|
The 1994 Taiwan Strait earthquake occurred on September 16, 1994 at 14:20 local time (06:20 UTC) in the southern Taiwan Strait. The magnitude of this earthquake was given as Mw 6.8 by USGS〔http://earthquake.usgs.gov/earthquakes/eqarchives/significant/sig_1994.php〕 and Ms 7.3 by Fujian Seismological Bureau.〔http://www.csi.ac.cn/manage/html/4028861611c5c2ba0111c5c558b00001/zhenli/wjf/html/zhenli137.htm〕 The epicenter was located about 150 to 180 km from the coast of the border of Guangdong and Fujian, and about 150 km southwest of Taiwan.〔http://tao.cgu.org.tw/pdf/v71p013.pdf〕 == Geology == The earthquake occurred in the transition zone from the continental margin to the continent-ocean transitional crust. In this region, the depth of the Moho interface decreases from about 28 km in the west to about 20 km in the east. The transition between continental and oceanic crusts is reflected in the variation of the depth of the Moho interface.〔 There are several NW trending faults in the Taiwan Strait, including the Ningde-Sandiaojiao fault zone (宁德-三貂角断裂带), the Taizhong-Jinjiang fault zone (台中-晋江断裂带), and the Bashi fault zone (巴士断裂带).〔"台湾海峡地区横向构造及其对东南沿海地震的作用" by 沈金瑞, 许世远, and 傅文杰〕 In addition, there are several faults in the NE direction, including the Binhai Fault Zone (or the Littoral Fault Zone) (滨海断裂带).〔"南澎列岛及邻近海域地质地貌与灾害地质分析" by 詹文欢, 张乔民, 孙宗勋, 唐诚, and 丘学林〕 Some sources suggested that the earthquake was related to the activity of the Bashi fault system. However, there are still disputes over whether the fault plane should have been in the NW or the NE direction.〔 A paper of Fujian Seismological Bureau showed that the earthquake was caused by left-lateral strike slip of a normal fault.〔 The earthquake had a maximum slip of 14 m in the hypocentral region. The source duration was about 4 s, which is short for an event with magnitude about Mw 6.7. From the slip amplitude and the source duration, it was suggested that this earthquake began as a breaking of a strong asperity with low dynamic friction, had high stress drop, and was stopped by large friction around the asperity.〔"The 16 September 1994 Taiwan Strait earthquake: a simple rupture event starting as a break of asperity" by T.-Y. Zheng, Y.-S. Ai, and Q.-Z. Chen〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「1994 Taiwan Strait earthquake」の詳細全文を読む スポンサード リンク
|