A Blind Normal Fault beneath the Taipei Basin in Northern Taiwan

被引：11

作者：

Chen, Kou-Cheng ^{[1
]}

Huang, Bor-Shouh ^{[1
]}

Huang, Win-Gee ^{[1
]}

Wang, Jeen-Hwa ^{[1
]}

Kim, Kwang-Hee ^{[2
]}

Lee, Shiann-Jong ^{[1
]}

Lai, Ya-Chuan ^{[3
]}

Tsao, Shuhjong ^{[4
]}

Chen, Chi-Hsuan ^{[4
]}

机构：

[1] Acad Sinica, Inst Earth Sci, Taipei 115, Taiwan

[2] Korea Ocean Res & Dev Inst, Ansan, South Korea

[3] Natl Cent Univ, Inst Geophys, Jhongli, Taiwan

[4] Minist Econ Affairs, Cent Geol Survey, Taipei, Taiwan

来源：

TERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCES | 2010年 / 21卷 / 03期

关键词：

Taipei basin; Seismicity; Blind normal fault; 1999; CHI-CHI; EARTHQUAKE; SEQUENCE; VOLCANO; PLATE; BELT; AREA;

D O I：

10.3319/TAO.2010.01.25.01(TH)

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The Taipei basin, historically low in seismicity, is located in northern Taiwan. A dense broadband seismic array was deployed in the basin in June 2004 to monitor seismic activity. During the period of operation, three felt earthquakes occurred near the eastern part of the Taipei basin, about 3 km to the south of Taipei 101 then the tallest building in the world Relocated earthquakes show a southeast-clipping distribution of hypocenters beneath the Taipei basin. The seismicity pattern and focal mechanisms of the three felt events suggest the existence of a blind normal fault whose surface projection is along the river channel in the middle of the basin

引用

页码：495 / 502

页数：8

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