Using Double Difference Earthquake Location Algorithm to Relocate the Aftershocks of Great Earthquakes in the Past Ten Years
碩士 === 國立中央大學 === 地球物理研究所 === 90 === The distribution of aftershocks often indicates the geological structure in that area and implies the type of fault rupture. Except of 1999 Chi-chi earthquake, most of earthquake in Taiwan did not cause surface rupture. It yields the ambiguous on determination of...
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ndltd-TW-090NCU051340032015-10-13T10:10:53Z http://ndltd.ncl.edu.tw/handle/77306100553490572807 Using Double Difference Earthquake Location Algorithm to Relocate the Aftershocks of Great Earthquakes in the Past Ten Years 利用雙差分地震定位演算法重新定位過去十年台灣中、大型地震之餘震 Chung-Han Chan 詹忠翰 碩士 國立中央大學 地球物理研究所 90 The distribution of aftershocks often indicates the geological structure in that area and implies the type of fault rupture. Except of 1999 Chi-chi earthquake, most of earthquake in Taiwan did not cause surface rupture. It yields the ambiguous on determination of rupture plane and its associated active fault. More accurate relocation of aftershocks might be able to help us on identification of its rupture plane and understanding its corresponding geological structure. In this paper, we reexam the aftershocks of several large earthquakes in the past ten years e.g. 1993 Da-Pu, 1994 Nan-Ao, 1998 Ruey-Li, 1999 Chi-Chi and 1999 Chia-I earthquakes. Using CWBSN data, we apply the “Double Difference Earthquake Location Algorithm” ( Waldhauser, F., Ellsworth, W. L., 2000 ) to relocate aftershocks and to understand their association with geological structure. Because of the concept of multiplet (a group of earthquake which are close to each other), so the algorithm can filter the error from the ray path and improve the data quality. Kuo-Fong Ma 馬國鳳 2002 學位論文 ; thesis 108 zh-TW |
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碩士 === 國立中央大學 === 地球物理研究所 === 90 === The distribution of aftershocks often indicates the geological structure in that area and implies the type of fault rupture. Except of 1999 Chi-chi earthquake, most of earthquake in Taiwan did not cause surface rupture. It yields the ambiguous on determination of rupture plane and its associated active fault. More accurate relocation of aftershocks might be able to help us on identification of its rupture plane and understanding its corresponding geological structure.
In this paper, we reexam the aftershocks of several large earthquakes in the past ten years e.g. 1993 Da-Pu, 1994 Nan-Ao, 1998 Ruey-Li, 1999 Chi-Chi and 1999 Chia-I earthquakes. Using CWBSN data, we apply the “Double Difference Earthquake Location Algorithm” ( Waldhauser, F., Ellsworth, W. L., 2000 ) to relocate aftershocks and to understand their association with geological structure. Because of the concept of multiplet (a group of earthquake which are close to each other), so the algorithm can filter the error from the ray path and improve the data quality.
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author2 |
Kuo-Fong Ma |
author_facet |
Kuo-Fong Ma Chung-Han Chan 詹忠翰 |
author |
Chung-Han Chan 詹忠翰 |
spellingShingle |
Chung-Han Chan 詹忠翰 Using Double Difference Earthquake Location Algorithm to Relocate the Aftershocks of Great Earthquakes in the Past Ten Years |
author_sort |
Chung-Han Chan |
title |
Using Double Difference Earthquake Location Algorithm to Relocate the Aftershocks of Great Earthquakes in the Past Ten Years |
title_short |
Using Double Difference Earthquake Location Algorithm to Relocate the Aftershocks of Great Earthquakes in the Past Ten Years |
title_full |
Using Double Difference Earthquake Location Algorithm to Relocate the Aftershocks of Great Earthquakes in the Past Ten Years |
title_fullStr |
Using Double Difference Earthquake Location Algorithm to Relocate the Aftershocks of Great Earthquakes in the Past Ten Years |
title_full_unstemmed |
Using Double Difference Earthquake Location Algorithm to Relocate the Aftershocks of Great Earthquakes in the Past Ten Years |
title_sort |
using double difference earthquake location algorithm to relocate the aftershocks of great earthquakes in the past ten years |
publishDate |
2002 |
url |
http://ndltd.ncl.edu.tw/handle/77306100553490572807 |
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