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The drilling project also uncovered that one of the causes of the earthquake was the movement of underground water. The team was the first to characterize this unusual type of earthquake, naming it an "isotropic event," that is, an earthquake-like event caused by natural hydraulic fracturing. Some
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and Yiben Tsai collaborated on the Taiwan
Chelungpu-fault Drilling Project (TCDP) with international collaborators in the US and Japan. The purpose of the project was to obtain physical samples of the fault, in particular where large displacements occurred during the
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503:
220:, drilled research boreholes to investigate the Chelungpu fault, leading to multiple discoveries about the causes of the earthquake. Most notably, the project led to an empirical breakthrough in
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Ma, Kuo-Fong; Lin, Yen-Yu; Lee, Shiann-Jong; Mori, Jim; Brodsky, Emily E. (27 July 2012). "Isotropic Events
Observed with a Borehole Array in the Chelungpu Fault Zone, Taiwan".
410:"Frictional and transport properties of the Chelungpu fault from shallow borehole data and their correlation with seismic behavior during the 1999 Chi-Chi earthquake"
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in Miaoli County, Taiwan. It is a major 90-km structure with a shallow eastward pointing tilt (30°) and primarily slips within and parallel to the bedding of the
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was located on the fault line. It was badly damaged by the quake. Today the high school is the site of the
National Museum of Natural Science's
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The
Chelungpu Fault has unique characteristics that make it an ideal research site, easy to drill and measure. It is a 12-meter long inland
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610:"Preface to the Special Issue on Taiwan Chelungpu-Fault Drilling Project (TCDP): Site Characteristics and On-Site Measurements"
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35:
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518:"National Museum of Natural Science -> Exhibition -> Permanent Exhibits -> Chelungpu Fault Preservation Park"
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Ma, KF (2006). "Slip zone and energetics of a large earthquake from the Taiwan
Chelungpu-fault Drilling Project".
259:"Stress orientations of Taiwan Chelungpu-Fault Drilling Project (TCDP) hole-A as observed from geophysical logs"
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385:"Heat Signature on the Chelungpu Fault Associated with the 1999 Chi-Chi, Taiwan Earthquake"
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Wu, H.-Y.; Ma, K.-F.; Zoback, M.; Boness, N.; Ito, H.; Hung, J.-H.; Hickman, S. (2007).
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The fault was reportedly discovered by Dr. Wen-shan Chen, Professor of
Geology at
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307:"Chelungpu Fault Preservation Park with BenQ Projector | BenQ Display Solution"
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suggest that this finding has important implications for fracking operations.
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was created by the earthquake. In the middle-western part of the island,
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Song, Sheng-Rong; Wang, Chien-Ying; Hung, Jih-Hao; Ma, Kuo-Fong (2007).
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counties. Some sections of land near the fault were changed in
128:). Near the northern end of the fault line, a 7-meter tall
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https://www.icdp-online.org/projects/world/asia/chelungpu/
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The epicenter of the earthquake was Chichi
Township. The
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with a 30 degrees tilt and a 105 km surface rupture.
188:was established and opened to the public in 2013.
155:, the damage was very bad. The village's Guangfu
408:Tanikawa, Wataru; Shimamoto, Toshihiko (2009).
72:The Chelungpu fault is a North–South-trending
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614:Terrestrial, Atmospheric and Oceanic Sciences
8:
414:Journal of Geophysical Research: Solid Earth
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769:
100:of Taiwan. The fault is located along the
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565:"【921防災篇】斷裂的防災網:世界級地震研究帶頭,建築規範、應用產業慢半拍"
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16:Active seismic fault located in Taiwan
709:"Erdbeben durch natürliches Fracking"
7:
737:
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180:, in November 2002. To preserve the
755:. You can help Knowledge (XXG) by
212:. The team, in part funded by the
14:
747:This article about a location in
492:《1:12,000 臺中縣太平市行政區域圖》內政部發行 2005年
238:Chelungpu Fault Preservation Park
186:Chelungpu Fault Preservation Park
171:Chelongpu Fault Preservation Park
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397:from the original on 2020-03-21.
48:
39:
1:
635:10.3319/TAO.2007.18.2.I(TCDP)
520:. Nmns.edu.tw. Archived from
136:were destroyed. This stopped
92:happened along the Chelungpu
263:Geophysical Research Letters
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178:National Taiwan University
214:National Science Council
679:10.1126/science.1222119
96:in western part of the
817:Taiwan geography stubs
812:Seismic faults of Asia
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27:
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161:921 Earthquake Museum
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713:Wissenschaft Aktuell
435:10.1029/2008JB005750
284:10.1029/2006GL028050
90:1999 Jiji earthquake
84:1999 Jiji earthquake
62:1999 Jiji earthquake
25:1999 Jiji earthquake
23:Running track after
807:Landforms of Taiwan
671:2012Sci...337..459M
626:2007TAOS...18.....S
464:註:車籠埔是光隆里、興隆里兩地的地名。
426:2009JGRB..114.1402T
355:10.1038/nature05253
347:2006Natur.444..473M
275:2007GeoRL..34.1303W
203:Taiwanese scholars
595:2021-01-16 at the
545:. 3 September 2008
479:2009-11-09 at the
460:2008-12-28 at the
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49:Chēlóngbù Duàncéng
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802:Geology of Taiwan
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665:(6093): 459–463.
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341:(7118): 473–476.
106:Central Mountains
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504:"臺中盆地與車籠埔斷層的關係"
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153:Taichung County
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68:Characteristics
32:Chelungpu Fault
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569:The Reporter
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522:the original
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502:台灣師範大學地理學系.
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311:www.benq.com
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198:thrust fault
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151:in southern
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54:active fault
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205:Kuo-Fong Ma
157:High School
140:for weeks.
56:located in
796:Categories
718:11 January
644:2090143485
620:(2): 000.
574:14 January
549:14 January
528:2014-05-13
455:太平市公所 里的特色
441:2020-12-12
316:2020-12-12
244:References
222:seismology
163:of Taiwan.
94:fault line
130:waterfall
118:elevation
102:foothills
695:33508855
687:22837526
640:ProQuest
593:Archived
477:Archived
458:Archived
392:Archived
363:17122854
232:See also
216:and the
192:Research
114:Taichung
78:Pliocene
52:) is an
667:Bibcode
659:Science
622:Bibcode
483:中央地質調查所
422:Bibcode
371:4413738
343:Bibcode
293:4694354
271:Bibcode
149:village
138:traffic
134:bridges
104:of the
36:Chinese
749:Taiwan
693:
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642:
543:"歷史沿革"
474:施政計畫報告
420:(B1).
369:
361:
335:Nature
291:
184:, the
145:Wufeng
122:meters
110:Nantou
98:island
58:Taiwan
46::
44:pinyin
38::
751:is a
691:S2CID
395:(PDF)
388:(PDF)
367:S2CID
289:S2CID
269:(1).
74:fault
40:車籠埔斷層
753:stub
720:2021
683:PMID
576:2021
551:2021
359:PMID
147:, a
126:feet
124:(23
112:and
30:The
675:doi
663:337
630:doi
430:doi
418:114
351:doi
339:444
279:doi
143:In
108:in
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