Eigenvector of gravity gradient tensor for estimating fault dips considering fault type
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DOI[10.1186/s40645-017-0130-0]to the data of the same series
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- Material Type
- 記事
- Author/Editor
- Shigekazu Kusumoto
- Publication, Distribution, etc.
- Publication Date
- 2017-06-02
- Publication Date (W3CDTF)
- 2017-06-02
- Periodical title
- Progress in earth and planetary science
- No. or year of volume/issue
- 4(15)
- Volume
- 4(15)
- ISSN (Periodical Title)
- 2197-4284
- ISSN-L (Periodical Title)
- 2197-4284
- Text Language Code
- eng
- DOI
- 10.1186/s40645-017-0130-0
- Persistent ID (NDL)
- info:ndljp/pid/10369592
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2017-06-29T04:49:44+09:00
- Date Captured (W3CDTF)
- 2017-06-26
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/10369577
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- DOI
- 10.1186/s40645-017-0130-0
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Gravity gradient tensor analysis and its application to the Eastern Boundary Fault Zone of the Shonai Plain, Northeastern JapanInconsistent Structure and Motion of the Eastern Median Tectonic Line, Southwest Japan, during the QuaternaryPreface to the special issue “High-definition topographic and geophysical data in geosciences”Gravity gradient tensor analysis to an active fault : a case study at the Togi-gawa Nangan fault, Noto Peninsula, central Japan
- References
- TSVD analysis of Euler deconvolution to improve estimating magnetic source parameters: An example from the Åsele area, SwedenAutomatic generation of 3D geophysical models using curvatures derived from airborne gravity gradient dataAnalytic signals of gravity gradient tensor and their application to estimate source locationThe second derivative method of gravity interpretationEigenvector analysis of gravity gradient tensor to locate geologic bodiesThe limitation of curvature gravity gradient tensor for edge detection and a method for overcoming itApproximating edges of source bodies from magnetic or gravity anomaliesCurvature of a geometric surface and curvature of gravity and magnetic anomaliesApplication of edge detection to potential field data using eigenvalue analysis of structure tensorEnhancement of the total horizontal gradient of magnetic anomalies using the tilt angleApplied GeophysicsEdge enhancement of potential field data using an enhanced tilt angleCurvature attributes and their application to 3D interpreted horizonsRecipe for Predicting Strong Ground Motion from Crustal Earthquake ScenariosThe removal of unwanted edge contours from gravity datasetsEffects of the hanging wall and footwall on ground motions recorded during the Northridge earthquakeSurface shape and curvature scalesTHE PLACE OF THE VERTICAL GRADIENT IN GRAVITATIONAL INTERPRETATIONSWindow constrained inversion of gravity gradient tensor data using dike and contact modelsGeometric shapes derived from airborne gravity gradiometry data: New tools for the explorationistRapid gravity computations for two-dimensional bodies with application to the Mendocino submarine fracture zonePotential field tilt—a new concept for location of potential field sourcesConforming Falcon<sup>‡</sup> gravity and the global gravity anomalyEnhancing potential field data using filters based on the local phase3D full tensor gradiometry and Falcon Systems data analysis for iron ore exploration: Baú Mine, Quadrilátero Ferrífero, Minas Gerais, BrazilEuler deconvolution of gravity tensor gradient dataEdge detection of potential field data using improved local phase filter3D inversion of airborne gravity gradiometry data in mineral exploration: A case study in the Quadrilátero Ferrífero, BrazilThe complete gravity gradient tensor derived from the vertical component of gravity: a Fourier transform technique2次元重力解析より推定された京都盆地における未固結堆積層の密度明治以後の内陸浅発地震の被害から見た強震動の特徴１次元重力探査による断層周辺の密度構造推定 樫原断層および麓村断層について重力勾配テンソルの固有ベクトルを用いた断層あるいは構造境界の傾斜角の推定The First and Second Vertical Derivatives of Gravity.Dip distribution of Oita-Kumamoto Tectonic Line located in central Kyushu, Japan, estimated by eigenvectors of gravity gradient tensor
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 10369592