{"@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/1361981470260643200.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1365-2478.2012.01117.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2478.2012.01117.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2478.2012.01117.x"}}],"dc:title":[{"@value":"Review paper: Instrumentation for marine magnetotelluric and controlled source electromagnetic sounding"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>ABSTRACT</jats:title><jats:p>We review and describe the electromagnetic transmitters and receivers used to carry out magnetotelluric and controlled source soundings in the marine environment. Academic studies using marine electromagnetic methods started in the 1970s but during the last decade these methods have been used extensively by the offshore hydrocarbon exploration industry. The principal sensors (magnetometers and non‐polarizing electrodes) are similar to those used on land but magnetotelluric field strengths are not only much smaller on the deep sea‐floor but also fall off more rapidly with increasing frequency. As a result, magnetotelluric signals approach the noise floor of electric field and induction coil sensors (0.1 nV/m and 0.1 pT) at around 1 Hz in typical continental shelf environments. Fluxgate magnetometers have higher noise than induction coils at periods shorter than 500 s but can still be used to collect sea‐floor magnetotelluric data down to 40–100 s. Controlled source transmitters using electric dipoles can be towed continuously through the seawater or on the sea‐bed, achieving output currents of 1000 A or more, limited by the conductivity of seawater and the power that can be transmitted down the cables used to tow the devices behind a ship. The maximum source‐receiver separation achieved in controlled source soundings depends on both the transmitter dipole moment and on the receiver noise floor and is typically around 10 km in continental shelf exploration environments. The position of both receivers and transmitters needs to be navigated using either long baseline or short baseline acoustic ranging, while sea‐floor receivers need additional measurements of orientations from compasses and tiltmeters. All equipment has to be packaged to accommodate the high pressure (up to 40 MPa) and corrosive properties of seawater. Usually receiver instruments are self‐contained, battery powered and have highly accurate clocks for timekeeping, even when towed on the sea‐floor or in the water column behind a transmitter.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981470260643200","@type":"Researcher","foaf:name":[{"@value":"Steven Constable"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00168025"},{"@type":"EISSN","@value":"13652478"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00168025"}],"prism:publicationName":[{"@value":"Geophysical Prospecting"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2013-01-29","prism:volume":"61","prism:number":"s1","prism:startingPage":"505","prism:endingPage":"532"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1365-2478.2012.01117.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1365-2478.2012.01117.x"}],"createdAt":"2013-01-29","modifiedAt":"2023-09-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050022457826467968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Offshore-onshore resistivity imaging of freshwater using a controlled-source electromagnetic method: A feasibility study"}]},{"@id":"https://cir.nii.ac.jp/crid/1050022457826475776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A cost-effective three-dimensional marine controlled-source electromagnetic survey: Exploring seafloor massive sulfides"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708924339584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Robust data processing of noisy marine controlled-source electromagnetic data using independent component analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238117193344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evaluations of effectiveness of marine deep-towed DC resistivity survey in investigation of seafloor massive sulfide deposits"},{"@language":"ja","@value":"海底熱水鉱床調査における深海曳航式電気探査の有効性評価"},{"@language":"ja-Kana","@value":"カイテイ ネッスイ コウショウ チョウサ ニ オケル シンカイ エイコウシキ デンキ タンサ ノ ユウコウセイ ヒョウカ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842051751936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Validity of the dispersion relations in magnetotellurics. 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