Zobrazeno 1 - 10
of 76
pro vyhledávání: '"G.C. AMSTUTZ"'
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 114, Iss 114, Pp 1-10 (1992)
Bu makalede tanımlanan pirit oluşumları, Attepe demir yatağının (Mansurlu-Feke) doğu bitişiğinde yüzeyleyen infrakambriyen yaşlı birimlerin tabanında yer alırlar. Sözkonusu piritler, iki ayrı mineral parajenezi sunarlar. Bunlardan ilk
Externí odkaz:
https://doaj.org/article/97380787f55f4b41b2e7127704bb92ef
Autor:
Münür Burhan SADIKLAR, G.C. AMSTUTZ
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 95, Iss 95, Pp 1-11 (1981)
Gazipaşa (Antalya) yöresinde Kıcık, Endişegüney ve Seyfe mıntıkasında bulunan tabakaya bağlı barit - galen zuhurlarının yankayaç ilişkileri ve kökenlerim açıklama denemesi, bu çalışmanın konusunu oluşturmaktadır. Cevher minera
Externí odkaz:
https://doaj.org/article/04ae1f155e0c4333b514c86753030e9e
Autor:
G.C. Amstutz
The idea for the present Spilite Volume was born during the Spilite Symposium at the XXIIIrd session of the International Geological Con gress in Prague, 1968. At that time, only a restricted number of petro logists working on spilites was presen
Autor:
G.C. Amstutz, A.J. Bernard
In 1963 the first Symposium on'Ores in Sediments'took place as part of an Inter national Sedimentological Congress. At the end of that first Symposium. the group then assembled adopted a resolution printed in the book which resulted from it (AM S
Autor:
J. Pebler, H. Kuhlmann, D. Klein, M. Drabek, T. Lind, S. Takeno, I. Burkart-Baumann, G.C. Amstutz, Günter H. Moh, G. Amthauer, P. Ramdohr, G. Kullerud, D. Hanus, R. Sobott, N. Wang, H.-J. Bernhardt
Publikováno v:
Neues Jahrbuch für Mineralogie - Abhandlungen. 144:291-342
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c471d6400eb1c4c5f4e9014b026d0e9
https://doi.org/10.1127/njma/144/1982/291
https://doi.org/10.1127/njma/144/1982/291
Publikováno v:
Geochimica et Cosmochimica Acta. 49:1553-1560
Amphibolite-grade metasediments from the Mgama Hills region, Kenya, contain conspicuous quantities of graphite, most probably derived from organic progenitor materials. The highest graphite contents (5.1–20.4%) are found in schists whereas calcite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f51c5423d5f6df5658f425ed84855f17
https://doi.org/10.1016/0016-7037(85)90260-1
https://doi.org/10.1016/0016-7037(85)90260-1
Autor:
G.C. Amstutz
Publikováno v:
Geochimica et Cosmochimica Acta. 3:157-168
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61f2e876eb077457b43eb8430d95958f
https://doi.org/10.1016/0016-7037(53)90006-4
https://doi.org/10.1016/0016-7037(53)90006-4
Publikováno v:
Mineralium Deposita. 12
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da8e4223796ec66ca6e2943a71227f54
https://doi.org/10.1007/bf00204511
https://doi.org/10.1007/bf00204511
Publikováno v:
Mineralium Deposita. 14
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aba87fb32ce56f4d692a900f25ec078d
https://doi.org/10.1007/bf00202940
https://doi.org/10.1007/bf00202940