Zobrazeno 1 - 5
of 5
pro vyhledávání: '"J.-C. Engels"'
Autor:
M. Girot, Hugues Lefort, Vincent Navarro, W. Szurhaj, B. Clair, H. Outin, N. Engrand, F. Villega, Sophie Dupont, Arielle Crespel, Romain Sonneville, J.-C. Engels, Andrea O. Rossetti, P. Thomas, L. Titomanlio, Stéphane Auvin, V. Alvarez, F. Santoli, Yonathan Freund, P. Convers, M.-O. Marcoux, V. Peigne, S. Demeret, P. Gueye, Philippe Gelisse
Publikováno v:
Annales françaises de médecine d’urgence. 10:151-186
La Société de réanimation de langue française et la Société française de médecine d’urgence ont décidé d’élaborer de nouvelles recommandations sur la prise en charge de l’état mal épileptique (EME) avec l’ambition de répondre le
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1988d0a4af64191ea26f896ad1eb017
https://doi.org/10.3166/afmu-2020-0232
https://doi.org/10.3166/afmu-2020-0232
Akademický článek
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Autor:
J. C. Engels, C. O. Ingamells
Publikováno v:
Geostandards and Geoanalytical Research. 1:51-60
Selection, preparation, analysis for composition and for degree of homogeneity, certification and distribution of a useful geochemical reference sample is a long and complicated endeavour. Certain basic principles must be observed if this endeavour -
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e15c3f1f5f3a000c2879060d875e7e34
https://doi.org/10.1111/j.1751-908x.1977.tb00858.x
https://doi.org/10.1111/j.1751-908x.1977.tb00858.x
Publikováno v:
Journal of Geophysical Research. 75:1579-1584
The epidote group of minerals is well-suited for age determination by the fission-track method. The minerals occur in a large variety of rock types; fission tracks are readily etched in them; and epidote retains its tracks at high temperatures. No an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cbdb684955c957cc4c44498aa37fefea
https://doi.org/10.1029/jb075i008p01579
https://doi.org/10.1029/jb075i008p01579
Publikováno v:
Geological Society of America Bulletin. 87:1217
Contact relations and internal fabric suggest that penetrative metamorphism and deformation of parental rocks of the Okanogan gneiss dome culminated in their mobilization and diapiric intrusion into the country rocks. The gneiss dome cuts both pluton
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b175de3e9877f6ccc4fd6f39f24854d3
https://doi.org/10.1130/0016-7606(1976)87<1217:aoeoto>2.0.co
https://doi.org/10.1130/0016-7606(1976)87<1217:aoeoto>2.0.co