Alteration of detrital Fe-Ti oxides in sedimentary rocks.

S. Morad; A. A. Aldahan

doi:10.1130/0016-7606(1986)97<567:AODFOI>2.0.CO;2

Alteration of detrital Fe-Ti oxides in sedimentary rocks.

S. Morad
, A. A. Aldahan

Research output: Contribution to journal › Article › peer-review

86 Citations (Scopus)

Abstract

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 language	English
Pages (from-to)	567-578
Number of pages	12
Journal	Geological Society of America Bulletin
Volume	97
Issue number	5
DOIs	https://doi.org/10.1130/0016-7606(1986)97<567:AODFOI>2.0.CO;2
Publication status	Published - 1986
Externally published	Yes

ASJC Scopus subject areas

Geology

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10.1130/0016-7606(1986)97<567:AODFOI>2.0.CO;2

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abstract = "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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AU - Morad, S.

AU - Aldahan, A. A.

PY - 1986

Y1 - 1986

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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

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JO - Geological Society of America Bulletin

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IS - 5

ER -

Alteration of detrital Fe-Ti oxides in sedimentary rocks.

Abstract

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