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英文摘要     
《物探化探计算技术》2009,31(3):I0001-I0006
Forward modeling is the base of inversion techniques, and the speed of forward modeling and how to store the coefficient matrix from inversion are the key techniques of the gravity and magnetic 3D inversion. An new Gravity and Magnetic 3D forward modeling method with rolling topography is presented in this paper. The principle is that two different scale matrixes with different measurements from forwarding modeling are produced based on the layers partition for inversion vertically, and the forward modeling values of the gravity and magnetic value with rolling topography are direcdy computed based on the local linear interpolating by taking the topography as the horizontal in the local model space.  相似文献   

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英文摘要     
《物探化探计算技术》2009,31(5):I0001-I0006
STUDY ON GRAVITY METHOD FOR DETECTING SUBSURFACE MASS;THE DYNAMIC RESPONSE OF SATURATED SANDSTONE BY CYCLIC LOADING;SOLUTION STRATEGIES FOR 2D AND 3D MAGNETOTELLURIC FORWARD MODELING BASED ON THE FINITE ELEMENT METHOD;A STABLE ALGORITHM FOR CALCULATING THE VERTICAL DERIVATIVES OF POTENTIAL FIELD;THE INSTANT DISPLAY FOUNCTION OF THE AIRBORNE ELECTROMAGNETIC PROFILE CURVE BASED ON SECONDARY DEVELOPMENT OF MAPGIS;  相似文献   

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英文摘要     
《物探化探计算技术》2009,31(6):I0001-I0006
APPLICATION OF WAVELET ANALYSIS FOR GEOPHYSICAL DATA AND COPPER MINERAL DEPOSITS FORECAST IN MANDAMAH AREA
SHEN Wei, FANG Cong-hui, CHANG Xing-guo (State Key Laboratory of Geo-Processes and Mineral Resources, Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China). COMPUTING TECHNIQUES FOR GEOPHYSICAL AND GEOCHEMICAL EXPLORA- TION. 2009. 31 (6): 0525  相似文献   

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英文摘要     
《物探化探计算技术》2009,31(4):I0001-I0006
2D INVERSION OF VES DATA UNDER ROLLING TOPOGRAPHY AND ITS APPLICATION
Considering to meet usually the rolling topogra- phy in the groundwater resource investigation, mineral exploration, engineering detection, etc. and based on the published literature in existence, this paper pres- ent our settlement of 2D inversion problem of VES da- m with the rolling topography by applying the total smooth constraint in the inversion. The approach can effectively process the FEM grid division and the in version software is made. Finally, it is proved that the inverted results is reliable through inverting the simulated and measured VES data, and the inversion software can be applied to the practical work.  相似文献   

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  • Li Siguang (1976) Research Method of Geomechanics[M].Science Press,Beijing (in Chinese).
  • Liu Zhaochang,Li Fanyou,Zhong Kanghui,and Li Wei (1996) Tectonic Evolution and Metallogenesis on the Western Margin of the Yangtze Platform[M].pp.17-67.University of Electronics Science Press,Chengdu (in Chinese with English abstract).
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  • Marc Polliand and Robert Moritz (1999) Basement-hosted quartz-barite sulfide veins in the French Alps:a record of Alpine tectonic fluid expulsion in external crystalline massifs-structural,fluid inclusion and isotopes (S and Sr) evidences[J].Economic Geology.94,37-56.
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  • Shen Shumin,Zheng Fangfang,and Liu Wenying (1994) Three Dimensional Migration Potential Fields of the Tectonic Stress Driving and the Fluid Within Rocks[M].pp.37-42.Press of Earthquake,Beijing (in Chinese).
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    17.
    <正>Fourteen graptolite species of the Late Tremadoc and Early Floian are described from the Nanba section in the Yiyang area,Hunan Province.Among them,Paradelograptus onubensis, Kiaerograptus bulmani,K.kutchini and Paratemnograptus isolatus of the Late Tremadoc are first found in China.Based on the current graptolite materials,the correspondingly complete graptolite zones of Upper Tremadocian in China are recognized as follows(in ascending order):the Adelograptus tenellus Zone,the Aorograptus victoriae Zone,the Araneograptus murrayi Zone and the Hunnegraptus copiosus Zone.In the Nanba section,the Hunnegraptus copiosus Zone is overlain directly by the Tetragraptus approximatus Zone,there is no hiatus below the base of Floian.  相似文献   

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    <正>A new family of so-called‘higher' planthoppers,Weiwoboidae fam.nov.,from the Lower Eocene of Yunnan is described.A new monotypic genus,Weiwoboa gen.nov.,with Weiwoboa meridiana sp.nov.is also described and illustrated.The characters of tegmen venation of the new family,its evolution,and supposed relationships are briefly discussed.  相似文献   

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