TY - JOUR
T1 - Alteration of detrital Fe-Ti oxides in sedimentary rocks.
AU - Morad, S.
AU - Aldahan, A. A.
PY - 1986
Y1 - 1986
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
UR - http://www.scopus.com/inward/record.url?scp=0022822996&partnerID=8YFLogxK
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 - Bulletin of the Geological Society of America
JF - Bulletin of the Geological Society of America
IS - 5
ER -