| 沂沭断裂带地壳垂直形变的演化及其构造含义 |
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| 引用本文： | 王若柏,扬国华.沂沭断裂带地壳垂直形变的演化及其构造含义[J].中国地震,1995,11(2):174-180. |
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| 作者姓名： | 王若柏 扬国华 |
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| 作者单位： | 国家地震局第一地形变监测中心 |
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| 摘 要： | 本文使用多期精密水准资料，经采用统一的计算方法和起算标准处理后，分别对沂沭断裂带上的山东和苏鲁皖地区地壳垂直形变场及其演化特征进行了深入的分析，并结合地震地质背景、区域应力场、地震活动特征等研究了地震危险性问题。
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| 关 键 词： | 地震活动性 郯－庐断裂带 苏鲁皖地区 地壳变形 |
Evolotion of the Crustal Vertical Deformation along the Yishu Fault Zone and Its Tectonic Implication |
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| Wang Robai,Yang Guohua,Han Yueping,Geng Shichang.Evolotion of the Crustal Vertical Deformation along the Yishu Fault Zone and Its Tectonic Implication[J].Earthquake Research in China,1995,11(2):174-180. |
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| Authors: | Wang Robai Yang Guohua Han Yueping Geng Shichang |
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| Abstract: | The precise leveling data for serveral periods along the Yishu fault zone in JiangsuShandong-Anhui area have been adjusted by using same caculated method for uniform leveling network and from the same initial point. The crustal vertical deormation field and it's feature of development have been analysed in this area. Combined with geological and seismological background, seimisity and stress field, the seismic risk of this area has been studied. |
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| Keywords: | Seismicity The Tancheng-Lujiang fault zone Jiangsu-Shangdong-Anhui area |
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