博士 / 國立中央大學 / 地球科學學系 / 103 / Taiwan is a young mountain belt, known as one of the most active area in the world. Since the beginning of the
20th century more than twenty Mw7 earthquakes have struck the island. However, the occurrence of larger
events (Mw8) is still a matter of debate. In this framework it is of key importance to obtain longer record
in order to evaluate the occurrence of large past earthquakes. The sub-aqueous paleoseismology, based on the
record of the sedimentary gravity deposits, appears as a serious alternative to approach this thematic and is a
rapidly advancing field that has the potential to illuminate the long-term history of seismicity.
The first part of this work was to investigate the present sedimentary systems off east Taiwan, essential to
understand the morphosedimentary features, sedimentary facies and processes governing the evolution of the
submarine slope, and the controlling factors of the recent sedimentation. Our results showed that the offshore
slope east Taiwan is affected by a variety of sedimentary systems and processes, and that turbidity currents
appear as the main erosional processes covering nearly 60% of the sedimentary record. Turbidity currents are
generated by distinct controlling factors such as tectonic and climatic activity that enabled us to define two
end-members relative to turbidity currents initiation: Turbidity currents preconditioned by tectonic activity and
triggered by earthquakes shaking and likely deposited into intra-slope basin and turbidity currents driven by
climatic activity such as extreme floods or typhoons, generated in basin directly connected with onland rivers.
The second part consisted to apply a paleoseismic approach, based on turbidites record, at two time-scales. First,
we tested and validated the method by correlating turbidites deposits with instrumental earthquakes. Then, once
calibrated we extended the time-series back in time. We dated the three most recent turbidites layers circa AD
2001 3, AD 1950 5 and AD 1928 8. Using empirical relationship that link peakground acceleration,
distance and magnitude to calibrate the seismic sources, we correlate these three turbidites with instrumental
earthquakes: the Chengkong Earthquake 12/10/2003 (Mw 6.8), the 11/24/1951 Taitung Earthquake (Mw 7.1)
and the 9/4/1935 Lutao Earthquake (Mw 7.0) respectively. Dating and age modeling provided a chronology of
extreme events since the last 3000 years. Applying criteria to discriminating the different triggering mechanisms
for turbidity current generation, we propose that earthquakes are the main triggering mechanisms. We also
estimate that synchronous turbidite events correlated over the whole margin were triggered by a Mw8 earthquake
between 50 BC and 600 AD. This work represents a good starting-point for future investigations in order to better
assess Holocene time series of extreme events.
| Identifer | oai:union.ndltd.org:TW/103NCU05134009 |
| Date | January 2015 |
| Creators | Remi Lehu, 雷米 |
| Contributors | Shu-kun Hsu, 許樹坤 |
| Source Sets | National Digital Library of Theses and Dissertations in Taiwan |
| Language | en_US |
| Detected Language | English |
| Type | 學位論文 ; thesis |
| Format | 317 |
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