North China Plate and the Southern China Plate in the Palaeo-Tanlu Fault Zone;but during the Mesozoic-Cenozoic stage,that mainly from the subduction of the Pacific plate toward the Eurasian plate. In the horizontal,15 seismic event horizons distributed in the fault zone or extended from the fault zone to its both sides,which reflects that the Yishu Fault Zone has been the main part of seismogenic structures in the research area. All of these seismic event strata distributed in syn-sedimentary basins within 150~180,km on both sides of the longitudinal axis of the fault zone,which proves that peripheries on the two sides of the deep fracture zone have been active areas of strong tectonic earthquakes. Expounding and diagrams on the time-space distribution of seismic event horizons have reconstructed the basic process and the history of seismic action of the Yishu Fault Zone for the first time,and clearly delineated the influence scope of the long-active seismic zone in the paper,which are important significance not only to analyze earthquake-induced soft sediment deformations and seismic action in the such large active fault zone and its vicinities,but also to evaluate seismic damage effects surface and buildings in such seismic zone.
Tian Hongshui,Zhu Jiewang,Wang Hualin et al. Spatio-temporal distribution and significance of seismic event horizon in the Yishu Fault Zone and its adjacent area[J]. JOPC, 2017, 19(3): 393-417.
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