【摘要】 笔者 1999— 2 0 0 3年在华北太行山区和北京地区多次进行洞穴调查 ,发现很多古地震遗迹。文中论述了岩溶古地震研究的原理与依据 ,以及岩溶古地震遗迹的主要特征与岩溶古地震标志 ,对辨别洞穴正常岩溶现象与岩溶古地震遗迹的问题提出了新的方法 ,指出了在岩溶古地震调查时应注意的问题更多还原

【Abstract】 Karst caves are an ideal place for palaeoseismic research.This paper introduces at first the basic prin-ciple and method for the research of palaeosecsmic traces in karst caves.Under normal condition,stalac-tite,drips and stalagmite in cave are arranged as a system following a common vertical line.During earth-quake they are dislocated,and the vertical median line among them is displaced;the stalagmite is de-formed(e.g.broken off),while after the earthquake a new stalagmite may grow on the remaining base of old stalagmite,on the fallen stalagmite or on new place,and then a new system of stalactite,drip and sta-lagmite will be aligned along a new vertical line again.With the alternation of earthquake and non-earth-quake processes,the time-space correlation of the varied vertical lines may constitute“a natural pendu-lum”,which swing successively,just like a“seismograph”recording permanently palaeoseismic events oc-curred near the cave in different times.The investigation of the time-space correlation among these cave deposits may provide valuable information about palaeoseismic events in that region. Furthermore,the main characteristics of palaeoseismic traces and the indicators of palaeoseismic events in karst caves are demonstrated in this paper.When an earthquake occurs,the landscape of the caves may be destroyed and deformed.The distribution of the traces of paleoseismic events in the cave shows statistically a preferred orientation.During earthquake the vertical median line between the stalactite and stalagmite may be displaced or deformed laterally,in contrast to the normal phenomenon in karsts cave.The vertical projection of the collapsed roof on the floor of the cave is not coincident with the extent of colluvial deposits,which are displaced laterally.The distribution of slightly sorted colluvial deposits on the floor of the branch caves shows a preferred orientation.These earthquake-produced characteristics differ significantly from those of gravity collapse deposits in the cave. This study shows that the indicators of paleoseismic events in karst cave can be enumerated as fol-lows:the dislocation of karsts cave and/or its corridor along vertical,horizontal or oblique fault planes;displacement of rock mass,existence of earthquake fault and earthquake groove(line or fracture);rock splitting and lateral dislocation or pull-apart of stone column;lateral displacement of vertical median axis between stalactite and stalagmite;deformation of stalagmite(dislocation,riving,dumping and tilting)and earthquake-induced deformation of cave deposits. It is worth noting that the investigation of paleoseismic traces in karst caves should be carried out at the beginning of the exploration of the karst caves,so that geological phenomena generated by aseismic fac-tors in the cave can be distinguished.更多还原