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鄂尔多斯块体东南缘现今的变形特征与构造模式探讨 被引量:4
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作者 刘瑞春 张锦 +3 位作者 郭文峰 陈慧 郑亚迪 成诚 《地震地质》 EI CSCD 北大核心 2021年第3期540-558,共19页
鄂尔多斯块体东南缘是中国大陆西部碰撞挤压到东部伸展拉张动力学转换的关键地区,其新构造运动以强烈的差异升降运动为主,在该区开展空间高分辨率的地壳垂直运动观测尤为重要。文中基于Radarsat-2宽模式影像,采用干涉图堆叠(Stacking)... 鄂尔多斯块体东南缘是中国大陆西部碰撞挤压到东部伸展拉张动力学转换的关键地区,其新构造运动以强烈的差异升降运动为主,在该区开展空间高分辨率的地壳垂直运动观测尤为重要。文中基于Radarsat-2宽模式影像,采用干涉图堆叠(Stacking)技术获得了研究区的空间高分辨LOS向平均形变速率场,并与研究区域内长期观测的GPS连续站数据开展对比分析。在此基础上,利用倾滑断层位错模型、粒子群算法(PSO)反演了主要断裂的滑动速率和闭锁深度,结果表明:1)利用干涉图堆叠(Stacking)技术得到的研究区年尺度地壳形变场具有较高的精度,且区域地壳短期形变与长期形变具有一致性。2)鄂尔多斯东南缘的构造和非构造形变相互叠加,构造形变主要发生在活动断裂附近,与断层滑动速率和闭锁深度有关。非构造形变主要发生在盆地内部的第四纪地层,与含水层厚度和地下水开采量有关,最大量级>5cm/a。3)中条山北麓断裂和峨嵋台地北缘断裂的滑动速率为0.37mm/a和0.74mm/a,闭锁深度为3.4km和4.3km,可能表明断裂在最后一次强震发生后还未完全闭锁,现今以浅部活动为主。峨嵋台地南缘断裂的滑动速率为0.47mm/a,闭锁深度为0.95km,表明断层现今可能以蠕滑活动为主。4)鄂尔多斯地块的逆时针旋转和秦岭山地的向E挤出逃逸,形成了鄂尔多斯东南缘以走滑-伸展转换为特征的似三联点构造区。 展开更多
关键词 鄂尔多斯东南缘 INSAR GPS 滑动速率 闭锁深度 构造变形模型
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Seismotectonic Zonation of the Longmengshan and Chengdu Region
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作者 Kong Jun Shi Bingxin +1 位作者 Zhou Rongjun Wang Shiyuan 《Earthquake Research in China》 CSCD 2016年第4期566-577,共12页
The principle of three-level delineation is adopted in determination of a potential seismic source for the new National Seismic Ground Motion Parameters Zoning Map of China,to embody the inhomogeneity of the spatial d... The principle of three-level delineation is adopted in determination of a potential seismic source for the new National Seismic Ground Motion Parameters Zoning Map of China,to embody the inhomogeneity of the spatial distribution of background seismic activity and induct a uniform seismotectonic model for each seismotectonic region. Based on achievements of determining potential seismic sources in southwestern China,this paper introduces the basic characteristics, historical earthquakes magnitude and frequency distribution,identification of deformation mechanism of main active tectonic structures for the Longmenshan and Chengdu seismotectonic region in the Longmenshan seismic region,establishes the seismogenic model for each seismotectonic region,and identifies the upper limit of background earthquakes. A simple method is also put forward for calculating the spatial distribution function of a background seismic source. 展开更多
关键词 Potential seismic source Seismotectonic region Spatial distribution function
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g factors of nuclear low-lying states:A covariant description 被引量:5
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作者 YAO JiangMing PENG Jing +1 位作者 MENG Jie RING Peter 《Science China(Physics,Mechanics & Astronomy)》 SCIE EI CAS 2011年第2期198-203,共6页
The g factors and spectroscopic quadrupole moments of low-lying excited states 2+1,…,81+ in 24Mg are studied in a covariant density functional theory.The wave functions are constructed by configuration mixing of axia... The g factors and spectroscopic quadrupole moments of low-lying excited states 2+1,…,81+ in 24Mg are studied in a covariant density functional theory.The wave functions are constructed by configuration mixing of axially deformed mean-field states projected on good angular momentum.The mean-field states are obtained from the constraint relativistic point-coupling model plus BCS calculations using the PC-F1 parametrization for the particle-hole channel and a density-independent delta-force for the particle-particle channel.The available experimental g factor and spectroscopic quadrupole moment of 21+ state are reproduced quite well.The angular momentum dependence of g factors and spectroscopic quadrupole moments,as well as the effects of pairing correlations are investigated. 展开更多
关键词 covariant density functional theory magnetic moment g factor spectroscopic quadrupole moment
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