Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.p333
I. Fabricius, C. Olsen, A. Krogsbøll, M. Prasad
P333 Static and Dynamic Young’s Modulus of Marly Chalk from the North Sea Introduction 1 Deformation properties of a rock are governing factors for production of oil from a reservoir. These properties can be either determined from geotechnical consolidation testing (also called static tests) or from acoustic data (dynamic tests). The main differences between the two tests lie in the frequency of the measurements and the strain amplitude used in the tests. When a sound wave propagates through a porous medium the deformation of the grains is elastic. In a geotechnical test the strain is larger and a non-elastic deformation
{"title":"Static and Dynamic Young's Modulus of Marly Chalk from the North Sea","authors":"I. Fabricius, C. Olsen, A. Krogsbøll, M. Prasad","doi":"10.3997/2214-4609-pdb.3.p333","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.p333","url":null,"abstract":"P333 Static and Dynamic Young’s Modulus of Marly Chalk from the North Sea Introduction 1 Deformation properties of a rock are governing factors for production of oil from a reservoir. These properties can be either determined from geotechnical consolidation testing (also called static tests) or from acoustic data (dynamic tests). The main differences between the two tests lie in the frequency of the measurements and the strain amplitude used in the tests. When a sound wave propagates through a porous medium the deformation of the grains is elastic. In a geotechnical test the strain is larger and a non-elastic deformation","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"92 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132725140","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.g046
T. Probert, R. Dok, J. Gaiser
G046 TIME-LAPSE SHEAR WAVE SPLITTING ANALYSIS AT EKOFISK FIELD NORTH SEA Summary 1 The ability to detect and measure shear-wave (S-wave) birefringence or shear splitting using modeconverted (PS) waves is well understood and is demonstrated in several recent studies. In September 2002 a 4-component (4C) test line was acquired at the Ekofisk Field to investigate the application of PS-waves. Analysis of the PS-wave data indicated the presence of significant S-wave birefringence in the near surface. This phenomenon has been correlated to the local sea floor subsidence that is induced by the compaction within the underlying chalk reservoir at a depth
{"title":"Time-Lapse Shear Wave Splitting Analysis at Ekofisk Field, North Sea","authors":"T. Probert, R. Dok, J. Gaiser","doi":"10.3997/2214-4609-pdb.3.g046","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.g046","url":null,"abstract":"G046 TIME-LAPSE SHEAR WAVE SPLITTING ANALYSIS AT EKOFISK FIELD NORTH SEA Summary 1 The ability to detect and measure shear-wave (S-wave) birefringence or shear splitting using modeconverted (PS) waves is well understood and is demonstrated in several recent studies. In September 2002 a 4-component (4C) test line was acquired at the Ekofisk Field to investigate the application of PS-waves. Analysis of the PS-wave data indicated the presence of significant S-wave birefringence in the near surface. This phenomenon has been correlated to the local sea floor subsidence that is induced by the compaction within the underlying chalk reservoir at a depth","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"5 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"116866588","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.p231
J. Haldorsen, R. Coates, S. Petersen, A. Hawthorn, M. V. Schaack
P231 FULL-WAVEFORM WHILE-DRILLING SEISMICS A CASE STUDY FROM THE GRANE FIELD THE NORTH SEA Introduction 1 R.T. COATES 1 J. B.U. HALDORSEN 1 S.A. PETERSEN 2 A. HAWTHORN 3 and M. VAN SCHAACK 4 In most exploration and in some development wells the seismic map is the primary guide for well placement. The estimated depth to a seismic target is based on certain assumptions with regard to the anisotropy of the formation. These assumptions are necessary because the surface-seismic data give poorly constrained estimates of the vertical velocities. However borehole-seismic travel times give a direct calibration of the vertical velocity
{"title":"Full-Waveform While-Drilling Seismics, a Case Study from the Grane Field, the North Sea","authors":"J. Haldorsen, R. Coates, S. Petersen, A. Hawthorn, M. V. Schaack","doi":"10.3997/2214-4609-pdb.3.p231","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.p231","url":null,"abstract":"P231 FULL-WAVEFORM WHILE-DRILLING SEISMICS A CASE STUDY FROM THE GRANE FIELD THE NORTH SEA Introduction 1 R.T. COATES 1 J. B.U. HALDORSEN 1 S.A. PETERSEN 2 A. HAWTHORN 3 and M. VAN SCHAACK 4 In most exploration and in some development wells the seismic map is the primary guide for well placement. The estimated depth to a seismic target is based on certain assumptions with regard to the anisotropy of the formation. These assumptions are necessary because the surface-seismic data give poorly constrained estimates of the vertical velocities. However borehole-seismic travel times give a direct calibration of the vertical velocity","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"60 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121830916","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.p101
P. Stavrev, Daniela Gerovska, E. Aboud
P101 MAGNITUDE TRANSFORMS IN THE PROCESS OF MAGNETIC DATA ANALYSIS SUMMARY 1 The magnitude transforms include magnitude magnetic anomalies (MMA) their gradients and Laplacian. They are calculable from the total magnetic anomalies (TMA) or other component anomalies. MMAs have space distribution different from that of the component anomalies. Their values are non-negative and the respective patterns are similar to the positive gravity anomalies. Thus a MMA from a compact source has only a maximum centered above the source. The sensitivity to the source magnetization direction is suppressed. The modulus of full gradients and Laplacian of MMAs are also non-negative space
{"title":"Magnitude Transforms in the Process of Magnetic Data Analysis","authors":"P. Stavrev, Daniela Gerovska, E. Aboud","doi":"10.3997/2214-4609-pdb.3.p101","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.p101","url":null,"abstract":"P101 MAGNITUDE TRANSFORMS IN THE PROCESS OF MAGNETIC DATA ANALYSIS SUMMARY 1 The magnitude transforms include magnitude magnetic anomalies (MMA) their gradients and Laplacian. They are calculable from the total magnetic anomalies (TMA) or other component anomalies. MMAs have space distribution different from that of the component anomalies. Their values are non-negative and the respective patterns are similar to the positive gravity anomalies. Thus a MMA from a compact source has only a maximum centered above the source. The sensitivity to the source magnetization direction is suppressed. The modulus of full gradients and Laplacian of MMAs are also non-negative space","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"134 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123220454","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.d032
D. Pham, S. Xu
D032 Seismic Data Regularization with Anti-leakage Fourier Transform SHENG XU and DON PHAM Abstract 1 Veritas DCG Inc. Town Park Drive Houston Tx 77072 USA In the theory of Fourier reconstruction from discrete seismic data it aims to estimate the spatial frequency content on an irregularly sampled grid. After obtaining the Fourier coefficients the data can be reconstructed on any desired grid. For this type of transform difficulties arise from the non-orthogonality of the global basis functions on an irregular grid. As a consequence energy from one Fourier coefficient leaks onto other coefficients. This well-known phenomenon is called “spectral leakage”.
{"title":"Seismic Data Regularization with Anti-Leakage Fourier Transform","authors":"D. Pham, S. Xu","doi":"10.3997/2214-4609-pdb.3.d032","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.d032","url":null,"abstract":"D032 Seismic Data Regularization with Anti-leakage Fourier Transform SHENG XU and DON PHAM Abstract 1 Veritas DCG Inc. Town Park Drive Houston Tx 77072 USA In the theory of Fourier reconstruction from discrete seismic data it aims to estimate the spatial frequency content on an irregularly sampled grid. After obtaining the Fourier coefficients the data can be reconstructed on any desired grid. For this type of transform difficulties arise from the non-orthogonality of the global basis functions on an irregular grid. As a consequence energy from one Fourier coefficient leaks onto other coefficients. This well-known phenomenon is called “spectral leakage”.","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"115 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123987422","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.c043
M. Willis, F. Pearce, D. Burns, J. Byun, B. Minsley
C043 RESERVOIR FRACTURE ORIENTATION AND DENSITY FROM REFLECTED AND SCATTERED SEISMIC ENERGY M. E. WILLIS F. PEARCE D. R. BURNS J. BYUN B. MINSLEY Earth Resources Laboratory Massachusetts Institute of Technology 42 Carleton St. Cambridge MA USA 02142 Abstract Synthetic seismic shot records were generated using a 3D elastic finite difference modeling code simulating the seismic scattering from sets of discrete large-scale vertical fractures in a subsurface reservoir. We used these shot records to develop data analysis methods applicable to reflection seismic field data in order to determine the orientation and density of the fractures. For shot records acquired parallel
{"title":"Reservoir Fracture Orientation and Density from Reflected and Scattered Seismic Energy","authors":"M. Willis, F. Pearce, D. Burns, J. Byun, B. Minsley","doi":"10.3997/2214-4609-pdb.3.c043","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.c043","url":null,"abstract":"C043 RESERVOIR FRACTURE ORIENTATION AND DENSITY FROM REFLECTED AND SCATTERED SEISMIC ENERGY M. E. WILLIS F. PEARCE D. R. BURNS J. BYUN B. MINSLEY Earth Resources Laboratory Massachusetts Institute of Technology 42 Carleton St. Cambridge MA USA 02142 Abstract Synthetic seismic shot records were generated using a 3D elastic finite difference modeling code simulating the seismic scattering from sets of discrete large-scale vertical fractures in a subsurface reservoir. We used these shot records to develop data analysis methods applicable to reflection seismic field data in order to determine the orientation and density of the fractures. For shot records acquired parallel","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"175 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122591264","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.p308
T. Tabti, T. Tvedt, J. Langhammer
P308 AZIMUTH DEPENDENT PROCESSING – APPLICATION TO THE CLAIR OBS DATA Summary 1 The Clair data set is a 3D-4C Ocean Bottom Seismic data acquired by PGS for BP in the West of Shetlands area in the North Atlantic. With the view of characterizing azimuthal variations in elastic properties the data were acquired using a patch geometry that allowed for a good offset and azimuth distribution. Processing of the acquired multi-component dataset was also awarded to PGS Data Processing centre in Oslo. The main challenge was to apply true 3D processing that takes into account the azimuth dimension. Conventional seismic
{"title":"Azimuth Dependent Processing – Application to the Clair OBS Data","authors":"T. Tabti, T. Tvedt, J. Langhammer","doi":"10.3997/2214-4609-pdb.3.p308","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.p308","url":null,"abstract":"P308 AZIMUTH DEPENDENT PROCESSING – APPLICATION TO THE CLAIR OBS DATA Summary 1 The Clair data set is a 3D-4C Ocean Bottom Seismic data acquired by PGS for BP in the West of Shetlands area in the North Atlantic. With the view of characterizing azimuthal variations in elastic properties the data were acquired using a patch geometry that allowed for a good offset and azimuth distribution. Processing of the acquired multi-component dataset was also awarded to PGS Data Processing centre in Oslo. The main challenge was to apply true 3D processing that takes into account the azimuth dimension. Conventional seismic","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"87 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126400606","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.p043
R. Ondrak, R. Lippmann, V. Neumann, R. Gaup, R. Primio, B. Horsfield
P043 MODELING BURIAL HISTORY AND FLUID- ROCK-INTERACTIONS OF DEEP OVERPRESSURED RESERVOIRS IN THE CENTRAL GRABEN NORTH SEA Abstract 1 We study temperature and pressure-controlled inorganic and organic diagenetic processes in a study area of the Central Graben North Sea containing clastic Mesozoic reservoirs situated at depths of 4.5-5 km and temperatures of 170-192°C. The reservoirs are highly overpressured due to rapid burial during the last 2 Ma. We present first results of a basin modeling study focusing on the burial and temperature history of these HPHT-reservoirs. Furthermore we concentrate on organic-inorganic interactions enhancing mineral solubility and increasing porosity. This is
{"title":"Modeling Burial History and Fluid-Rock-Interactions of Deep Overpressured Reservoirs in the Central Graben, North Sea","authors":"R. Ondrak, R. Lippmann, V. Neumann, R. Gaup, R. Primio, B. Horsfield","doi":"10.3997/2214-4609-pdb.3.p043","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.p043","url":null,"abstract":"P043 MODELING BURIAL HISTORY AND FLUID- ROCK-INTERACTIONS OF DEEP OVERPRESSURED RESERVOIRS IN THE CENTRAL GRABEN NORTH SEA Abstract 1 We study temperature and pressure-controlled inorganic and organic diagenetic processes in a study area of the Central Graben North Sea containing clastic Mesozoic reservoirs situated at depths of 4.5-5 km and temperatures of 170-192°C. The reservoirs are highly overpressured due to rapid burial during the last 2 Ma. We present first results of a basin modeling study focusing on the burial and temperature history of these HPHT-reservoirs. Furthermore we concentrate on organic-inorganic interactions enhancing mineral solubility and increasing porosity. This is","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"39 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126794043","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.e031
A. Kitchka, Y. Kostyuchenko
E031 RADAR IMAGING DATA APPLICATIONS TO HYDROCARBON PROSPECTING IN THE SOUTH KERCH OFFSHORE BLACK SEA BASIN Abstract 1 A.A. KITCHKA and Yu.V. KOSTYUCHENKO Centre for Aerospace Research of the Earth IGS NASU 55-B Gonchar St. Kiev 01601 Ukraine Nowadays application of remotely sensed data acquired by synthetic aperture radar sensors installed onboard of ERS JERS ENVISAT and other satellites and Space Shuttles proves to be a useful tool for offshore oil and gas exploration using processing and thematic interpretation of space-born imagery coupled with analysis of available geological geophysical hydrophysical and meteo information. Radar imaging is a basic remote sensing
{"title":"Radar Imaging Data Applications to Hydrocarbon Prospecting in the South Kerch Offshore, Black Sea Basin","authors":"A. Kitchka, Y. Kostyuchenko","doi":"10.3997/2214-4609-pdb.3.e031","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.e031","url":null,"abstract":"E031 RADAR IMAGING DATA APPLICATIONS TO HYDROCARBON PROSPECTING IN THE SOUTH KERCH OFFSHORE BLACK SEA BASIN Abstract 1 A.A. KITCHKA and Yu.V. KOSTYUCHENKO Centre for Aerospace Research of the Earth IGS NASU 55-B Gonchar St. Kiev 01601 Ukraine Nowadays application of remotely sensed data acquired by synthetic aperture radar sensors installed onboard of ERS JERS ENVISAT and other satellites and Space Shuttles proves to be a useful tool for offshore oil and gas exploration using processing and thematic interpretation of space-born imagery coupled with analysis of available geological geophysical hydrophysical and meteo information. Radar imaging is a basic remote sensing","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"113965936","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2004-06-07DOI: 10.3997/2214-4609-pdb.3.p035
J. N. Yakymchuk, S. Levashov, N. Yakymchuk, I. Korchagin, J. Pyschaniy
P035 ELECTRIC-RESONANCE SOUNDING METHOD AND ITS APPLICATION FOR THE ECOLOGICAL GEOLOGICAL-GEOPHYSICAL AND ENGINEERING-GEOLOGICAL INVESTIGATIONS 1 S.P. LEVASHOV 1 N.A. YAKYMCHUK 1 I.N. KORCHAGIN 2 JU.M. PYSCHANIY 2 JU.N. YAKYMCHUK 3 1 Institute of applied problems of Ecology Geophysics and Geochemistry Laboratory lane 1 Kyiv 01133 Ukraine e-mail: yakymchuk@karbon.com.ua slevashov@mail.ru 2 Institute of Geophysics of Ukraine National Academy of Science e-mail: korchagin@karbon.com.ua 3 MMC Kyiv Ukraine Abstract. The method of electric-resonance sounding is described. It is based on studying the processes of natural polarization of medium and spectral features of natural electric field under investigation objects. The method allows to define
P035电共振测深方法及其在生态地质地球物理和工程地质调查中的应用[j] .列瓦绍夫1 n.a. yakymchuk 1 in . korchagin 2 jun . m。心理学6月2日。2乌克兰国家科学院地球物理研究所e-mail: korchagin@karbon.com.ua 2乌克兰国家科学院地球物理研究所e-mail: korchagin@karbon.com.ua 3 MMC乌克兰基辅摘要介绍了电共振测深方法。它是在研究被测对象的介质自然极化过程和自然电场光谱特征的基础上建立起来的。方法允许定义
{"title":"Electric-Resonance Sounding Method and Its Application for the Ecological, Geological-Geophysical and Engineering-Geological Investigations","authors":"J. N. Yakymchuk, S. Levashov, N. Yakymchuk, I. Korchagin, J. Pyschaniy","doi":"10.3997/2214-4609-pdb.3.p035","DOIUrl":"https://doi.org/10.3997/2214-4609-pdb.3.p035","url":null,"abstract":"P035 ELECTRIC-RESONANCE SOUNDING METHOD AND ITS APPLICATION FOR THE ECOLOGICAL GEOLOGICAL-GEOPHYSICAL AND ENGINEERING-GEOLOGICAL INVESTIGATIONS 1 S.P. LEVASHOV 1 N.A. YAKYMCHUK 1 I.N. KORCHAGIN 2 JU.M. PYSCHANIY 2 JU.N. YAKYMCHUK 3 1 Institute of applied problems of Ecology Geophysics and Geochemistry Laboratory lane 1 Kyiv 01133 Ukraine e-mail: yakymchuk@karbon.com.ua slevashov@mail.ru 2 Institute of Geophysics of Ukraine National Academy of Science e-mail: korchagin@karbon.com.ua 3 MMC Kyiv Ukraine Abstract. The method of electric-resonance sounding is described. It is based on studying the processes of natural polarization of medium and spectral features of natural electric field under investigation objects. The method allows to define","PeriodicalId":110744,"journal":{"name":"66th EAGE Conference & Exhibition","volume":"31 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2004-06-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127815766","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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