GROUND DEFORMATION DUE TO FAULT RUPTURE AND LIQUEFACTION DURING THE 1999 KOCAELI AND DUZCE, TURKEY, EARTHQUAKES:

CMS0085306PI：Jean-Pierre Bardet机构：题目：“1999年土耳其科贾埃利和杜兹切地震期间由于地表断层和隆起而引起的地震变形“摘要1999年土耳其科贾埃利和杜兹切地震期间，地表断层对建筑物和生命线造成了重大破坏。这是第一次地表断层对城市和工业区的影响达到如此程度，并对我们目前的地震工程实践提出了重大关注。在1999年土耳其科贾埃利地震中，由于地壳运动引起的横向扩展和伊兹米特湾和萨潘卡湖沿岸的沿着沉降，也造成了重大破坏。本探索性研究的目的是测量1999年土耳其科贾埃利和杜兹切地震中地表断层和液化引起的地面变形。这些信息将通过互联网传播给研究人员和从业人员，将有助于改进断层作用引起的横向扩展模型和地表断层作用的缓解标准。拟议的探索性研究完成了地震侦察队在地震发生后立即进行的工作，随后由我们在土耳其的研究合作者进行。地表断层的不连续位错已被地质学家填图，但地表断层周围的连续应变场尚未被测量。地震前后拍摄的航空照片还有待于解释，以产生对地面变形和破坏机制的大规模理解，特别是在两个走滑链之间的跨越（例如，Golcuk）。同样的图像处理技术也需要应用于产生摩擦引起的地面变形的地图（例如，萨潘卡湖）。航空照片的处理和解释将有助于理解1999年土耳其Kocaeli和Duzce地震期间观察到的大规模地面变形和破坏机制。拟议的探索性研究的目标是：（1）澄清和整理关于1999年土耳其科贾埃利和杜兹切地震的地表断层和液化引起的地面变形的现有数据;（2）处理地震前后拍摄的航空照片，以制作地表断层和液化引起的永久位移矢量和沉降图;（3）收集额外的地面调查以及地质和岩土土壤剖面数据（例如，（4）在因特网上传播通过新的地理信息系统平台（因特网地图服务器）收集的信息。

CMS0085306PI: Jean-Pierre BardetInstitution: University of Southern CaliforniaTitle: "GROUND DEFORMATION DUE TO SURFACE FAULTING AND LIQUEFACTION DURING THE 1999 KOCAELI AND DUZCE, TURKEY, EARTHQUAKES"AbstractDuring the 1999 Kocaeli and Duzce, Turkey, earthquakes, surface faultingcaused substantial damage to structures and lifelines. It is the first timethat surface faulting impacts urban and industrial areas to such an extent,and raises major concerns about our current practices in earthquakeengineering. During the 1999 Kocaeli, Turkey, earthquake, there was alsomajor damage due to liquefaction-induced lateral spreads and coastalsubsidences along the coasts of the Bay of Izmit and Lake Sapanca. Theobjective of this proposed exploratory research is to measure grounddeformations caused by surface faulting and liquefaction during the 1999Kocaeli and Duzce, Turkey earthquakes. This information, which will bedisseminated to researchers and practitioners via the Internet, willcontribute to improving models for liquefaction-induced lateral spreads andmitigation criteria for surface faulting effects. The proposed exploratory research completes the work performed immediatelyafter the earthquakes by the earthquake reconnaissance teams andsubsequently by our research collaborators in Turkey. The discontinuousdislocations from surface faulting have already been mapped by geologists.However, the continuous fields of ground strain surrounding surfacefaulting have not yet been measured. The aerial photographs taken prior andafter the earthquakes are yet to be interpreted to yield a large-scaleunderstanding of ground deformation and failure mechanisms, especially instepovers between two strike-slip strands (e.g., Golcuk). The same imageprocessing techniques need also to be also applied for producing maps ofliquefaction-induced ground deformations (e.g., Sapanca Lake). Theprocessing and interpretation of aerial photographs will be instrumental inunderstanding the large-scale ground deformation and failure mechanismsobserved during the 1999 Kocaeli and Duzce, Turkey, earthquakes. The objectives of the proposed exploratory research are: (1) Compilationand organization of existing data on surface-faulting andliquefaction-induced ground deformation for the 1999 Kocaeli and Duzce,Turkey, earthquakes; (2) Processing of aerial photographs taken prior toand after the earthquakes for producing maps of permanent displacementvectors and settlements induced by surface faulting and liquefaction; (3)Collection of additional ground surveys, and data on geology andgeotechnical soil profiles (e.g., SPT and CPT soundings) in selected areas;and (4) Dissemination of information collected thorough a new GIS platform(Internet Map Server) on the Internet.