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Fe-Mn crusts from underwater rises of the Kashevarov Trough (Sea of Okhotsk)

โœ Scribed by P. E. Mikhailik; A. N. Derkachev; O. V. Chudaev; N. V. Zarubina


Book ID
111470814
Publisher
Pleiades Publishing
Year
2009
Tongue
English
Weight
633 KB
Volume
3
Category
Article
ISSN
1819-7140

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Factors controlling the genesis of Fe๎—ธMn
โœ R. Jimรฉnez-Espinosa; J. Jimรฉnez-Milฤบan; L. Nieto ๐Ÿ“‚ Article ๐Ÿ“… 1997 ๐Ÿ› Elsevier Science ๐ŸŒ English โš– 759 KB

Fe-Mn crusts occur in four stratigraphic breaks of Jurassic pelagic swell sequences in the eastern Betic Cordillera. Crusts were characterized by quantitative and qualitative variables deduced from their stratigraphic position (under-and overlying lithologies), texture (thin or banded), mineralogica