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Fluid distribution along the Nankai-...
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Akuhara, Takeshi.
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Fluid distribution along the Nankai-Trough megathrust ault off the Kii Peninsula = inferred from receiver function analysis /
紀錄類型:
書目-電子資源 : Monograph/item
正題名/作者:
Fluid distribution along the Nankai-Trough megathrust ault off the Kii Peninsula/ by Takeshi Akuhara.
其他題名:
inferred from receiver function analysis /
作者:
Akuhara, Takeshi.
出版者:
Singapore :Springer Singapore : : 2018.,
面頁冊數:
xvi, 94 p. :ill. (some col.), digital ;24 cm.
Contained By:
Springer eBooks
標題:
Thrust faults (Geology) - Japan. -
電子資源:
http://dx.doi.org/10.1007/978-981-10-8174-3
ISBN:
9789811081743
Fluid distribution along the Nankai-Trough megathrust ault off the Kii Peninsula = inferred from receiver function analysis /
Akuhara, Takeshi.
Fluid distribution along the Nankai-Trough megathrust ault off the Kii Peninsula
inferred from receiver function analysis /[electronic resource] :by Takeshi Akuhara. - Singapore :Springer Singapore :2018. - xvi, 94 p. :ill. (some col.), digital ;24 cm. - Springer theses,2190-5053. - Springer theses..
This thesis explores fluid distribution along the Nankai-Trough megathrust fault around the Kii Peninsula of Japan, where devastating earthquakes are expected to occur in the near future. Exploring fluid distribution along subduction zones is an important issue because the fluid is considered to control the occurrence of earthquakes. One of the effective strategies to estimate fluid content is retrieving receiver functions (RFs) from seismograms, but in the case of ocean-bottom seismometers (OBSs), noisy P-wave reverberations within the seawater column make such an analysis difficult. The author therefore developed a novel technique to suppress the water reverberations, which allows obtaining the fluid distribution data along a wide depth range on the plate interface. This thesis first presents the new technique, called the water layer filter method, and demonstrates its efficiency by using both synthetic and observation data. Then, using the method, a receiver function image of the Philippine Sea Plate is constructed to reveal dehydration processes of the subducting oceanic crust around the Kii Peninsula. Finally, the author performs high-frequency receiver function inversion analysis. The results indicate the presence of a thin fluid-rich sediment layer along the megathrust fault off the Kii Peninsula that acts as a pathway of fluid. Nowadays, the number of offshore observations is increasing worldwide. In this respect, the attempt to better analyze OBS data employing the new method will become more important in future studies.
ISBN: 9789811081743
Standard No.: 10.1007/978-981-10-8174-3doiSubjects--Topical Terms:
3301760
Thrust faults (Geology)
--Japan.
LC Class. No.: QE511.46 / .A384 2018
Dewey Class. No.: 551.872
Fluid distribution along the Nankai-Trough megathrust ault off the Kii Peninsula = inferred from receiver function analysis /
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This thesis explores fluid distribution along the Nankai-Trough megathrust fault around the Kii Peninsula of Japan, where devastating earthquakes are expected to occur in the near future. Exploring fluid distribution along subduction zones is an important issue because the fluid is considered to control the occurrence of earthquakes. One of the effective strategies to estimate fluid content is retrieving receiver functions (RFs) from seismograms, but in the case of ocean-bottom seismometers (OBSs), noisy P-wave reverberations within the seawater column make such an analysis difficult. The author therefore developed a novel technique to suppress the water reverberations, which allows obtaining the fluid distribution data along a wide depth range on the plate interface. This thesis first presents the new technique, called the water layer filter method, and demonstrates its efficiency by using both synthetic and observation data. Then, using the method, a receiver function image of the Philippine Sea Plate is constructed to reveal dehydration processes of the subducting oceanic crust around the Kii Peninsula. Finally, the author performs high-frequency receiver function inversion analysis. The results indicate the presence of a thin fluid-rich sediment layer along the megathrust fault off the Kii Peninsula that acts as a pathway of fluid. Nowadays, the number of offshore observations is increasing worldwide. In this respect, the attempt to better analyze OBS data employing the new method will become more important in future studies.
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