TY - JOUR
T1 - Alteration of detrital Fe-Ti oxides in sedimentary rocks.
AU - Morad, S.
AU - Aldahan, A. A.
PY - 1986/1/1
Y1 - 1986/1/1
N2 - 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
AB - 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
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U2 - 10.1130/0016-7606(1986)97<567:AODFOI>2.0.CO;2
DO - 10.1130/0016-7606(1986)97<567:AODFOI>2.0.CO;2
M3 - Article
AN - SCOPUS:0022822996
SN - 0016-7606
VL - 97
SP - 567
EP - 578
JO - Geological Society of America Bulletin
JF - Geological Society of America Bulletin
IS - 5
ER -