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Archaeoseismology and Palaeoseismology in the Alpine ... - Tierra

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DISCUSSION<br />

The fall<strong>in</strong>g time of <strong>the</strong> Buddha statue is important to<br />

analyse earthquake hazards for a specific earthquake.<br />

From <strong>the</strong> artistic style <strong>and</strong> wea<strong>the</strong>r<strong>in</strong>g condition of <strong>the</strong><br />

Buddha statue, <strong>the</strong> fall<strong>in</strong>g time could be estimated<br />

roughly. However, we can not determ<strong>in</strong>e <strong>the</strong> exact fall<strong>in</strong>g<br />

time from <strong>the</strong>se methods. Recently, optically stimulated<br />

lum<strong>in</strong>escence (OSL) dat<strong>in</strong>g method has emerged as a<br />

powerful dat<strong>in</strong>g method for <strong>the</strong>se cases, because quartz<br />

<strong>and</strong> feldspar to be dated are abundant <strong>in</strong> this situation<br />

(Choi et al, 2009). The fallen Buddha statue is ly<strong>in</strong>g on <strong>the</strong><br />

wea<strong>the</strong>r<strong>in</strong>g soil of Cretaceous granite. If we can collect<br />

suitable materials for OSL dat<strong>in</strong>g, <strong>the</strong> fall<strong>in</strong>g time could be<br />

determ<strong>in</strong>ed. It could <strong>in</strong>dicate <strong>the</strong> <strong>in</strong>terrelationship<br />

between <strong>the</strong> fall<strong>in</strong>g Buddha statue <strong>and</strong> 779 AD<br />

earthquake. Therefore, fur<strong>the</strong>r studies are required to<br />

solve this problem.<br />

Many Quaternary faults were reported around <strong>the</strong> study<br />

area. The aerial photograph of <strong>the</strong> area shows obviously<br />

NE‐SW, NNE‐SSW, <strong>and</strong> E‐W trend<strong>in</strong>g l<strong>in</strong>eaments. Data<br />

obta<strong>in</strong>ed from trenches excavated across active faults are<br />

of great value <strong>in</strong> studies of earthquake hazards.<br />

Therefore, if we f<strong>in</strong>d Quaternary faults around <strong>the</strong><br />

Buddha statue, <strong>the</strong>y could provide useful <strong>in</strong>formation for<br />

paleo‐earthquakes <strong>in</strong> this area.<br />

CONCLUSIONS<br />

The study area is located around <strong>the</strong> junction between<br />

<strong>the</strong> Yangsan <strong>and</strong> Ulsan faults. Recently many Quaternary<br />

faults have been reported along <strong>the</strong> Yangsan <strong>and</strong> Ulsan<br />

faults encourag<strong>in</strong>g researches on <strong>the</strong> fault activities <strong>and</strong><br />

associated paleoseismicities. Accord<strong>in</strong>g to historical<br />

records, <strong>the</strong> study area was significantly affected by<br />

earthquakes. The earthquakes produced heavy casualties<br />

<strong>and</strong> damages <strong>in</strong> historical properties. Although we need<br />

additional absolute dat<strong>in</strong>g data, <strong>the</strong> fall<strong>in</strong>g time of <strong>the</strong><br />

Buddha looks co<strong>in</strong>cident with <strong>the</strong> 779 AD earthquake,<br />

which killed over one hundred people. Fracture sets<br />

measured from <strong>the</strong> fallen Buddha statue well match with<br />

those fractures measured from nearby <strong>in</strong> situ granite if<br />

<strong>the</strong> fallen statue were rotated 20° clockwise back <strong>in</strong>to<br />

<strong>the</strong>ir orig<strong>in</strong>al positions. It <strong>in</strong>dicates that <strong>the</strong> Buddha statue<br />

might be fallen down with 20° counterclockwise rotation.<br />

Although we can not sure about <strong>the</strong> consistency of <strong>the</strong><br />

tim<strong>in</strong>g between <strong>the</strong> fall<strong>in</strong>g time of <strong>the</strong> Buddha statue <strong>and</strong><br />

<strong>the</strong> 779 AD earthquake, it must be fallen down by any<br />

episodic force such as l<strong>and</strong>slides or earthquakes. This idea<br />

1 st INQUA‐IGCP‐567 International Workshop on Earthquake Archaeology <strong>and</strong> <strong>Palaeoseismology</strong><br />

66<br />

is supported by <strong>the</strong> wea<strong>the</strong>r<strong>in</strong>g condition of <strong>the</strong> Buddha<br />

statue, <strong>the</strong> distribution of surround<strong>in</strong>g blocks, <strong>and</strong> <strong>the</strong><br />

geomorphological pattern of <strong>the</strong> slope around <strong>the</strong> statue.<br />

O<strong>the</strong>r earthquake damages were also reported <strong>in</strong><br />

historical records. Based on recent geological <strong>and</strong><br />

archaeoseismological studies, <strong>the</strong> Gyeongju area might<br />

not be free from future earthquake hazards.<br />

Acknowledgements: This work was funded by <strong>the</strong> Korea<br />

Meteorological Adm<strong>in</strong>istration Research <strong>and</strong> Development<br />

Program under Grant CATER 2008‐5502.<br />

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