Alteration of detrital Fe-Ti oxides in sedimentary rocks.

S. Morad, A. A. Aldahan

Research output: Contribution to journalArticlepeer-review

77 Citations (Scopus)


In Proterozoic sandstones, shales, and carbonate rocks of the Visingso Group in southern Sweden, detrital Fe-Ti oxides have undergone alteration by dissolution and/or replacement mainly by titanium oxides, hematite (reddish rocks), or pyrite (greenish sandstones, shales, and carbonate rocks). The alteration of ilmenite occurs through several intermediate phases, each successively enriched in titanium and depleted in iron.-from Authors

Original languageEnglish
Pages (from-to)567-578
Number of pages12
JournalGeological Society of America Bulletin
Issue number5
Publication statusPublished - 1986
Externally publishedYes

ASJC Scopus subject areas

  • Geology


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