Zobrazeno 1 - 5
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pro vyhledávání: '"Jacky Bouloton"'
Autor:
Jacky Bouloton
Publikováno v:
Volcanica, Vol 4, Iss 2, Pp 149-187 (2021)
Almandine-rich garnets from a Neogene andesite of Slovakia can be divided into two main types. Garnet megacrysts are magmatic and form a chemically homogeneous group that contains, on average, about 5 wt% CaO and 4.5 wt% MgO as petrogenetically signi
Externí odkaz:
https://doaj.org/article/5dcbfc7a8902456f939323eb273a1f58
Publikováno v:
Journal of African Earth Sciences
Journal of African Earth Sciences, Elsevier, 2019, 149, pp.451-464. ⟨10.1016/j.jafrearsci.2018.08.023⟩
Journal of African Earth Sciences, 2019, 149, pp.451-464. ⟨10.1016/j.jafrearsci.2018.08.023⟩
Journal of African Earth Sciences, Elsevier, 2019, 149, pp.451-464. ⟨10.1016/j.jafrearsci.2018.08.023⟩
Journal of African Earth Sciences, 2019, 149, pp.451-464. ⟨10.1016/j.jafrearsci.2018.08.023⟩
International audience; A dyke swarm composed of hypabyssal rocks of intermediate composition cross-cuts Variscan granites and Palaeozoic metasedimentary country-rocks of the Jebilet range. Based on K-Ar isotope dating on kaersutite phenocrysts, thes
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 330:241-244
Garnets from the Montasset microgranite (Velay, France) are the most magnesian garnets (up to 38.5 mol % pyrope) ever described in acidic rocks. Textural relations and chemical zoning profiles indicate that they grew with rising temperature in equili
Autor:
Jacky Bouloton
Publikováno v:
Canadian Journal of Earth Sciences. 29:658-668
Cordierite, a quite common mineral in granitic rocks, originates from various processes; many types of crystals can be found in a given massif. The high-level Oulad Ouaslam pluton, in Morocco, displays cordierites of three different origins. Primary
Publikováno v:
Comptes rendus de l’Académie des sciences. Série IIa, Sciences de la terre et des planètes
Comptes rendus de l’Académie des sciences. Série IIa, Sciences de la terre et des planètes, Elsevier, 1998, pp.473-177
Comptes rendus de l’Académie des sciences. Série IIa, Sciences de la terre et des planètes, Elsevier, 1998, pp.473-177
A garnet-spinel metaperidotite body has been found in the leptyno-amphibolitic complex of the central pan of the Maures Massif (Hercynian Belt, south eastern France). Based on bulk rock and mineral chemistry, a mantle tectonite origin can be ruled ou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::054f5b1bf9aaf08a23fca946e193bc08
https://hal.archives-ouvertes.fr/hal-00221523
https://hal.archives-ouvertes.fr/hal-00221523