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pro vyhledávání: '"Mansoore Maghsoudloo Mahalli"'
Publikováno v:
Journal of Economic Geology, Vol 8, Iss 1, Pp 39-59 (2016)
Introduction Oolitic iron formations are sedimentary rocks with >5 vol.% oolites and >15 wt.% iron, corresponding to 21.4 wt.% Fe2O3 (Young, 1989; Petranek and Van Houten, 1997; Mucke and Farshad, 2005). In Iran, new iron oolite-bearing members have
Externí odkaz:
https://doaj.org/article/06ed184f3f64454cbac120d4349d66e0
