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Abstract: <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> Earthquake risk study basicly is a function of shaking effect value, local effect, and population factor. This study conduct to analyze and compare a risk pattern using maximum...
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id-itb.:69582017-10-09T10:31:13Z#TITLE_ALTERNATIVE# Firmansyah (NIM 124 02 021), Yusi Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/6958 Abstract: <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> Earthquake risk study basicly is a function of shaking effect value, local effect, and population factor. This study conduct to analyze and compare a risk pattern using maximum PGA (Peak Ground Acceleration) with avearage PGA by 18 fault model with few simplification such as: Shaking effect factor expressed by an estimation of PGA and population factor expressed by population density value (N). Otherwise, a local effect assumed have the same value. By the assumption we have a risk as a linear function of PGA times N. Fault model which is used in this study is courtesy of Seismotectonic Map (E.K. Kertapati et al., 1998). Those fault model used as an earthquake resource to estimate a shaking effect value. The result obtained is a risk map of the study area. By using different PGA estimation we obtained a risk patterns which is apparently the same but have a different vulnerable intentisty value <br /> text |
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Abstract: <br />
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Earthquake risk study basicly is a function of shaking effect value, local effect, and population factor. This study conduct to analyze and compare a risk pattern using maximum PGA (Peak Ground Acceleration) with avearage PGA by 18 fault model with few simplification such as: Shaking effect factor expressed by an estimation of PGA and population factor expressed by population density value (N). Otherwise, a local effect assumed have the same value. By the assumption we have a risk as a linear function of PGA times N. Fault model which is used in this study is courtesy of Seismotectonic Map (E.K. Kertapati et al., 1998). Those fault model used as an earthquake resource to estimate a shaking effect value. The result obtained is a risk map of the study area. By using different PGA estimation we obtained a risk patterns which is apparently the same but have a different vulnerable intentisty value <br />
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Firmansyah (NIM 124 02 021), Yusi |
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Firmansyah (NIM 124 02 021), Yusi #TITLE_ALTERNATIVE# |
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Firmansyah (NIM 124 02 021), Yusi |
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Firmansyah (NIM 124 02 021), Yusi |
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https://digilib.itb.ac.id/gdl/view/6958 |
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