Controlled source apparent resistivity tensors and their relationship to the magnetotelluric impedance tensor   总被引：2，自引：0，他引：2  

T. Grant Caldwell  Hugh M. Bibby  Colin Brown 《Geophysical Journal International》2002,151(3):755-770

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The S-velocity structure of the East Asian mantle from inversion of shear and surface waveforms   总被引：15，自引：0，他引：15  

Wolfgang Friederich 《Geophysical Journal International》2003,153(1):88-102

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A high-resolution magnetotelluric survey of the Iapetus Suture Zone in southwest Scotland   总被引：1，自引：0，他引：1  

Sebastian Tauber  Roger Banks  Oliver Ritter  Ute Weckmann 《Geophysical Journal International》2003,153(3):548-568

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Separation of intrinsic absorption and scattering attenuation from Lg coda decay in central France using acoustic radiative transfer theory   总被引：3，自引：0，他引：3  

Céline Lacombe  Michel Campillo  Anne Paul  Ludovic Margerin 《Geophysical Journal International》2003,154(2):417-425

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Time-domain, spectral finite-element approach to transient 2-D geomagnetic induction in a spherical heterogeneous Earth     

Zden&#;k Martinec  Mark E. Everett  Jakub Velímský 《Geophysical Journal International》2003,155(1):33-43

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太湖水体吸收系数与散射系数的特征研究   总被引：19，自引：2，他引：19       下载免费PDF全文

俞宏  蔡启铭  吴敬禄 《水科学进展》2003,14(1):46-49

湖泊水体光学特性是进行湖泊水体光学及水体光学遥感研究的基础。计算了太湖冬、夏季水体的吸收系数和散射系数,并在分析水体吸收特性的基础上对水体的光学类型进行了分类。结果表明:冬季太湖水体的光学类型属PY型(悬浮粒和黄质共同作用型),即水体的吸收特性受悬浮质和黄质的共同作用,而夏季则属CPY型(浮游藻类、悬浮粒和黄质共同作用型),即水体的吸收特性受悬浮质、黄质和浮游藻类三者的共同作用;不论冬季还是夏季,非色素悬浮粒是影响太湖水体散射特性的主要因子。  相似文献   

青海平安电磁辐射在中强震前短期前兆异常特征及预报效能研究   总被引：2，自引：0，他引：2  

马玉虎  马文静 《地震地磁观测与研究》2003,24(6):64-71

分析和整理了青海平安电磁辐射台自1993年7月以来的资料，发现震前平安单台电磁辐射在中强地震临震前有最大脉冲信号，并通过对无震异常，地震异常的分析判断，对其预报效能进行了R值评价。  相似文献   

Tensor time domain electromagnetic resistivity measurements at Ngatamariki geothermal field, New Zealand     

George F. Risk  T. Grant Caldwell  Hugh M. Bibby 《Journal of Volcanology and Geothermal Research》2003,127(1-2):33-54

Experimental measurements in the Ngatamariki geothermal field, North Island, New Zealand were made to test the applicability of the time domain electromagnetic method for detailed investigation of the resistivity structure within a geothermal field. Low-frequency square wave signals were transmitted through three grounded bipole current sources sited about 8 km from the measurement lines. Despite high levels of electrical noise, transient electric field vectors could be determined reliably for times between 0.02 and 3.3 s after each step in the source current. Instantaneous apparent resistivity tensors were then calculated. Apparent resistivity pseudosections along the two measurement lines show smooth variations of resistivity from site to site. Over most of the field the images consistently show a three-layer resistivity structure with a conductive middle layer (3–10 Ωm) representing the conductive upper part of the thermal reservoir. A deep-seated region of low resistivity in the northwest of the field may indicate a conductive structure at about 1 km associated with a deeper diorite intrusion. Measurements sited closer than about 100 m to drillholes appear to have been disturbed by metallic casing in the holes. A change in resistivity structure in the east of the field may indicate a major geological or hydrothermal boundary.  相似文献   

Imaging buried Quaternary valleys using the transient electromagnetic method   总被引：3，自引：0，他引：3  

Flemming Jrgensen  Peter B. E. Sandersen  Esben Auken 《Journal of Applied Geophysics》2003,53(4):199

Buried Quaternary valleys in Denmark are complex structures filled with various deposits consisting primarily of glacio-lacustrine clay, till and meltwater sand, and gravel. The valleys are important geophysical targets, because they often contain significant volumes of groundwater used for public water supply. About 700 km of buried valley structures have been imaged in the western part of Denmark by the transient electromagnetic (TEM) method. The ability to map the valleys depends primarily on valley geometry, infill architecture and the resistivity of the fill sediments as well as the substratum. One-dimensional (1-D) inversion models of the TEM soundings have been used to construct contour maps of 20 m average resistivities and depth to a good conductor, which provide images for geological interpretation. Images of buried valley morphology, fill properties, infill architecture, such as cut-and-fill structures, valley distribution and valley generations, are characterized for case studies from Hornsyld, Holstebro and the Vonsild/Agtrup areas of Denmark.  相似文献   

时间谱电阻率法中的剩余电磁效应研究   总被引：2，自引：0，他引：2  

昌彦君  罗延钟  彭复员 《吉林大学学报(地球科学版)》2003,33(1):92-95

根据频谱激电（SIP）法或复电阻率（CR）法中研究剩余电磁（REM）效应的思想，通过分析时间谱电阻率（TSR）法中场的基本特征，在TSR法中建立了与SIP（或CR）法中参数Φmax/Φ0max相类似的参数－Emax/E0，用来描述了TSR法中的REM效应。通过对一维可极化大地模型的REM效应的理论计算，验证了用Emax/E0表示的REM异常可用来形象地反映地电断面电阻率的高低。  相似文献