تقرير
中国陝西省渭河盆地の地震観測(日中共同研究序報) ; PRELIMINARY REPORT OF EARTHQUAKE OBSERVATION IN WEIHE BASIN, SHAANXI PROVINCE, CHINA
| العنوان: | 中国陝西省渭河盆地の地震観測(日中共同研究序報) ; PRELIMINARY REPORT OF EARTHQUAKE OBSERVATION IN WEIHE BASIN, SHAANXI PROVINCE, CHINA |
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| المؤلفون: | 尾池, 和夫, 松村, 一男, 大倉, 敬宏, 謝, 正章, LIU, Jing-Wen, LUO, Bai-Fa, 李, 徳利, 馬, 守信, 丁, 蘊玉, 田, 小平, 王, 洪体, LIU, Shang-Xiao |
| المساهمون: | OIKE, Kazuo, MATSUMURA, Kazuo, OKURA, Takahiro, XIE, Zheng-Zhang, LIU, Jing-Wen, LUO, Bai-Fa, LI, De-Li, MA, Shou-Xin, DING, Yun-Yu, TIAN, Xiao-Ping, WANG, Hong-Ti, LIU, Shang-Xiao |
| بيانات النشر: | 京都大学防災研究所 Disaster Prevention Research Institute, Kyoto University |
| سنة النشر: | 1989 |
| المجموعة: | Kyoto University Research Information Repository (KURENAI) / 京都大学学術情報リポジトリ |
| مصطلحات موضوعية: | 453.3, 454.55 |
| الوصف: | The joint study on the seismic activity in and around the Xian and active faults regionsin the Weihe basin, Shaanxi province, China, started on March, 1988 and has been in progress.Five stations with high-sensitive short period seismometers were established in theregion. During half an year from March, 1988, only two microearthquakes have beenrecorded. It shows that the seismic activity in the region is now very low. The larger eventof them occurred in the Qinling mountains region and its magnitude was 3.0. The other wasa small event with magnitude of 1.0 near the Zhou-Zhi station.Some records of teleseismic waves show clear later phases and those obtained at differentstatons show similar wave forms. Such records are going to be utilized to analyze the crustalstructure in the region. ; The joint study on the seismic activity in and around the Xian and active faults regionsin the Weihe basin, Shaanxi province, China, started on March, 1988 and has been in progress.Five stations with high-sensitive short period seismometers were established in theregion. During half an year from March, 1988, only two microearthquakes have beenrecorded. It shows that the seismic activity in the region is now very low. The larger eventof them occurred in the Qinling mountains region and its magnitude was 3.0. The other wasa small event with magnitude of 1.0 near the Zhou-Zhi station.Some records of teleseismic waves show clear later phases and those obtained at differentstatons show similar wave forms. Such records are going to be utilized to analyze the crustalstructure in the region. |
| نوع الوثيقة: | report |
| وصف الملف: | application/pdf |
| اللغة: | Japanese |
| تدمد: | 0386-412X |
| العلاقة: | http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.htmlTest; http://hdl.handle.net/2433/72166Test; AN00027784; 京都大学防災研究所年報. B; 32; B-1; 117; 124; Disaster Prevention Research Institute Annuals. B |
| الإتاحة: | http://hdl.handle.net/2433/72166Test |
| رقم الانضمام: | edsbas.8853EB9 |
| قاعدة البيانات: | BASE |
| تدمد: | 0386412X |
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