Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Jean-Michel Liotard"'
Autor:
H. Mehdizadeh, Delphine Bosch, Michel Condomines, Jean-Michel Liotard, Jean-Marie Dautria, Jean-François Ritz
Publikováno v:
International Journal of Earth Sciences
International Journal of Earth Sciences, Springer Verlag, 2008, 97 (1), pp.89-102. ⟨10.1007/s00531-006-0159-6⟩
International Journal of Earth Sciences, Springer Verlag, 2008, 97 (1), pp.89-102. ⟨10.1007/s00531-006-0159-6⟩
The activity of the Damavand volcano (Central Alborz, northern Iran) began 1.8 Ma ago and continued up to 7 ka BP. Although the volcanic suite is clearly of shoshonitic affinity, only two petrographic types can be distinguished in the studied lavas:
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8438525ab94bd9a479e04ffbe0241a9a
https://doi.org/10.1007/s00531-006-0159-6
https://doi.org/10.1007/s00531-006-0159-6
Publikováno v:
Comptes Rendus Geoscience. 336:971-981
Resume Les compositions isotopiques en Sr et Nd d'un trachyte, de huit phonolites et de cinq basaltes ont ete mesurees. Une contamination crustale importante, contemporaine de la differenciation, n'apparait que dans le cas du trachyte. Certaines phon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d395fa7c2f8b9f4b9c8e7eb49a6af814
https://doi.org/10.1016/j.crte.2004.03.006
https://doi.org/10.1016/j.crte.2004.03.006
Publikováno v:
Comptes Rendus Geoscience. 334:111-117
Lavas of the Quaternary Damavand volcano (Central Alborz, Northern Iran) have been analysed for major and trace elements. The shoshonitic character of this magmatic series is definitively confirmed and most samples correspond to banakites. The Nb, Ta
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::68f71caf8b63945c187781b06c2b9e57
https://doi.org/10.1016/s1631-0713(02)01717-0
https://doi.org/10.1016/s1631-0713(02)01717-0
Publikováno v:
Chemical Geology. 176:235-263
Basaltic glasses are considered as natural analogs for industrial nuclear aluminoborosilicate glasses. Alteration experiments were conducted in closed and open systems at 90°C with a synthetic basalt glass doped with 1% lithium (dissolution tracer).
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38a45f9e9105e6cab0d1cd78aedabec4
https://doi.org/10.1016/s0009-2541(00)00400-9
https://doi.org/10.1016/s0009-2541(00)00400-9
Publikováno v:
Journal of Nuclear Materials. 282:40-46
A synthetic basaltic glass was dissolved experimentally at 90°C under static conditions in initially pure water. The basaltic glass dissolution rates measured near and far from equilibrium were compared with those of SON 68 nuclear waste glass. Expe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ab320eed7f17e5b32384e46565786332
https://doi.org/10.1016/s0022-3115(00)00399-8
https://doi.org/10.1016/s0022-3115(00)00399-8
Publikováno v:
Comptes Rendus Géoscience
Comptes Rendus Géoscience, Elsevier, 2006, 338 (8), pp.527-536. ⟨10.1016/j.crte.2006.03.001⟩
Comptes Rendus Géoscience, Elsevier, 2006, 338 (8), pp.527-536. ⟨10.1016/j.crte.2006.03.001⟩
International audience; Lherzolite xenoliths with calcite-rich microgranular secondary aggregates (0.1–1 mm) have been sampled in a Messinian breccia pipe from the northeastern part of the Languedoc volcanic province (South France). Their study sho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::288c672fdf2eb9eebcabfb061c73575a
https://hal.archives-ouvertes.fr/hal-02009091
https://hal.archives-ouvertes.fr/hal-02009091
Publikováno v:
Périodiques Scientifiques en Édition Électronique.
Some tertiary and quaternary basaltic lavas from the French Massif Central with their associated amphiboles megacrysts have been analysed for major elements, transition elements, and the following trace elements : Rb, Sr, Ba, Hf, Ta, Th, U, and Rare
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4249556f8c1983580749fde262fdeaed
https://www.persee.fr/doc/bulmi_0180-9210_1983_num_106_4_7725
https://www.persee.fr/doc/bulmi_0180-9210_1983_num_106_4_7725