Factors controlling the genesis of FeMn
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R. Jiménez-Espinosa; J. Jiménez-Milĺan; L. Nieto
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Article
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1997
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Elsevier Science
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English
⚖ 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