山西井水位短临异常分析     

吴定定  王爱英 《山西地震》1993,(4)

通过对山西地下水动态井冈,在山西地震带几次中强地震前,表现出异常变化情况的分析,获得一批有价值的短临异常资料,这些异常资料对利用地下水预报地震具有参考意义;另一方面说明在有发震背景地区实现短临跟踪是完全有可能的.  相似文献   

滇西北伸展构造区的构造特点及其动力学研究   总被引：1，自引：0，他引：1  

韩竹君  徐杰  虢顺民  杨主恩  向宏发  吴大宁 《中国地震》1993,(2)

本文研究了滇西北伸展构造区活动构造、地震活动和新构造环境的特点。该区构造与地震的活动强度为南、北部强,中间弱;第四纪最大沉降中心、湖积台地及第四纪褶皱分布呈对角对称。滇西北地区的伸展构造是在近南北向挤压力和南西—北东向剪切力的共同作用下形成的,其合力方向为北北东,与用水压致裂法和物理模拟获得的结果相符。该区在形成机制上属于一种特殊的拉分构造。  相似文献   

甘肃西成铅锌矿田中泥盆统碳酸盐沉积相的初步研究     

武安斌  宋春晖 《甘肃地质》1993,2(1):25-34,T003

本文根据岩石类型、沉积构造、生物组合和指相矿物将西成矿田中泥盆统碳酸盐沉积划分为两个相带,7个相和11个亚相,即碳酸盐台地相带和碳酸盐台地边缘相带;台地潮坪相、局限台地相、半开阔台地相、开阔台地相、台缘前斜坡相、生物滩层礁相和礁相。可以看出,区内铅锌矿床的形成和分布明显受着碳酸盐沉积相带的控制。  相似文献   

胶南隆起北缘中段左行正滑韧性剪切带研究   总被引：2，自引：0，他引：2  

张长厚  朱忠 《现代地质》1993,7(4):435-443

在详细的野外地质填图的基础上,通过各种尺度的构造研究和系统的应变测量,确定了胶南隆起北缘中段的大型左行正滑韧性剪切带的存在及其延展范围,并提出了确定韧性剪切带边界的构造几何学准则。研究了该韧性剪切带的几何学和运动学特征及变形机制,估算了其剪切位移量(大于7557m)及形成时的差异应力(σ_1-σ_3=94.6～114.4MPa)。该韧性剪切带可以作为胶南隆起的北部边界,但不是重要的板块碰撞边界。  相似文献   

新疆石炭—二叠纪植物地理区的形成与演变   总被引：4，自引：1，他引：4  

吴绍祖 《新疆地质》1993,(1)

通过对晚古生代气候演化趋向的分析,探讨了新疆石炭纪和二叠纪植物地理分区的形成与演变。认为植物地理分区在早石炭世晚期末—晚石炭世早期即已形成,随着温带气候区的逐渐扩大,安加拉区植物在新疆自北向南逐渐推移,至晚二叠世中—晚期到达北塔里木。早二叠世—晚二叠世早期南准噶尔、伊犁等地受欧洲东移的干旱气流的影响,有欧美型松柏类混生。塔里木为特提斯生物大区的一部分,植物主要为欧美-华夏区类型。  相似文献   

2-(2-苯并噻唑偶氮)-5-二羧甲氨基苯甲酸的合成及其应用——多元显色体系光度法测定金属材料中的镍   总被引：2，自引：0，他引：2  

樊学忠  吴斌才  刘恒椽  吴诚 《岩矿测试》1993,(1):31-34

报道了新显色剂2-(2-苯并噻唑偶氮)-5-二羧甲氨基苯甲酸(BTACB)的合成,研究了在十二烷基硫酸钠(NaLS)存在下Ni~(2+)与BTACB形成蓝紫色配合物的条件,其λ_(max)~(MR)=600nm,ε=2.79×10~4L·mol~(-1)·cm~(-1),Ni在0～0.6μg/ml范围内服从比尔定律,反应具有一定的选择性。方法已用于直接测定铝合金、纯镁及含一定量Co的钢铁中痕量Ni和经萃取分离后测定纯钴中痕量Ni。  相似文献   

X射线荧光光谱法测定叶腊石中的铝铁钾钠   总被引：1，自引：0，他引：1  

郭寿兴  吴玉庆 《岩矿测试》1993,12(4):290-292

采用同一矿区已知成分含量的叶腊石配制标样系列，克服了粉末法测定叶腊石中Ａｌ２Ｏ３，Ｆｅ２Ｏ３，Ｋ２Ｏ，Ｎａ２Ｏ的矿物和粒度效应。分析结果准确度满足出口材料的检测要求。  相似文献   

743离子交换快速分离—等离子体光谱法同时测定十五个稀土元素   总被引：1，自引：0，他引：1  

吴锡凤  蒋铁珊 《铀矿地质》1993,(5)

本文研制了适用于地质样品中15个稀土元素分析的快速方法。样品经碱熔沉淀分离和743阳离子交换树脂分离富集将稀土元素制备成溶液用等离子体光谱法(ICP-AES)进行测量。方法检出限为0.002-0.3μg/g,当稀土元素含量为0.5-80,μg/g时,方法相对标准偏差为15％-2％。本方法经过多年的样品分析考验以及不断的改进和完善,证明方法简便快速,分析数据稳定可靠,能很好地满足地质样品中15个稀土分量测定的要求。  相似文献   

The phase velocities of Rayleigh waves and the lateral variation of lithospheric structure in Tibetan Plateau   总被引：1，自引：0，他引：1  

Guo-Ying Chen  Rong-Sheng Zeng  Francis T. Wu  Xiao-Lan Su 《地震学报(英文版)》1993,6(2):289-297

According to a Sino-U. S. joint project, eleven broadband digital PASSCAL seismometers had been deployed inside the Tibetan Plateau, of which 7 stations were on the profile from Lhasa to Golmud and other 4 stations situated at Maxin, Yushu, Xigatze and Linzhi. Dispersions and phase velocities of the Rayleigh surface waves (10s–120s) were obtained on five paths distributed in the different blocks of Tibetan Plateau. Inversions of the S-wave velocity structures in Songpan-Ganzi block, Qiang-Tang block, Lhasa block and the faulted rift zone were obtained from the dispersion data. The results show that significant lateral variation of the S-wave velocity structures among the different blocks exists. The path from Wenquan to Xigatze (abbreviated as Wndo-Xiga) passes through the rift-zone of Yadong-Anduo. The phase velocities of Rayleigh waves from 10s to 100s on this path are significantly higher than that on other paths. The calculated mean crustal velocity on this path is 3.8 km/s, much greater than that on other paths, where mean crustal velocities of 3.4–3.5 km/s are usually observed. Low velocity zones with different thicknesses and velocities are observed in the middle-lower crust for different paths. Songpan-Ganzi block, located in the northern part of Tibetan Plateau is characterized by a thinner crust of 65 km thick and a prominent low velocity zone in the upper mantle. The low velocity zone with a velocity of 4.2 km/s is located at a depth form 115 km to 175 km. While in other blocks, no low velocity zone in the upper mantle is observed. The value of Sn in Songpan-Ganzi is calculated to be 4.5 km/s, while those in Qiang-Tang and Lhasa blocks are about 4.6 km/s. The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,14, Supp., 566–573, 1992.  相似文献   

Preliminary study of crust-upper mantle structure of the Tibetan Plateau by using broadband teleseismic body waveforms   总被引：2，自引：0，他引：2  

Lu-Pei Zhu  Rong-Sheng Zeng  Francis T. Wu  Thomas J. Owens  George E. Randall 《地震学报(英文版)》1993,6(2):305-316

As part of a joint Sino-U.S. research project to study the deep structure of the Tibetan Plateau, 11 broadband digital seismic recorders were deployed on the Plateau for one year of passive seismic recording. In this report we use teleseimic P waveforms to study the seismic velocity structure of crust and upper mantle under three stations by receiver function inversion. The receiver function is obtained by first rotating two horizontal components of seismic records into radial and tangential components and then deconvolving the vertical component from them. The receiver function depends only on the structure near the station because the source and path effects have been removed by the deconvolution. To suppress noise, receiver functions calculated from events clustered in a small range of back-azimuths and epicentral distances are stacked. Using a matrix formalism describing the propagation of elastic waves in laterally homogeneous stratified medium, a synthetic receiver function and differential receiver functions for the parameters in each layer can be calculated to establish a linearized inversion for one-dimensional velocity structure. Preliminary results of three stations, Wen-quan, Golmud and Xigatze (Coded as WNDO, TUNL and XIGA), located in central, northern and southern Plateau are given in this paper. The receiver functions of all three stations show clear P-S converted phases. The time delays of these converted phases relative to direct P arrivals are: WNDO 7.9s (for NE direction) and 8.3s (for SE direction), TUNL 8.2s, XIGA 9.0s. Such long time delays indicate the great thickness of crust under the Plateau. The differences between receiver function of these three station shows the tectonic difference between southern and north-central Plateau. The waveforms of the receiver functions for WNDO and TUNL are very simple, while the receiver function of XIGA has an additional midcrustal converted phase. The S wave velocity structures at these three stations are estimated from inversions of the receiver function. The crustal shear wave velocities at WNDO and TUNL are vertically homogeneous, with value between 3.5–3.6 km/s down to Moho. This value in the lower crust is lower than the normal value for the lower crust of continents, which is consistent with the observed strong Sn attenuation in this region. The velocity structure at XIGA shows a velocity discontinuity at depth of 20 km and high velocity value of 4.0 km/s in the midcrust between 20–30 km depth. Similar results are obtained from a DSS profile in southern Tibet. The velocity under XIGA decreases below a depth of 30 km, reaching the lowest value of 3.2 km/s between 50–55 km. depth. This may imply that the Indian crust underthrusts the low part of Tibetan crust in the southern Plateau, forming a “double crust”. The crustal thickness at each of these sites is: WNDO, 68 km; TUNL, 70 km; XI-GA, 80 km. The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,14, Supp., 581–592, 1992.  相似文献