Lithology and geochemistry of ODP Leg 198 sites, Shatsky Rise

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Hauptverfasser: Fontilea, Kristin, Marsaglia, Kathleen M, Dean, Norman
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2006
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author Fontilea, Kristin
Marsaglia, Kathleen M
Dean, Norman
author_facet Fontilea, Kristin
Marsaglia, Kathleen M
Dean, Norman
collection Datos científicos de ciencias marinas y ambientales
contents Samples of chert, porcellanite, and chalk/limestone from Cretaceous chert-bearing sections recovered during Leg 198 were studied to elucidate the nature and origin of chert color zonations with depth/age. Sedimentary structures, trace fossils, compactional features, sediment composition, texture, geochemistry, and diagenetic history were compared among lithologies. Trends in major and minor element composition were determined. Whereas geochemical analyses demonstrate systematic elemental differences among the different lithologies, there are less distinct patterns in composition for the colored cherts. The color of the chert appears to be related primarily to the amount of silica and secondarily to the proportion of other components. Red cherts are almost pure silica with only minor impurities. This may allow pigmentation from fine Fe oxides to dominate the color. These red cherts are from places where geophysical logs indicate that chert is the dominant rock type of the section. These red chert intervals cannot be unequivocally distinguished from surrounding chert-bearing lithologies in terms of sedimentary structures.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_778101
institution PANGAEA
language en
publishDate 2006
publisher PANGAEA
record_format pangaea
spellingShingle Lithology and geochemistry of ODP Leg 198 sites, Shatsky Rise
Fontilea, Kristin
Marsaglia, Kathleen M
Dean, Norman
198-1207B; 198-1213A; 198-1213B; 198-1214A; DRILL; Drilling/drill rig; Joides Resolution; Leg198; North Pacific Ocean; Ocean Drilling Program; ODP
Samples of chert, porcellanite, and chalk/limestone from Cretaceous chert-bearing sections recovered during Leg 198 were studied to elucidate the nature and origin of chert color zonations with depth/age. Sedimentary structures, trace fossils, compactional features, sediment composition, texture, geochemistry, and diagenetic history were compared among lithologies. Trends in major and minor element composition were determined. Whereas geochemical analyses demonstrate systematic elemental differences among the different lithologies, there are less distinct patterns in composition for the colored cherts. The color of the chert appears to be related primarily to the amount of silica and secondarily to the proportion of other components. Red cherts are almost pure silica with only minor impurities. This may allow pigmentation from fine Fe oxides to dominate the color. These red cherts are from places where geophysical logs indicate that chert is the dominant rock type of the section. These red chert intervals cannot be unequivocally distinguished from surrounding chert-bearing lithologies in terms of sedimentary structures.
title Lithology and geochemistry of ODP Leg 198 sites, Shatsky Rise
topic 198-1207B; 198-1213A; 198-1213B; 198-1214A; DRILL; Drilling/drill rig; Joides Resolution; Leg198; North Pacific Ocean; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.778101