Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Morgan J. Williams"'
Autor:
Ya-Jing Mao, Louise Schoneveld, Stephen J Barnes, Morgan J Williams, Ben-Xun Su, Philipp Ruprecht, Noreen J Evans, Ke-Zhang Qin
Publikováno v:
Journal of Petrology. 63
Olivine is an important mineral in mafic–ultramafic rocks and records various crustal and mantle processes in basaltic magma. Generally, phosphorus (P) is immobile in olivine and its zoning tends to record magmatic processes. In contrast, lithium (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::173a7f2f0ebe6f91089bedbd8eab160b
https://doi.org/10.1093/petrology/egac018
https://doi.org/10.1093/petrology/egac018
Autor:
Scott A. Whattam, Gretchen L. Früh-Green, Mathilde Cannat, Jan C.M. De Hoog, Esther M. Schwarzenbach, Javier Escartin, Barbara E. John, Mathew I. Leybourne, Morgan J. Williams, Stéphane Rouméjon, Norikatsu Akizawa, Chiara Boschi, Michelle Harris, Kirsten Wenzel, Andrew McCaig, Dominique Weis, Laura Bilenker
Publikováno v:
Chemical geology 594 (2022). doi:10.1016/j.chemgeo.2021.120681
info:cnr-pdr/source/autori:Whattam S.A.[1], Früh-Green G.L.[2], Cannat M.[3], De Hoog J.C.M.[4], Schwarzenbach E.M.[5], Escartin J.[6], John B.E.[7], Leybourne M.I.[8], Williams M.J.[9], Rouméjon S.[2], Akizawa N.[10], Boschi C.[11], Harris M.[12], Wenzel K.[13], McCaig A.[14], Weis D.[15], Bilenker L.[16]/titolo:Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes/doi:10.1016%2Fj.chemgeo.2021.120681/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:594
Whattam, S A, Früh-green, G L, Cannat, M, De Hoog, J C M, Schwarzenbach, E M, Escartin, J, John, B E, Leybourne, M I, Williams, M J, Rouméjon, S, Akizawa, N, Boschi, C, Harris, M, Wenzel, K, Mccaig, A, Weis, D & Bilenker, L 2021, ' Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes ', Chemical Geology . https://doi.org/10.1016/j.chemgeo.2021.120681
Chemical Geology, 594
info:cnr-pdr/source/autori:Whattam S.A.[1], Früh-Green G.L.[2], Cannat M.[3], De Hoog J.C.M.[4], Schwarzenbach E.M.[5], Escartin J.[6], John B.E.[7], Leybourne M.I.[8], Williams M.J.[9], Rouméjon S.[2], Akizawa N.[10], Boschi C.[11], Harris M.[12], Wenzel K.[13], McCaig A.[14], Weis D.[15], Bilenker L.[16]/titolo:Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes/doi:10.1016%2Fj.chemgeo.2021.120681/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:594
Whattam, S A, Früh-green, G L, Cannat, M, De Hoog, J C M, Schwarzenbach, E M, Escartin, J, John, B E, Leybourne, M I, Williams, M J, Rouméjon, S, Akizawa, N, Boschi, C, Harris, M, Wenzel, K, Mccaig, A, Weis, D & Bilenker, L 2021, ' Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes ', Chemical Geology . https://doi.org/10.1016/j.chemgeo.2021.120681
Chemical Geology, 594
International Ocean Discovery Program (IODP) Expedition 357 drilled 17 shallow sites distributed ~10 km in the spreading direction (from west to east) across the Atlantis Massif oceanic core complex (Mid-Atlantic Ridge, 30°N). Mantle exposed in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40c118812ebac27a8f1f457abb54d52e
http://www.cnr.it/prodotto/i/466258
http://www.cnr.it/prodotto/i/466258
