Nontronite in a deep-sea core from the South Pacific.

A. Singer; P. Stoffers; L. Heller-Kallai; D. Szafranek

doi:10.1346/CCMN.1984.0320505

Nontronite in a deep-sea core from the South Pacific.

A. Singer
, P. Stoffers
, L. Heller-Kallai
, D. Szafranek

Fredy & Nadine Herrmann Institute of Earth Sciences

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

51 Scopus citations

Abstract

Clay material recovered during the 1980 cruise SO-14 RV of 'Sonne' in the SW Pacific basin from core KL9 at 4250 m depth on a small sediment contains some layers of nearly pure nontronite which have only trace levels of Al. The b-axis spacing is 9.09 A and the mineral consists of sheaves of fibres <50 A wide, with an unusually low dehydroxylation T of 454oC. Definitive dating of the mineral was not possible but it probably formed at least 12 m.y. ago. -D.F.B.

Original language	English
Pages (from-to)	375-383
Number of pages	9
Journal	Clays and Clay Minerals
Volume	32
Issue number	5
DOIs	https://doi.org/10.1346/CCMN.1984.0320505
State	Published - 1984

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title = "Nontronite in a deep-sea core from the South Pacific.",

abstract = "Clay material recovered during the 1980 cruise SO-14 RV of 'Sonne' in the SW Pacific basin from core KL9 at 4250 m depth on a small sediment contains some layers of nearly pure nontronite which have only trace levels of Al. The b-axis spacing is 9.09 A and the mineral consists of sheaves of fibres <50 A wide, with an unusually low dehydroxylation T of 454oC. Definitive dating of the mineral was not possible but it probably formed at least 12 m.y. ago. -D.F.B.",

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AU - Singer, A.

AU - Stoffers, P.

AU - Heller-Kallai, L.

AU - Szafranek, D.

PY - 1984

Y1 - 1984

N2 - Clay material recovered during the 1980 cruise SO-14 RV of 'Sonne' in the SW Pacific basin from core KL9 at 4250 m depth on a small sediment contains some layers of nearly pure nontronite which have only trace levels of Al. The b-axis spacing is 9.09 A and the mineral consists of sheaves of fibres <50 A wide, with an unusually low dehydroxylation T of 454oC. Definitive dating of the mineral was not possible but it probably formed at least 12 m.y. ago. -D.F.B.

AB - Clay material recovered during the 1980 cruise SO-14 RV of 'Sonne' in the SW Pacific basin from core KL9 at 4250 m depth on a small sediment contains some layers of nearly pure nontronite which have only trace levels of Al. The b-axis spacing is 9.09 A and the mineral consists of sheaves of fibres <50 A wide, with an unusually low dehydroxylation T of 454oC. Definitive dating of the mineral was not possible but it probably formed at least 12 m.y. ago. -D.F.B.

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ER -

Nontronite in a deep-sea core from the South Pacific.

Abstract

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