Wide-angle observations of ALP 2002 shots on the TRANSALP profile: Linking the two DSS projects     

Florian Bleibinhaus  Ewald Brückl  ALP Working Group 《Tectonophysics》2006,414(1-4):71

Dynamite shots of the crustal-scale refraction seismic project ALP 2002 were recorded by an array of 40 seismological three-component stations on the TRANSALP profile. These observations provide a direct link between the two deep seismic projects. We report preliminary results obtained from these data. In a first approach, we verified the TRANSALP refraction seismic velocity model computing travel times for several shots and comparing them to the new observations. The results generally confirm this model. Significant first-break travel time differences in and near the Tauern Window are explained by anisotropy. Large-scale features of the model, particularly the Moho structure, seem to be continuous towards the east. Travel time residuals of wide-angle reflections indicate a slight eastward dip component of the Adriatic Moho.  相似文献   

Lithospheric structure of the Tornquist Zone resolved by nonlinear P and S teleseismic tomography along the TOR array   总被引：1，自引：1，他引：1  

Z. Hossein Shomali  Roland G. Roberts  Laust B. Pedersen  the TOR Working Group 《Tectonophysics》2006,416(1-4):133

The main aim of the TOR project is to study the lithospheric–asthenospheric boundary structure under the Sorgenfrei–Tornquist Zone, across northern Germany, Denmark and southern Sweden. Relative arrival-time residuals of teleseismic P and S phases from 51 earthquakes, recorded by 150 seismic stations along the TOR array, were used to delineate the transition zone in the studied area. The effects of crustal structures were investigated by correcting the teleseismic residuals for travel-time variations in the crust based on a 3D crustal model derived from other data. The inversion was carried out for S phases. The results were then compared with the corresponding P-wave models. As expected, the derived models show that the relatively old and cold Baltic Shield has higher velocity at depth than the younger lithosphere farther South. The models show two sharp and distinct increases in depth to velocities which are low compared to our reference model, as we move from South to North. The location and sharpness of these boundaries suggests that the features resolved are, at least partially, compositional in origin, presumably related to mantle depletion. A sharp and steep subcrustal boundary is found roughly coincident with the southern edge of Sweden. This is below where the edge of the Baltic Shield is usually placed, based on surface geological evidence (the Sorgenfrei–Tornquist Zone). Another less significant transition is recognised more or less beneath the Elbe-lineament. Relatively high d(V_p / V_s) ratios under the central part of the profile (Denmark) indicate relatively low S-velocity in an area where a gravity high supports the hypothesis of extensive mafic intrusions.  相似文献   

"磁暴基础数据库"项目成果介绍     

"磁暴基础数据库"项目组 《国际地震动态》2006,(9):9-12

本文详细介绍了“磁暴基础数据库”项目的立项背景、目标、所开展的主要工作、取得的成果、研究成果的社会效益和对该领域研究未来工作的展望。  相似文献   

被动源电磁阵列系统及其在某铜矿区的应用试验   总被引：3，自引：0，他引：3  

遥测电磁项目组 《物探与化探》1998,22(4):247-250271

本文介绍被动源电磁阵列系统的特点及该系统在某铜矿区的应用试验工作。与已知资料对比,试验结果给出了地下矿体的空间赋存形态,为矿区下一步工作提供了有意义的参考资料。  相似文献   

Search for Young Giant Planets with the Subaru 8-Meter Telescope: Instrument and Strategy     

Tamura  M.  Suto  H.  Itoh  Y.  CIAO Group 《Earth, Moon, and Planets》1998,81(1):109-110

Earth, Moon, and Planets -  相似文献   

MASS MOVEMENTS AND SEDIMENT TRANSPORT AS A NATURAL HAZARD     

Wolfgang KRON Senior Hydraulic Engineer  Geosciences Research Group  Munich Reinsurance Company  Munich  Germany 《国际泥沙研究》1997,(3)

I.INTRODUCTIONFormillionsofyearswindandwaterhaveshapedtheearth,mountainshavebeenliftedanderodedaway,waterhasevaporatedfromtheoceansandfallenbackonland,rivershaveformedandcarriedwaterandsedanmentfromthemoufltainstotheseas.Someoftherivers--suchastheColoradoRiverintheGrandCanyonregionofNorthAJnerica-foundstablecoursesastheycarvedthemselvesintotheground,others--suchastheYellowhiverinChina-havechangedtheircoursesfrequentlyallthewayintorecenthistory.Itwasonlyafewthousandyearsagothatmanstarte…  相似文献   

中国空间物理学学科发展战略研究报告     

中国空间物理学学科发展战略研究组 《地球科学进展》1996,11(2):140-150

从战略高度论述了空间物理学在认识人类生存环境、航天活动、经济发展中的重要地位和战略意义；以科学的态度分析了空间物理的发展史、现状和趋势；根据学科发展与我国国情相结合的原则提出了长期、中期和近期空间物理学的战略目标、战略重点和鼓励研究的课题以及实现战略目标的基本措施。  相似文献   

定点符号表示数量特征的方法探讨     

欧竹斌 《北京测绘》1996,(1):24-27

本文就定点符号法表示点状分布事物数量特征的三种连续比率符号和非比率分级符号进行了较深刻的分析与比较，指出了它们各自的特点和适用条件，并结合实例提出了如何改进和正确运用的方法。文中对定点符号如何表示两种相关内容的数量特征也结合实际作了具体分析。  相似文献   

Crustal structure across the TESZ along POLONAISE''97 seismic profile P2 in NW Poland     

T. Janik  J. Yliniemi  M. Grad  H. Thybo  T. Tiira  POLONAISE P Working Group 《Tectonophysics》2002,360(1-4):129-152

The POLONAISE'97 (POlish Lithospheric ONset—An International Seismic Experiment, 1997) seismic experiment in Poland targeted the deep structure of the Trans-European Suture Zone (TESZ) and the complex series of upper crustal features around the Polish Basin. One of the seismic profiles was the 300-km-long profile P2 in northwestern Poland across the TESZ. Results of 2D modelling show that the crustal thickness varies considerably along the profile: 29 km below the Palaeozoic Platform; 35–47 km at the crustal keel at the Teisseyre–Tornquist Zone (TTZ), slightly displaced to the northeast of the geologic inversion zone; and 42 km below the Precambrian Craton. In the Polish Basin and further to the south, the depth down to the consolidated basement is 6–14 km, as characterised by a velocity of 5.8–5.9 km/s. The low basement velocities, less than 6.0 km/s, extend to a depth of 16–22 km. In the middle crust, with a thickness of ca. 4–14 km, the velocity changes from 6.2 km/s in the southwestern to 6.8 km/s in the northeastern parts of the profile. The lower crust also differs between the southwestern and northeastern parts of the profile: from 8 km thickness, with a velocity of 6.8–7.0 km/s at a depth of 22 km, to ca.12 km thickness with a velocity of 7.0–7.2 km/s at a depth of 30 km. In the lowermost crust, a body with a velocity of 7.20–7.25 km/s was found above Moho at a depth of 33–45 km in the central part of the profile. Sub-Moho velocities are 8.2–8.3 km/s beneath the Palaeozoic Platform and TTZ, and about 8.1 km/s beneath the Precambrian Platform. Seismic reflectors in the upper mantle were interpreted at 45-km depth beneath the Palaeozoic Platform and 55-km depth beneath the TTZ.

The Polish Basin is an up to 14-km-thick asymmetric graben feature. The basement beneath the Palaeozoic Platform in the southwest is similar to other areas that were subject to Caledonian deformation (Avalonia) such that the Variscan basement has only been imaged at a shallow depth along the profile. At northeastern end of the profile, the velocity structure is comparable to the crustal structure found in other portions of the East European Craton (EEC). The crustal keel may be related to the geologic inversion processes or to magmatic underplating during the Carboniferous–Permian extension and volcanic activity.  相似文献   

High-resolution body wave tomography beneath the SVEKALAPKO array: I. A priori three-dimensional crustal model and associated traveltime effects on teleseismic wave fronts   总被引：3，自引：0，他引：3  

Senén Sandoval  Edi Kissling  Jörg Ansorge  the SVEKALAPKO Seismic Tomography Working Group 《Geophysical Journal International》2003,153(1):75-87

  相似文献