Upper mantle lateral heterogeneities and magnetotelluric daily variation data
Identifieur interne : 001949 ( Istex/Corpus ); précédent : 001948; suivant : 001950Upper mantle lateral heterogeneities and magnetotelluric daily variation data
Auteurs : J. L. Counil ; M. Menvielle ; J. L. Le MouelSource :
- pure and applied geophysics [ 0033-4553 ] ; 1987-03-01.
Abstract
Abstract: We use telluric and magnetic data of the diurnal variation recorded in Europe, Australia and North America to study the magnetotelluric tensor in the 6h–24h period range. We use associate directions and we eliminate the effects of deviation of telluric currents. We thus obtain for each observatory reliable phases and apparent resistivity values representative of the neighbouring stratified substratum. It appears that the values obtained in the four European observatories (Saint-Maur, France; Ebro, Spain; Toledo, Spain; Nagycenk, Hungary) give similar results and that these results are different from those obtained either in Tucson (USA) or in Watheroo (Australia). Using Bostick transform we interpret these phase and apparent resistivity values in terms of conductivity of the upper mantle. We discuss then the conductivity heterogeneities in terms of change either in temperature, or partial melting or percentage of fluids of the upper mantle: at depths of about 300 km, the upper mantle appears to be 100 °C hotter under Australia than under Europe; the probable presence of fluids at depths about 100 km in the southwestern North America upper mantle appears to be responsible for the high observed conductivities. All these conductivity values are coherent with tomography results from Woodhouse and Dziewonsky: high (low) conductivities are cohernet with low (high)seismic wave velocities.
Url:
DOI: 10.1007/BF00874500
Links to Exploration step
ISTEX:96F7E62528FA095306B339AA4E91CFD51478542ELe document en format XML
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CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</mods:affiliation></affiliation></author><author><name sortKey="Menvielle, M" sort="Menvielle, M" uniqKey="Menvielle M" first="M." last="Menvielle">M. Menvielle</name><affiliation><mods:affiliation>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</mods:affiliation></affiliation></author><author><name sortKey="Le Mouel, J L" sort="Le Mouel, J L" uniqKey="Le Mouel J" first="J. L." last="Le Mouel">J. L. Le Mouel</name><affiliation><mods:affiliation>Laboratoire de Géomagnétisme, I.P.G.P., U.A. 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We use associate directions and we eliminate the effects of deviation of telluric currents. We thus obtain for each observatory reliable phases and apparent resistivity values representative of the neighbouring stratified substratum. It appears that the values obtained in the four European observatories (Saint-Maur, France; Ebro, Spain; Toledo, Spain; Nagycenk, Hungary) give similar results and that these results are different from those obtained either in Tucson (USA) or in Watheroo (Australia). Using Bostick transform we interpret these phase and apparent resistivity values in terms of conductivity of the upper mantle. We discuss then the conductivity heterogeneities in terms of change either in temperature, or partial melting or percentage of fluids of the upper mantle: at depths of about 300 km, the upper mantle appears to be 100 °C hotter under Australia than under Europe; the probable presence of fluids at depths about 100 km in the southwestern North America upper mantle appears to be responsible for the high observed conductivities. All these conductivity values are coherent with tomography results from Woodhouse and Dziewonsky: high (low) conductivities are cohernet with low (high)seismic wave velocities.</div></front></TEI><istex><corpusName>springer</corpusName><author><json:item><name>J. L. Counil</name><affiliations><json:string>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</json:string></affiliations></json:item><json:item><name>M. Menvielle</name><affiliations><json:string>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</json:string></affiliations></json:item><json:item><name>J. L. Le Mouel</name><affiliations><json:string>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</json:string></affiliations></json:item></author><articleId><json:string>BF00874500</json:string><json:string>Art7</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>OriginalPaper</json:string></originalGenre><abstract>Abstract: We use telluric and magnetic data of the diurnal variation recorded in Europe, Australia and North America to study the magnetotelluric tensor in the 6h–24h period range. We use associate directions and we eliminate the effects of deviation of telluric currents. We thus obtain for each observatory reliable phases and apparent resistivity values representative of the neighbouring stratified substratum. It appears that the values obtained in the four European observatories (Saint-Maur, France; Ebro, Spain; Toledo, Spain; Nagycenk, Hungary) give similar results and that these results are different from those obtained either in Tucson (USA) or in Watheroo (Australia). Using Bostick transform we interpret these phase and apparent resistivity values in terms of conductivity of the upper mantle. We discuss then the conductivity heterogeneities in terms of change either in temperature, or partial melting or percentage of fluids of the upper mantle: at depths of about 300 km, the upper mantle appears to be 100 °C hotter under Australia than under Europe; the probable presence of fluids at depths about 100 km in the southwestern North America upper mantle appears to be responsible for the high observed conductivities. All these conductivity values are coherent with tomography results from Woodhouse and Dziewonsky: high (low) conductivities are cohernet with low (high)seismic wave velocities.</abstract><qualityIndicators><score>7.532</score><pdfVersion>1.3</pdfVersion><pdfPageSize>475.28 x 677 pts</pdfPageSize><refBibsNative>false</refBibsNative><keywordCount>0</keywordCount><abstractCharCount>1414</abstractCharCount><pdfWordCount>7571</pdfWordCount><pdfCharCount>43871</pdfCharCount><pdfPageCount>22</pdfPageCount><abstractWordCount>211</abstractWordCount></qualityIndicators><title>Upper mantle lateral heterogeneities and magnetotelluric daily variation data</title><refBibs><json:item><host><pages><last>141</last><first>129</first></pages><author><json:item><name>Adam </name></json:item><json:item><name>A Vero</name></json:item><json:item><name>J </name></json:item><json:item><name>Wallner </name></json:item><json:item><name>A </name></json:item></author><title>Tellurische und erdmagnetische Messungen im Observatorium bei Nagyeenk</title><publicationDate>1966</publicationDate></host></json:item><json:item><author><json:item><name>R,J Banks</name></json:item></author><host><volume>17</volume><pages><last>487</last><first>457</first></pages><author></author><title>Geophys. J. R. Astr. Soc</title><publicationDate>1969</publicationDate></host><title>Geomagnetic variations and the electrical conductivity of the upper mantle</title><publicationDate>1969</publicationDate></json:item><json:item><author><json:item><name>R,J Banks</name></json:item></author><host><volume>24</volume><pages><first>332351</first></pages><author></author><title>J. Geomagn. Geoelectr</title><publicationDate>1972</publicationDate></host><title>The overall conductivity" distribution of the Earth</title><publicationDate>1972</publicationDate></json:item><json:item><author><json:item><name>Bauer </name></json:item><json:item><name>L,A </name></json:item></author><host><volume>27</volume><pages><last>34</last><first>1</first></pages><author></author><title>Terr. Mag. and Atm. Elect</title><publicationDate>1922</publicationDate></host><title>Some results of recent Earth current observations and relations with solar activity</title><publicationDate>1922</publicationDate></json:item><json:item><host><author><json:item><name>Bosttck </name></json:item><json:item><name>F,X Jr</name></json:item></author><title>A simple and almost exact method of magnetotelluric analysis (Abstract) Workshop on Electrical Method in Geothermal Exploration</title><publicationDate>1976</publicationDate></host></json:item><json:item><author><json:item><name>Campbell </name></json:item><json:item><name>W,H </name></json:item><json:item><name>Schlefmacher </name></json:item><json:item><name>E,R </name></json:item></author><host><volume>59</volume><pages><last>61</last><first>56</first></pages><author></author><title>Europe and Asia. J. Geophys</title><publicationDate>1986</publicationDate></host><title>A comparison of upper mantle subcontinentat electrical conductivity for North America</title><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>Cara </name></json:item><json:item><name>M </name></json:item></author><host><volume>54</volume><pages><last>460</last><first>439</first></pages><author></author><title>Geophys. J. R. Astr. Soc</title><publicationDate>1978</publicationDate></host><title>Regional variations of higher Rayleigh mode velocities: A spatial filtering method</title><publicationDate>1978</publicationDate></json:item><json:item><host><author><json:item><name>Cardus </name></json:item><json:item><name>J,O </name></json:item><json:item><name>Galdon </name></json:item><json:item><name>E </name></json:item></author><title>Observaeiones magneticas y telluricas en el observatorio del Ebro durante el decenio I950-1959</title><publicationDate>1962</publicationDate></host></json:item><json:item><author><json:item><name>Chapman </name></json:item><json:item><name>S </name></json:item></author><host><volume>218</volume><pages><last>125</last><first>95</first></pages><author></author><title>Phil. Trans. R. Soc</title><publicationDate>1919</publicationDate></host><title>The solar and lunar diurnal variation of the Earth magnetism</title><publicationDate>1919</publicationDate></json:item><json:item><author><json:item><name>Counil </name></json:item><json:item><name>J,L </name></json:item><json:item><name>Le Mouel</name></json:item><json:item><name>J,L </name></json:item><json:item><name>Menvielle </name></json:item><json:item><name>M </name></json:item></author><host><volume>78</volume><pages><last>845</last><first>831</first></pages><author></author><title>Geophys. J. R. Astr. Soc</title><publicationDate>1984</publicationDate></host><title>A study of the diurnal variation of the electromagnetic field in northern France using ancient recordings</title><publicationDate>1984</publicationDate></json:item><json:item><author><json:item><name>Counil </name></json:item><json:item><name>J,L </name></json:item><json:item><name>Le Mouel</name></json:item><json:item><name>J,L Menvlelle</name></json:item><json:item><name>M </name></json:item></author><host><volume>4</volume><pages><last>130</last><first>115</first></pages><author></author><title>Ann. Geophys</title><publicationDate>1986</publicationDate></host><title>Associate and conjugate direction concepts in magnetotellurics</title><publicationDate>1986</publicationDate></json:item><json:item><host><author><json:item><name>Coun~l </name></json:item><json:item><name>J,L Menwelle</name></json:item><json:item><name>M </name></json:item><json:item><name>Le Mouel</name></json:item><json:item><name>J,L </name></json:item></author><title>Study of the daily variation at Tucson (Arizona; USA): Experimental evidence of static distortion of telluric currents</title><publicationDate>1986</publicationDate></host></json:item><json:item><host><author><json:item><name>De Mtguel</name></json:item><json:item><name>L </name></json:item></author><title>Observatorio central geofisico de Toledo: corrientes telluricas ano 1948</title></host></json:item><json:item><host><author><json:item><name>De Miguel</name></json:item><json:item><name>L </name></json:item></author><title>Observatorio central geofisico de Toledo: corrientes telluricas ano 1949</title><publicationDate>1951</publicationDate></host></json:item><json:item><host><author><json:item><name>De Miguel</name></json:item><json:item><name>L </name></json:item></author><title>Observatorio Central geofisico de Toledo: corrientes telluricas ano 1952</title><publicationDate>1955</publicationDate></host></json:item><json:item><author><json:item><name>Duba </name></json:item><json:item><name>A Heard</name></json:item><json:item><name>H,C </name></json:item><json:item><name>Shock </name></json:item><json:item><name>R </name></json:item></author><host><volume>79</volume><pages><last>1673</last><first>166</first></pages><author></author><title>J. Geophys. Res</title><publicationDate>1974</publicationDate></host><title>Electrical conductivity of olivine at high pressure and under controlled oxygenfugacity</title><publicationDate>1974</publicationDate></json:item><json:item><author><json:item><name>Engebretson </name></json:item><json:item><name>D,C Cox</name></json:item><json:item><name>A </name></json:item><json:item><name>Thompson </name></json:item><json:item><name>G,A </name></json:item></author><host><volume>3</volume><pages><last>120</last><first>115</first></pages><author></author><title>Tectonics</title><publicationDate>1984</publicationDate></host><title>Correlation of plate motion with continental tectonics: Laramide to basin and range</title><publicationDate>1984</publicationDate></json:item><json:item><author><json:item><name>Fleming </name></json:item><json:item><name>J,A Johnston</name></json:item><json:item><name>H,F Forbush</name></json:item><json:item><name>S,E Mcn~sh</name></json:item><json:item><name>A,G </name></json:item><json:item><name>Scott </name></json:item><json:item><name>W,E </name></json:item></author><host><pages><last>1935</last><first>1919</first></pages><author></author><title>Magnetic results from Watheroo Observatory, Western Australia</title><publicationDate>1947</publicationDate></host><publicationDate>1947</publicationDate></json:item><json:item><author><json:item><name>Fleming </name></json:item><json:item><name>J,A Johnston</name></json:item><json:item><name>H,F Mcn1sh</name></json:item><json:item><name>A,G Parkinson</name></json:item><json:item><name>W,C Forbush</name></json:item><json:item><name>S,E Green</name></json:item><json:item><name>J,W </name></json:item><json:item><name>Scott </name></json:item><json:item><name>W,E </name></json:item></author><host><author></author><title>Magnetic results from Watheroo Observatory</title><publicationDate>1936</publicationDate></host><publicationDate>1936</publicationDate></json:item><json:item><author><json:item><name>Frantz </name></json:item><json:item><name>J,D </name></json:item><json:item><name>Marshall </name></json:item><json:item><name>W,L </name></json:item></author><host><volume>282</volume><pages><last>1693</last><first>1666</first></pages><author></author><title>Am. J. Sci</title><publicationDate>1982</publicationDate></host><title>Electrical conduetances and ionization constants of calcium chloride and magnesium chloride in aqueous solutions at temperatures to 600 ~ and pressures to 4000 bars</title><publicationDate>1982</publicationDate></json:item><json:item><author><json:item><name>Larsen </name></json:item><json:item><name>J,C </name></json:item></author><host><volume>43</volume><pages><last>46</last><first>17</first></pages><author></author><title>Geophys. J. R. Astr. Soc</title><publicationDate>1975</publicationDate></host><title>Low frequency (0.1 6.0 cpd) electromagnetic study of the deep mantle electrical conductivity beneath the Hawaian islands</title><publicationDate>1975</publicationDate></json:item><json:item><author><json:item><name>Larsen </name></json:item><json:item><name>J </name></json:item></author><host><volume>32</volume><pages><last>103</last><first>89</first></pages><author></author><title>J. Geomagn. Geoelectr</title><publicationDate>1980</publicationDate></host><title>Electromagnetic response .functions from interrupted and noisy data</title><publicationDate>1980</publicationDate></json:item><json:item><author><json:item><name>Le Mouel</name></json:item><json:item><name>J,L </name></json:item></author><host><author></author><title>L'induction dans le Globe</title><publicationDate>1976</publicationDate></host><publicationDate>1976</publicationDate></json:item><json:item><author><json:item><name>Le Mouel</name></json:item><json:item><name>J,L </name></json:item><json:item><name>Menvielle </name></json:item><json:item><name>M </name></json:item></author><host><volume>68</volume><pages><last>587</last><first>575</first></pages><author></author><title>Geophys. J. R. Astr. Soc</title><publicationDate>1982</publicationDate></host><title>Geomagnetic variation anomalies and deflection of telluric currents</title><publicationDate>1982</publicationDate></json:item><json:item><author><json:item><name>Madden </name></json:item><json:item><name>T,R </name></json:item></author><host><volume>41</volume><pages><last>125</last><first>1104</first></pages><author></author><title>Geophysics</title><publicationDate>1976</publicationDate></host><title>Random networks and mixing taws</title><publicationDate>1976</publicationDate></json:item><json:item><author><json:item><name>Matsushita </name></json:item><json:item><name>S </name></json:item></author><host><volume>1</volume><author></author><title>In Physics of Geomagnetic Phenomena</title><publicationDate>1967</publicationDate></host><title>Solar quiet and lunar daily variation fields</title><publicationDate>1967</publicationDate></json:item><json:item><author><json:item><name>Ma '~aud </name></json:item><json:item><name>P,N </name></json:item></author><host><volume>21</volume><pages><last>401</last><first>369</first></pages><author></author><title>Ann. Geophys</title><publicationDate>1965</publicationDate></host><title>Analyse morphologique de la variabilitd jour-d-jour de la variation journalibre rdguliOre S R du champ magndtigue terrestre, I. Le systOme de courants Cp (rkgions polaires et subpolaires)</title><publicationDate>1965</publicationDate></json:item><json:item><author><json:item><name>P,N Mayauig</name></json:item></author><host><volume>21</volume><pages><last>545</last><first>514</first></pages><author></author><title>Ann. Geophys</title><publicationDate>1965</publicationDate></host><title>Analyse morphologique de la variabiHt~ jour-h-jour de la variation journali~re rdguli&e Sr~ du champ magn~tique terrestre. 2. Le systbme de courants C M (rdgions non potaires)</title><publicationDate>1965</publicationDate></json:item><json:item><author><json:item><name>Mayauo </name></json:item><json:item><name>P,N </name></json:item></author><host><pages><first>113</first></pages><author></author><title>Atlas des Indices</title><publicationDate>1967</publicationDate></host><publicationDate>1967</publicationDate></json:item><json:item><author><json:item><name>Mayaud </name></json:item><json:item><name>P,N </name></json:item></author><host><volume>33</volume><pages><first>252</first></pages><author></author><title>commencements. IAGA Bull. Office</title><publicationDate>1973</publicationDate></host><title>A hundred year series of geomagnetic data, 1868-1967; indices aa, storm sudden</title><publicationDate>1973</publicationDate></json:item><json:item><author><json:item><name>J,P Mon 'ragner</name></json:item></author><host><volume>13</volume><pages><last>318</last><first>315</first></pages><author></author><title>Geophys. Res. Lett</title><publicationDate>1986</publicationDate></host><title>Three dimension structure of the Indian Ocean inferred from long period surface wave</title><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>Montagner </name></json:item><json:item><name>J,P </name></json:item><json:item><name>Jobert </name></json:item><json:item><name>N </name></json:item></author><host><volume>10</volume><pages><last>276</last><first>273</first></pages><author></author><title>Geophys. Res. Lett</title><publicationDate>1983</publicationDate></host><title>Variation with age of the deep structure of the Pacific Ocean inferred from very long period Rayleigh wave dispersion</title><publicationDate>1983</publicationDate></json:item><json:item><author><json:item><name>Morse </name></json:item><json:item><name>S,A </name></json:item></author><host><pages><first>493</first></pages><author></author><title>Basalts and Phase Diagrams</title><publicationDate>1980</publicationDate></host><publicationDate>1980</publicationDate></json:item><json:item><author><json:item><name>Moureaux </name></json:item><json:item><name>T </name></json:item></author><host><volume>6</volume><author></author><title>Annales du Bureau Central</title><publicationDate>1895</publicationDate></host><title>Observations magndtiques faites au Parc Saint-Maur durant l'annke 1893</title><publicationDate>1895</publicationDate></json:item><json:item><author><json:item><name>Moureaux </name></json:item><json:item><name>T </name></json:item></author><host><volume>6</volume><issue>6</issue><author></author><title>Annales du Bureau Central</title><publicationDate>1896</publicationDate></host><title>Observations magnktiques faites au Pare Saint-Maur durant l'annke 1894</title><publicationDate>1896</publicationDate></json:item><json:item><author><json:item><name>Moureaux </name></json:item><json:item><name>T </name></json:item></author><host><volume>6</volume><author></author><title>Annales du Bureau Central</title><publicationDate>1897</publicationDate></host><title>Observations magndtiques faites au Parc Saint-Maur durant l'annde 1895</title><publicationDate>1897</publicationDate></json:item><json:item><author><json:item><name>Natae </name></json:item><json:item><name>H,C Nakanisni</name></json:item><json:item><name>I </name></json:item><json:item><name>Anderson </name></json:item><json:item><name>D,L </name></json:item></author><host><volume>11</volume><pages><last>112</last><first>109</first></pages><author></author><title>Geophys. Res. Lett</title><publicationDate>1984</publicationDate></host><title>Anisotrophy of shear velocity inhomogeneities in the upper mantle</title><publicationDate>1984</publicationDate></json:item><json:item><author><json:item><name>Olhoeft </name></json:item><json:item><name>G,R </name></json:item></author><host><pages><first>548</first></pages><author></author><title>Electrical properties of rocks, In Physical Properties of Rocks and Minerals</title><publicationDate>1981</publicationDate></host><publicationDate>1981</publicationDate></json:item><json:item><author><json:item><name>Parker </name></json:item><json:item><name>R,L </name></json:item></author><host><volume>22</volume><pages><last>138</last><first>121</first></pages><author></author><title>Geophys. J. R. Astr. Soc</title><publicationDate>1970</publicationDate></host><title>The inverse problem of electrical conductivity in the mantle</title><publicationDate>1970</publicationDate></json:item><json:item><author><json:item><name>E,I Parkriomenko</name></json:item></author><host><volume>20</volume><pages><last>218</last><first>193</first></pages><author></author><title>Rev. Geophys. Space Phys</title><publicationDate>1982</publicationDate></host><title>Electrical resistivity of minerals and rocks at high temperature and pressure</title><publicationDate>1982</publicationDate></json:item><json:item><author><json:item><name>Ranganayaki </name></json:item><json:item><name>R,P </name></json:item></author><host><volume>49</volume><pages><last>1748</last><first>1731</first></pages><author></author><title>Geophysics</title><publicationDate>1984</publicationDate></host><title>An interpretive analysis of magnetotelluric data</title><publicationDate>1984</publicationDate></json:item><json:item><host><author><json:item><name>Ringwood </name></json:item><json:item><name>A,E </name></json:item></author><title>Composition and Petrology of the Earth's Mantle</title><publicationDate>1975</publicationDate></host></json:item><json:item><author><json:item><name>Roonev </name></json:item><json:item><name>W,J </name></json:item></author><host><volume>49</volume><pages><last>157</last><first>147</first></pages><author></author><title>Terr. Mag. and Atm. Elect</title><publicationDate>1944</publicationDate></host><title>Summary of Earth current records from Tucson, Arizona, for a complete sunspotcycle</title><publicationDate>1944</publicationDate></json:item><json:item><author><json:item><name>Rooney </name></json:item><json:item><name>W,J </name></json:item></author><host><volume>175</volume><author></author><title>Carnegie Inst. Wash. Pub</title><publicationDate>1949</publicationDate></host><title>Earth current results at Tucson magnetic observatory 1932 1942. Researches of the Department of Terrestrial Magnetism</title><publicationDate>1949</publicationDate></json:item><json:item><host><author><json:item><name>Rooney </name></json:item><json:item><name>W,J </name></json:item><json:item><name>Gish </name></json:item><json:item><name>O,H </name></json:item></author><title>Earth current results from Watheroo Observatory, Western Australia, 1932-1942. Researches of the Department of Terrestrial Magnetism</title><publicationDate>1949</publicationDate></host></json:item><json:item><author><json:item><name>B,A Romanowlcz</name></json:item></author><host><volume>57</volume><pages><last>506</last><first>479</first></pages><author></author><title>Geophys. J. R. Astr. Soc</title><publicationDate>1979</publicationDate></host><title>Seismic structure of the upper mantle beneath the United States by threedimensional inversion of body wave arrival times</title><publicationDate>1979</publicationDate></json:item><json:item><author><json:item><name>Romanowicz </name></json:item><json:item><name>B,A </name></json:item></author><host><volume>63</volume><pages><last>232</last><first>217</first></pages><author></author><title>Geophys. J. R. Astr. Soc</title><publicationDate>1980</publicationDate></host><title>A study of large-scale lateral variations of P-velocity in the upper mantle beneath western Europe</title><publicationDate>1980</publicationDate></json:item><json:item><host><author><json:item><name>Schultz </name></json:item><json:item><name>A </name></json:item></author><title>On the electrical heterogeneity of the Earth's interior: A global study of mid-mantle conductivity</title><publicationDate>1985</publicationDate></host></json:item><json:item><author><json:item><name>Sclater </name></json:item><json:item><name>J,G Jaupart</name></json:item><json:item><name>C </name></json:item><json:item><name>Galson </name></json:item><json:item><name>D </name></json:item></author><host><volume>18</volume><pages><last>311</last><first>269</first></pages><author></author><title>Rev. Geophys. Space Phys</title><publicationDate>1980</publicationDate></host><title>The heat flow through oceanic and continental crust and the heat loss of the Earth</title><publicationDate>1980</publicationDate></json:item><json:item><author><json:item><name>Shankland </name></json:item><json:item><name>T,J </name></json:item></author><host><volume>10</volume><pages><last>219</last><first>209</first></pages><author></author><title>Phys. Earth Planet. Interiors</title><publicationDate>1975</publicationDate></host><title>Electrical conduction in rocks and minerals: Parameters for interpretation</title><publicationDate>1975</publicationDate></json:item><json:item><author><json:item><name>Shankland </name></json:item><json:item><name>T,J </name></json:item><json:item><name>Ander </name></json:item><json:item><name>M,E </name></json:item></author><host><volume>88</volume><pages><last>9484</last><first>9475</first></pages><author></author><title>J. Geophys. Res</title><publicationDate>1983</publicationDate></host><title>Electrical conductivity, temperatures andfluids in the lower crust</title><publicationDate>1983</publicationDate></json:item><json:item><author><json:item><name>Shankland </name></json:item><json:item><name>T,J </name></json:item><json:item><name>Waff </name></json:item><json:item><name>H,S </name></json:item></author><host><volume>82</volume><pages><last>5417</last><first>5409</first></pages><author></author><title>J. Geophys. Res</title><publicationDate>1977</publicationDate></host><title>Partial melting and electrical conductivity anomalies in the upper mantle</title><publicationDate>1977</publicationDate></json:item><json:item><author><json:item><name>Tarits </name></json:item><json:item><name>P </name></json:item></author><host><pages><last>226</last><first>215</first></pages><author></author><title>Conductivity and fluids in the oceanic upper mantle</title><publicationDate>1986</publicationDate></host><publicationDate>1986</publicationDate></json:item><json:item><author><json:item><name>Woodhouse </name></json:item><json:item><name>J,H </name></json:item><json:item><name>Dz1ewonsk~ </name></json:item><json:item><name>A,M </name></json:item></author><host><volume>89</volume><pages><last>5986</last><first>5953</first></pages><author></author><title>J. Geophys. Res</title><publicationDate>1984</publicationDate></host><title>Mapping the upper mantle: Three-dimensional modelling of Earth structure by inversion of seismic waveforms</title><publicationDate>1984</publicationDate></json:item><json:item><author><json:item><name>Wyllie </name></json:item><json:item><name>P,J </name></json:item></author><host><author></author><title>The Dynamic Earth: Textbook in Geosciences</title><publicationDate>1971</publicationDate></host><publicationDate>1971</publicationDate></json:item><json:item><author><json:item><name>Yoshimatsu </name></json:item><json:item><name>T </name></json:item></author><host><pages><last>75</last><first>1</first></pages><author></author><title>Memo. Kakioka Mag. Obs</title><publicationDate>1957</publicationDate></host><title>Universal Earth currents and their local character&tics</title><publicationDate>1957</publicationDate></json:item></refBibs><genre><json:string>research-article</json:string></genre><host><volume>125</volume><pages><last>340</last><first>319</first></pages><issn><json:string>0033-4553</json:string></issn><issue>2-3</issue><subject><json:item><value>Geophysics/Geodesy</value></json:item></subject><journalId><json:string>24</json:string></journalId><genre><json:string>journal</json:string></genre><language><json:string>unknown</json:string></language><eissn><json:string>1420-9136</json:string></eissn><title>pure and applied geophysics</title><publicationDate>1987</publicationDate><copyrightDate>1987</copyrightDate></host><categories><wos><json:string>science</json:string><json:string>geochemistry & geophysics</json:string></wos><scienceMetrix><json:string>natural sciences</json:string><json:string>earth & environmental sciences</json:string><json:string>geochemistry & geophysics</json:string></scienceMetrix></categories><publicationDate>1987</publicationDate><copyrightDate>1987</copyrightDate><doi><json:string>10.1007/BF00874500</json:string></doi><id>96F7E62528FA095306B339AA4E91CFD51478542E</id><score>0.13148001</score><fulltext><json:item><extension>pdf</extension><original>true</original><mimetype>application/pdf</mimetype><uri>https://api.istex.fr/document/96F7E62528FA095306B339AA4E91CFD51478542E/fulltext/pdf</uri></json:item><json:item><extension>zip</extension><original>false</original><mimetype>application/zip</mimetype><uri>https://api.istex.fr/document/96F7E62528FA095306B339AA4E91CFD51478542E/fulltext/zip</uri></json:item><istex:fulltextTEI uri="https://api.istex.fr/document/96F7E62528FA095306B339AA4E91CFD51478542E/fulltext/tei"><teiHeader><fileDesc><titleStmt><title level="a" type="main" xml:lang="en">Upper mantle lateral heterogeneities and magnetotelluric daily variation data</title><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt><respStmt><resp>Références bibliographiques récupérées via GROBID</resp><name resp="ISTEX-API">ISTEX-API (INIST-CNRS)</name></respStmt></titleStmt><publicationStmt><authority>ISTEX</authority><publisher>Birkhäuser-Verlag</publisher><pubPlace>Basel</pubPlace><availability><p>Birkhäuser Verlag, 1987</p></availability><date>1986-07-01</date></publicationStmt><sourceDesc><biblStruct type="inbook"><analytic><title level="a" type="main" xml:lang="en">Upper mantle lateral heterogeneities and magnetotelluric daily variation data</title><author xml:id="author-1"><persName><forename type="first">J.</forename><surname>Counil</surname></persName><affiliation>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</affiliation></author><author xml:id="author-2"><persName><forename type="first">M.</forename><surname>Menvielle</surname></persName><affiliation>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</affiliation></author><author xml:id="author-3"><persName><forename type="first">J.</forename><surname>Le Mouel</surname></persName><affiliation>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</affiliation></author></analytic><monogr><title level="j">pure and applied geophysics</title><title level="j" type="sub">pageoph</title><title level="j" type="abbrev">PAGEOPH</title><idno type="journal-ID">24</idno><idno type="pISSN">0033-4553</idno><idno type="eISSN">1420-9136</idno><idno type="issue-article-count">15</idno><idno type="volume-issue-count">6</idno><imprint><publisher>Birkhäuser-Verlag</publisher><pubPlace>Basel</pubPlace><date type="published" when="1987-03-01"></date><biblScope unit="volume">125</biblScope><biblScope unit="issue">2-3</biblScope><biblScope unit="page" from="319">319</biblScope><biblScope unit="page" to="340">340</biblScope></imprint></monogr><idno type="istex">96F7E62528FA095306B339AA4E91CFD51478542E</idno><idno type="DOI">10.1007/BF00874500</idno><idno type="ArticleID">BF00874500</idno><idno type="ArticleID">Art7</idno></biblStruct></sourceDesc></fileDesc><profileDesc><creation><date>1986-07-01</date></creation><langUsage><language ident="en">en</language></langUsage><abstract xml:lang="en"><p>Abstract: We use telluric and magnetic data of the diurnal variation recorded in Europe, Australia and North America to study the magnetotelluric tensor in the 6h–24h period range. We use associate directions and we eliminate the effects of deviation of telluric currents. We thus obtain for each observatory reliable phases and apparent resistivity values representative of the neighbouring stratified substratum. It appears that the values obtained in the four European observatories (Saint-Maur, France; Ebro, Spain; Toledo, Spain; Nagycenk, Hungary) give similar results and that these results are different from those obtained either in Tucson (USA) or in Watheroo (Australia). Using Bostick transform we interpret these phase and apparent resistivity values in terms of conductivity of the upper mantle. We discuss then the conductivity heterogeneities in terms of change either in temperature, or partial melting or percentage of fluids of the upper mantle: at depths of about 300 km, the upper mantle appears to be 100 °C hotter under Australia than under Europe; the probable presence of fluids at depths about 100 km in the southwestern North America upper mantle appears to be responsible for the high observed conductivities. All these conductivity values are coherent with tomography results from Woodhouse and Dziewonsky: high (low) conductivities are cohernet with low (high)seismic wave velocities.</p></abstract><textClass><keywords scheme="Journal Subject"><list><head>Geosciences</head><item><term>Geophysics/Geodesy</term></item></list></keywords></textClass></profileDesc><revisionDesc><change when="1986-07-01">Created</change><change when="1987-03-01">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-11-22">References added</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2017-01-20">References added</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><extension>txt</extension><original>false</original><mimetype>text/plain</mimetype><uri>https://api.istex.fr/document/96F7E62528FA095306B339AA4E91CFD51478542E/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Springer, Publisher found" wicri:toSee="no header"><istex:xmlDeclaration>version="1.0" encoding="UTF-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//Springer-Verlag//DTD A++ V2.4//EN" URI="http://devel.springer.de/A++/V2.4/DTD/A++V2.4.dtd" name="istex:docType"></istex:docType><istex:document><Publisher><PublisherInfo><PublisherName>Birkhäuser-Verlag</PublisherName><PublisherLocation>Basel</PublisherLocation></PublisherInfo><Journal><JournalInfo JournalProductType="ArchiveJournal" NumberingStyle="Unnumbered"><JournalID>24</JournalID><JournalPrintISSN>0033-4553</JournalPrintISSN><JournalElectronicISSN>1420-9136</JournalElectronicISSN><JournalTitle>pure and applied geophysics</JournalTitle><JournalSubTitle>pageoph</JournalSubTitle><JournalAbbreviatedTitle>PAGEOPH</JournalAbbreviatedTitle><JournalSubjectGroup><JournalSubject Type="Primary">Geosciences</JournalSubject><JournalSubject Type="Secondary">Geophysics/Geodesy</JournalSubject></JournalSubjectGroup></JournalInfo><Volume><VolumeInfo VolumeType="Regular" TocLevels="0"><VolumeIDStart>125</VolumeIDStart><VolumeIDEnd>125</VolumeIDEnd><VolumeIssueCount>6</VolumeIssueCount></VolumeInfo><Issue IssueType="Combined"><IssueInfo TocLevels="0"><IssueIDStart>2</IssueIDStart><IssueIDEnd>3</IssueIDEnd><IssueArticleCount>15</IssueArticleCount><IssueHistory><CoverDate><DateString>1987</DateString><Year>1987</Year><Month>3</Month></CoverDate></IssueHistory><IssueCopyright><CopyrightHolderName>Birkhäuser-Verlag</CopyrightHolderName><CopyrightYear>1987</CopyrightYear></IssueCopyright></IssueInfo><Article ID="Art7"><ArticleInfo Language="En" ArticleType="OriginalPaper" NumberingStyle="Unnumbered" TocLevels="0" ContainsESM="No"><ArticleID>BF00874500</ArticleID><ArticleDOI>10.1007/BF00874500</ArticleDOI><ArticleSequenceNumber>7</ArticleSequenceNumber><ArticleTitle Language="En">Upper mantle lateral heterogeneities and magnetotelluric daily variation data</ArticleTitle><ArticleFirstPage>319</ArticleFirstPage><ArticleLastPage>340</ArticleLastPage><ArticleHistory><RegistrationDate><Year>2004</Year><Month>12</Month><Day>8</Day></RegistrationDate><Received><Year>1986</Year><Month>7</Month><Day>1</Day></Received><Revised><Year>1986</Year><Month>9</Month><Day>16</Day></Revised><Accepted><Year>1986</Year><Month>9</Month><Day>16</Day></Accepted></ArticleHistory><ArticleCopyright><CopyrightHolderName>Birkhäuser Verlag</CopyrightHolderName><CopyrightYear>1987</CopyrightYear></ArticleCopyright><ArticleGrants Type="Regular"><MetadataGrant Grant="OpenAccess"></MetadataGrant><AbstractGrant Grant="OpenAccess"></AbstractGrant><BodyPDFGrant Grant="Restricted"></BodyPDFGrant><BodyHTMLGrant Grant="Restricted"></BodyHTMLGrant><BibliographyGrant Grant="Restricted"></BibliographyGrant><ESMGrant Grant="Restricted"></ESMGrant></ArticleGrants><ArticleContext><JournalID>24</JournalID><VolumeIDStart>125</VolumeIDStart><VolumeIDEnd>125</VolumeIDEnd><IssueIDStart>2</IssueIDStart><IssueIDEnd>3</IssueIDEnd></ArticleContext></ArticleInfo><ArticleHeader><AuthorGroup><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>J.</GivenName><GivenName>L.</GivenName><FamilyName>Counil</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>M.</GivenName><FamilyName>Menvielle</FamilyName></AuthorName></Author><Author AffiliationIDS="Aff1"><AuthorName DisplayOrder="Western"><GivenName>J.</GivenName><GivenName>L.</GivenName><Particle>Le</Particle><FamilyName>Mouel</FamilyName></AuthorName></Author><Affiliation ID="Aff1"><OrgDivision>Laboratoire de Géomagnétisme</OrgDivision><OrgName>I.P.G.P., U.A. CNRS 922</OrgName><OrgAddress><Street>4 Place Jussieu-Tour 14</Street><Postcode>F-75252</Postcode><City>PARIS CEDEX 05</City></OrgAddress></Affiliation></AuthorGroup><Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading><Para>We use telluric and magnetic data of the diurnal variation recorded in Europe, Australia and North America to study the magnetotelluric tensor in the 6h–24h period range. We use associate directions and we eliminate the effects of deviation of telluric currents. We thus obtain for each observatory reliable phases and apparent resistivity values representative of the neighbouring stratified substratum. It appears that the values obtained in the four European observatories (Saint-Maur, France; Ebro, Spain; Toledo, Spain; Nagycenk, Hungary) give similar results and that these results are different from those obtained either in Tucson (USA) or in Watheroo (Australia).</Para><Para>Using Bostick transform we interpret these phase and apparent resistivity values in terms of conductivity of the upper mantle. We discuss then the conductivity heterogeneities in terms of change either in temperature, or partial melting or percentage of fluids of the upper mantle: at depths of about 300 km, the upper mantle appears to be 100 °C hotter under Australia than under Europe; the probable presence of fluids at depths about 100 km in the southwestern North America upper mantle appears to be responsible for the high observed conductivities. All these conductivity values are coherent with tomography results from Woodhouse and Dziewonsky: high (low) conductivities are cohernet with low (high)seismic wave velocities.</Para></Abstract><KeywordGroup Language="En"><Heading>Key words</Heading><Keyword>Daily variation</Keyword><Keyword>upper mantle</Keyword><Keyword>lateral heterogeneities</Keyword><Keyword>conductivity</Keyword><Keyword>magnetotelluric</Keyword></KeywordGroup></ArticleHeader><NoBody></NoBody></Article></Issue></Volume></Journal></Publisher></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Upper mantle lateral heterogeneities and magnetotelluric daily variation data</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Upper mantle lateral heterogeneities and magnetotelluric daily variation data</title></titleInfo><name type="personal"><namePart type="given">J.</namePart><namePart type="given">L.</namePart><namePart type="family">Counil</namePart><affiliation>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">M.</namePart><namePart type="family">Menvielle</namePart><affiliation>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">J.</namePart><namePart type="given">L.</namePart><namePart type="family">Le Mouel</namePart><affiliation>Laboratoire de Géomagnétisme, I.P.G.P., U.A. CNRS 922, 4 Place Jussieu-Tour 14, F-75252, PARIS CEDEX 05</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="OriginalPaper"></genre><originInfo><publisher>Birkhäuser-Verlag</publisher><place><placeTerm type="text">Basel</placeTerm></place><dateCreated encoding="w3cdtf">1986-07-01</dateCreated><dateIssued encoding="w3cdtf">1987-03-01</dateIssued><copyrightDate encoding="w3cdtf">1987</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">Abstract: We use telluric and magnetic data of the diurnal variation recorded in Europe, Australia and North America to study the magnetotelluric tensor in the 6h–24h period range. We use associate directions and we eliminate the effects of deviation of telluric currents. We thus obtain for each observatory reliable phases and apparent resistivity values representative of the neighbouring stratified substratum. It appears that the values obtained in the four European observatories (Saint-Maur, France; Ebro, Spain; Toledo, Spain; Nagycenk, Hungary) give similar results and that these results are different from those obtained either in Tucson (USA) or in Watheroo (Australia). Using Bostick transform we interpret these phase and apparent resistivity values in terms of conductivity of the upper mantle. We discuss then the conductivity heterogeneities in terms of change either in temperature, or partial melting or percentage of fluids of the upper mantle: at depths of about 300 km, the upper mantle appears to be 100 °C hotter under Australia than under Europe; the probable presence of fluids at depths about 100 km in the southwestern North America upper mantle appears to be responsible for the high observed conductivities. All these conductivity values are coherent with tomography results from Woodhouse and Dziewonsky: high (low) conductivities are cohernet with low (high)seismic wave velocities.</abstract><relatedItem type="host"><titleInfo><title>pure and applied geophysics</title><subTitle>pageoph</subTitle></titleInfo><titleInfo type="abbreviated"><title>PAGEOPH</title></titleInfo><genre type="journal" displayLabel="Archive Journal"></genre><originInfo><dateIssued encoding="w3cdtf">1987-03-01</dateIssued><copyrightDate encoding="w3cdtf">1987</copyrightDate></originInfo><subject><genre>Geosciences</genre><topic>Geophysics/Geodesy</topic></subject><identifier type="ISSN">0033-4553</identifier><identifier type="eISSN">1420-9136</identifier><identifier type="JournalID">24</identifier><identifier type="IssueArticleCount">15</identifier><identifier type="VolumeIssueCount">6</identifier><part><date>1987</date><detail type="volume"><number>125</number><caption>vol.</caption></detail><detail type="issue"><number>2-3</number><caption>no.</caption></detail><extent unit="pages"><start>319</start><end>340</end></extent></part><recordInfo><recordOrigin>Birkhäuser-Verlag, 1987</recordOrigin></recordInfo></relatedItem><identifier type="istex">96F7E62528FA095306B339AA4E91CFD51478542E</identifier><identifier type="DOI">10.1007/BF00874500</identifier><identifier type="ArticleID">BF00874500</identifier><identifier type="ArticleID">Art7</identifier><accessCondition type="use and reproduction" contentType="copyright">Birkhäuser Verlag, 1987</accessCondition><recordInfo><recordContentSource>SPRINGER</recordContentSource><recordOrigin>Birkhäuser Verlag, 1987</recordOrigin></recordInfo></mods></metadata><serie></serie></istex></record>Pour manipuler ce document sous Unix (Dilib)
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