Zobrazeno 1 - 10
of 627
pro vyhledávání: '"Marchig, V"'
Publikováno v:
Current Science, 1996 Apr . 70(8), 724-729.
Externí odkaz:
https://www.jstor.org/stable/24097587
Autor:
Wiedicke, M., Sahling, H., Delisle, G., Faber, E., Neben, S., Beiersdorf, H., Marchig, V., Weiss, W., von Mirbach, N., Afiat, A.
Publikováno v:
In Marine Geology 2002 184(1):121-141
Publikováno v:
In Chemical Geology 2002 185(1):125-147
Publikováno v:
In Marine Geology 2000 163(1):169-184
Publikováno v:
In Marine Geology 2000 162(2):479-500
Publikováno v:
In Marine Geology 1999 159(1):179-203
Autor:
SREMAC, JASENKA1 jsremac@geol.pmf.hr, VELIĆ, JOSIPA2 josipa.velic@rgn.unizg.hr, BOŠNJAK, MARIJA3 marija.bosnjak@hpm.hr, VELIĆ, IVO4 ivo.velic@zg.t-com.hr, BAKRAČ, KORALJKA5 kbakrac@hgi-cgs.hr, ŠIMIČEVIĆ, ANA6 anasimicevic@yahoo.com, MALVIĆ, TOMISLAV2 tomislav.malvic@rgn.unizg.hr, FOTOVIĆ, DANIEL7 daniel.fotovic@igm-sljuncara.hr
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia. Nov2024, Vol. 130 Issue 3, p613-631. 19p.
Autor:
Ayupova, Nuriya R.1 (AUTHOR) aupova@mineralogy.ru, Maslennikov, Valery V.1 (AUTHOR), Melekestseva, Irina Yu.1 (AUTHOR), Artemyev, Dmitry A.1 (AUTHOR), Belogub, Elena V.1 (AUTHOR)
Publikováno v:
Minerals (2075-163X). Sep2024, Vol. 14 Issue 9, p939. 21p.
Publikováno v:
Marine geology
236 (2007): 121–141.
info:cnr-pdr/source/autori:Dekov V.M. (a), Kamenov G.D. (b), Savelli C. (c), Stummeyer J. (d), Marchig V. (d)/titolo:Origin of basal dolomitic claystone in the Marsili Basin, Tyrrhenian Sea/doi:/rivista:Marine geology (Print)/anno:2007/pagina_da:121/pagina_a:141/intervallo_pagine:121–141/volume:236
236 (2007): 121–141.
info:cnr-pdr/source/autori:Dekov V.M. (a), Kamenov G.D. (b), Savelli C. (c), Stummeyer J. (d), Marchig V. (d)/titolo:Origin of basal dolomitic claystone in the Marsili Basin, Tyrrhenian Sea/doi:/rivista:Marine geology (Print)/anno:2007/pagina_da:121/pagina_a:141/intervallo_pagine:121–141/volume:236
Red-brown dolomitic claystones overlay the Marsili Basin basaltic basement at ODP Site 650. Sequential leaching experiments reveal that most of the elements considered to have a hydrothermal or hydrogenous origin in a marine environment, such as Fe,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::ac2c8198f6fcf265b6d317b8efc07046
http://www.cnr.it/prodotto/i/49268
http://www.cnr.it/prodotto/i/49268
Publikováno v:
Scopus-Elsevier
The Middle Jurassic (uppermost Bajocian-lower Bathonian to upper Bathonian-lower Callovian) radiolarian cherts in the Medvednica Mt (NW Croatia) have a high content of SiO2 (average 90.87 %). Most of the silica is of biogenic origin as is indicated b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::17d3665e95f612497f6d124fa6bd1b20
https://www.bib.irb.hr/195622
https://www.bib.irb.hr/195622