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- W2034512934 abstract "La fosse Blanco (ride Juan de Fuca) expose une section continue de la croûte océanique supérieure (basaltes et complexe filonien)hydrothermalisée dans un contexte de faille transformante. Des mesures de microthermométrie sur inclusions fluides couplées à des mesures des isotopes stables de l'oxygène ont été réalisées pour étudier l'évolution de la circulation hydrothermale. Un réseau dense de fractures, directement lié au site géotectonique de faille transformante, a entretenu une circulation hydrothermale horsaxe, encore chaude (environ 200 °C), enracinée jusqu'au toit de l'unité des diabases. The Blanco trough (Juan de Fuca ridge) exposes a continuous section of the upper part of the oceanic crust (basalts and sheeted dykes) hydrothermally altered in a transform fault context. Coupled microthermometric measurements on fluid inclusions and stable oxygen isotope compositions of secondary phases from the diabase unit were performed to investigate the evolution of hydrothermal fluids. The existence of a dense fracture network directly linked to the geotectonic transform fault environment has maintained a still hot hydrothermal circulation (about 200 °C) rooted down to the top of the diabase unit." @default.
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- W2034512934 date "1997-06-01" @default.
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- W2034512934 title "Evolution de la circulation hydrothermale en contexte de faille transformante: la fosse Blanco (dorsale Juan de Fuca)" @default.
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- W2034512934 doi "https://doi.org/10.1016/s1251-8050(97)83984-5" @default.
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