Ground Structure and Strong Motions in the Grenoble Basin

格勒诺布尔盆地的地面结构和强烈运动

基本信息

批准号：
18404006
负责人：
KAWASE Hiroshi
金额：
$ 3.13万
依托单位：
KYUSHU UNIVERCITY
依托单位国家：
日本
项目类别：
Grant-in-Aid for Scientific Research (B)
财政年份：
2006
资助国家：
日本
起止时间：
2006 至 2007
项目状态：
已结题

来源：
https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-18404006/
关键词：
Array Microtremors Strong Motions Sedimentary Basin Grenoble Underground Structure

项目摘要

What we would like to clarify in the present study is whether the estimation of strong ground motion and the estimation of damage scheme that Japan has developed aggressively in these years are similarly effective in Europe where the geological environment is different very much from Japan. To this end we investigated the underground structure of the Grenoble basin by using microtremor measurement in cooperation with the Grenoble University in France who offered us a joint research for the purpose. We then perform ground motion prediction study for the Grenoble city. It is expected to show that the strong ground motion prediction technology that has been developed as a Japanese original technology has the generality that can be applied to the region where the geological environment is quite different.The extremely long duration of the seismic ground motion were observed in the Laffrey 2005 event that had been occurred in the south of the Grenoble basin in 2005. We first extract information of duration and wave energy in comparison to the other events. We also use simulation results of the three-dimensional finite difference methods for the Grenoble basin. It was able to be pointed out that a long duration can be introduced if we assume considerably weak surface layers on top of the surrounding rock formations. As is quite natural an introduction of soft layers on top of sediments makes duration even longer and successfully reproduces durations at most of the site within the basin. However, very long duration in the northeastern part of the basin can only be explained by considering the very soft, weathered layer.On the other hand, it has been understood that the analysis of the ground survey in the region is advanced, and a weak surface of the layer thickness of about 25m exists in the surface in boring and the array measurement of microtremors. Therefore, the possibility of the soft surface sediments is high that create very long duration in the observed waveforms.

我们在本研究中想澄清的是，日本这些年积极开发的强地震动估计和损害估计方案在地质环境与日本截然不同的欧洲是否同样有效。为此，我们与法国格勒诺布尔大学合作，通过微震测量来调查格勒诺布尔盆地的地下结构，法国格勒诺布尔大学为我们提供了联合研究。然后我们对格勒诺布尔市进行地面运动预测研究。预计将表明，作为日本原创技术而开发的强地震动预测技术具有通用性，可以适用于地质环境差异较大的地区。观测到持续时间极长的地震地震动2005 年在格勒诺布尔盆地南部发生的 Laffrey 2005 事件中。我们首先提取与其他事件相比的持续时间和波浪能量信息。我们还使用了格勒诺布尔盆地三维有限差分法的模拟结果。可以指出的是，如果我们假设周围岩层顶部的表层相当薄弱，则可以引入较长的持续时间。很自然地，在沉积物顶部引入软层使得持续时间更长，并成功地再现了盆地内大部分地点的持续时间。然而，盆地东北部的持续时间非常长，只能通过考虑非常软的风化层来解释。另一方面，据了解，该地区的地面调查分析是先进的，但弱在钻孔和阵列测量中表面存在约25m的地层厚度的微动。因此，软表面沉积物的可能性很高，在观测到的波形中产生很长的持续时间。

项目成果

期刊论文数量（0）

专著数量（0）

科研奖励数量（0）

会议论文数量（0）

专利数量（0）

Site Effects Derived from Spectral Inversion Method for K-NET, KiK-net, and JMA Strong-Motion Network with Special Reference to Soil Nonlinearity in High PGA Records

DOI：
发表时间：
2006
期刊：
影响因子：
0
作者：
H. Kawase
通讯作者：
H. Kawase

Borehole Observation for Site Effect Studies

场地效应研究的钻孔观察

DOI：
发表时间：
2006
期刊：
Proc.of Third International Symposium on the Effects of Surface Geology on Seismic Motion, Grenoble, France 1(CD-ROM)
影响因子：
0
作者：
川本伸一;鉾井修一;小椋大輔;宇野朋子;川本伸一・鉾井修一・宮内真紀子・小椋大輔・宇野朋子;Hiroshi Kawase
通讯作者：
Hiroshi Kawase

観測強震記録のスペクトルインバージョンで分離した統計的地震動特性に含まれる予測誤差

预测误差包含在统计地震动特征中，通过观测到的强震动记录的谱反演来分离