The 1904 Ms 7.3 Earthquake in Central Alaska

被引:4
|
作者
Tape, Carl [1 ]
Lomax, Anthony [2 ]
Silwal, Vipul [1 ]
Agnew, James D. [3 ]
Brettschneider, Brian [4 ]
机构
[1] Univ Alaska Fairbanks, Geophys Inst, 903 Koyukuk Dr, Fairbanks, AK 99775 USA
[2] ALomax Sci, 320 Chemin Indes, F-06370 Mouans Sartoux, France
[3] Dept Water Resources, Operat & Maintenance Div, Civil Maintenance Branch, Earthquake Engn Sect, 1416 9th St,Room 150A-2, Sacramento, CA 95814 USA
[4] Univ Alaska Fairbanks, Int Arctic Res Ctr, POB 757340,930 Koyukuk Dr, Fairbanks, AK 99775 USA
基金
美国国家科学基金会;
关键词
LARGE SHALLOW EARTHQUAKES; DENALI FAULT EARTHQUAKE; ENERGY-RELEASE; MAGNITUDES; TECTONICS; LOCATION; CONSTRAINTS; CATALOG; RUPTURE; TENSORS;
D O I
10.1785/0120160178
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
On 27 August 1904, seismic stations from around the globe recorded an M > 7 earthquake originating from central Alaska. Very little was known about this earthquake. One felt report from Rampart, Alaska, had been attributed to the notes of Harry Fielding Reid, yet its original source was unknown. Here, we present five felt reports for the 1904 earthquake that show evidence of felt shaking across most of central Alaska. Using the 1904 arrival-time data, we estimate an epicentral location near Lake Minchumina at the northeastern extent of the Iditarod-Nixon fault. Our preferred fault for the 1904 earthquake is the right-lateral Iditarod-Nixon fault, which, though relatively seismically quiet, generated an M 6.2 earthquake in 1935. Paleoseismic investigations are needed to search for evidence of fault activity, including the 1904 earthquake rupture, in the tectonically complex region of the 1904 earthquake.
引用
收藏
页码:1147 / 1174
页数:28
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