{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1363388844544432128.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1365-2478.2009.00830.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2478.2009.00830.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2478.2009.00830.x"}}],"dc:title":[{"@value":"Conforming Falcon<sup>‡</sup> gravity and the global gravity anomaly"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>ABSTRACT</jats:title><jats:p>Gravity derived only from airborne gravity gradient measurements with a normal error distribution will have an error that increases with wavelength. It is straightforward in principle to use sparsely sampled regional gravimeter data to provide the long wavelength information, thereby conforming the derived gravity to the regional gravity. Regional surface or airborne gravimeter data are not always available and can be difficult and expensive to collect in many of the areas where an airborne gravity gradiometer survey is flown. However the recent release by the Danish National Space Centre of the DNSC08 global gravity anomaly data has provided regional gravity data for the entire earth of adequate quality for this purpose. Studies over three areas, including comparisons with ground, marine and airborne gravimetry, demonstrate the validity of this approach. Future improvements in global gravity anomaly data are expected, particularly as the product from the recently launched Gravity field and steady‐state Ocean Circulation Explorer (GOCE) satellite becomes available and these will lead directly to an improvement in the very wide bandwidth gravity available after conforming gravity derived from gravity gradiometry with the global gravity.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844544432128","@type":"Researcher","foaf:name":[{"@value":"Mark Dransfield"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00168025"},{"@type":"EISSN","@value":"13652478"}],"prism:publicationName":[{"@value":"Geophysical Prospecting"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2010-03-26","prism:volume":"58","prism:number":"3","prism:startingPage":"469","prism:endingPage":"483"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2478.2009.00830.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2478.2009.00830.x"}],"createdAt":"2009-10-30","modifiedAt":"2023-10-30","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390282681471827456","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"空中重力偏差法探査の概要と現状"},{"@language":"en","@value":"Introduction of airborne gravity gradient survey to Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681474013824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"重力偏差テンソルのg<sub>zz</sub>成分のパワースペクトルと平均境界層深度の関係"},{"@language":"en","@value":"Relationship between the average depth of a stratum boundary and the power spectrum of the g<sub>zz</sub> component of a gravity gradient tensor"},{"@value":"重力偏差テンソルのgzz成分のパワースペクトルと平均境界層深度の関係"},{"@language":"ja-Kana","@value":"ジュウリョク ヘンサ テンソル ノ gzz セイブン ノ パワースペクトル ト ヘイキン キョウカイソウ シンド ノ カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681474101760","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"日本の地熱資源ポテンシャル調査への空中物理探査の適用性"},{"@language":"en","@value":"Applicability of airborne geophysics for geothermal potential surveys in promised areas in Japan"},{"@language":"ja-Kana","@value":"ニホン ノ チネツ シゲン ポテンシャル チョウサ エ ノ クウチュウ ブツリ タンサ ノ テキヨウセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390853908029869568","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Multi-physics data integration for interpretation and lithology classification"},{"@language":"ja","@value":"多種物理探査データ統合解析・評価による構造形態推定と岩相推定"},{"@value":"講演 多種物理探査データ統合解析・評価による構造形態推定と岩相推定"},{"@language":"ja-Kana","@value":"コウエン タシュ ブツリ タンサ データ トウゴウ カイセキ ・ ヒョウカ ニ ヨル コウゾウ ケイタイ スイテイ ト ガンソウ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588891962970624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Eigenvector of gravity gradient tensor for estimating fault dips considering fault type"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1365-2478.2009.00830.x"},{"@type":"CROSSREF","@value":"10.1186/s40645-017-0130-0_references_DOI_JRZFyoItWFc5iImcV5ljnNb1R2L"},{"@type":"CROSSREF","@value":"10.3720/japt.84.42_references_DOI_JRZFyoItWFc5iImcV5ljnNb1R2L"},{"@type":"CROSSREF","@value":"10.3124/segj.70.1_references_DOI_JRZFyoItWFc5iImcV5ljnNb1R2L"},{"@type":"CROSSREF","@value":"10.3124/segj.70.96_references_DOI_JRZFyoItWFc5iImcV5ljnNb1R2L"},{"@type":"CROSSREF","@value":"10.3124/segj.69.5_references_DOI_JRZFyoItWFc5iImcV5ljnNb1R2L"}]}