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Volumn 160, Issue 1, 1983, Pages 49-66
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Tidal deposits in the early Proterozoic basin of the Lake Superior region-the Palms and the Pokegama formations: Evidence for subtidal-shelf deposition of Superior-type banded iron-formation
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Author keywords
[No Author keywords available]
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Indexed keywords
CORE DRILLING;
DEPOSITS;
ECONOMIC GEOLOGY;
LAKES;
METAMORPHIC ROCKS;
SANDSTONE;
SEDIMENTOLOGY;
SILICATES;
TEXTURES;
TIDAL POWER;
TIDES;
WETLANDS;
ARGILLACEOUS ROCKS;
BANDED IRON FORMATIONS;
ENERGY CONDITION;
LAW OF SUCCESSION;
SEDIMENTARY SEQUENCE;
SEDIMENTARY STRUCTURE;
SEDIMENTARY UNITS;
TIDAL CONDITIONS;
IRON DEPOSITS;
ARGILLACEOUS DEPOSIT;
BANDED IRON FORMATION;
CORE ANALYSIS;
DEPOSITIONAL SEQUENCE;
HIGH ENERGY ENVIRONMENT;
LAMINATION;
LITHOLOGY;
PROTEROZOIC;
SHALE;
SUBTIDAL ENVIRONMENT;
TIDAL CHANNEL;
UNCONFORMITY;
GREAT LAKES [NORTH AMERICA];
LAKE SUPERIOR;
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EID: 4544249605
PISSN: 00721069
EISSN: None
Source Type: Book Series
DOI: 10.1130/MEM160-p49 Document Type: Conference Paper |
Times cited : (35)
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References (0)
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