国际地震动态Issue(8)：3-8,6.DOI:10.3969/j.issn.0235-4975.2015.08.002
温度测量结果表明日本东北地区近海断层存在低速同震摩擦
P M Fulton 1S Toczko 2王林(译) 3黄宏生(校) 4E E Brodsky 1Y Kano 5J Mori 5F Chester 6T Ishikawa 7R N Harris 8W Lin 7N Eguchi2
作者信息
- 1. Department of Earth and Planetary Sciences，University of California，Santa Cruz，CA，USA
- 2. Center for Deep Earth Exploration，Japan Agency for Marine-Earth Science and Technology，Yokohama，Japan
- 4. 福建省地震局
- 5. Disaster Prevention Research Institute，Kyoto University，Kyoto，Japan
- 6. Center for Tectonophysics，Department of Geology and Geophysics，Texas A&M University，College Station，TX，USA
- 7. Kochi Institute for Core Sample Research，Japan Agency for Marine-Earth Science and Technology，Kochi，Japan
- 8. Oregon State University，Corvallis，OR，USA
- 折叠
引用本文复制引用
P M Fulton,S Toczko,王林(译),黄宏生(校),E E Brodsky,Y Kano,J Mori,F Chester,T Ishikawa,R N Harris,W Lin,N Eguchi..温度测量结果表明日本东北地区近海断层存在低速同震摩擦[J].国际地震动态,2015,(8):3-8,6.
