Origin and geochemistry of Cretaceous deep-sea black shales and multi-colored claystones, with emphasis on Deep Sea Drilling Project site 530, Southern Angola Basin.

W. E. Dean; M. A. Arthur; D. A.V. Stow

Origin and geochemistry of Cretaceous deep-sea black shales and multi-colored claystones, with emphasis on Deep Sea Drilling Project site 530, Southern Angola Basin.

W. E. Dean
, M. A. Arthur
, D. A.V. Stow

Geosciences

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

35 Scopus citations

Abstract

The deposits are rich in organic carbon and occur in cycles of sedimentation that range from 10420 000-100 000 years but average 09640 000-50 000 years. The organic carbon-rich lithologies are commonly enriched in Cr, Ni, V, Cu, Zn and Mo. The slowly deposited oxidized shales are enriched in Fe, Mn, Zn and Cu.-K.A.R.

Original language	English (US)
Pages (from-to)	819-844
Number of pages	26
Journal	Initial Reports of the D.S.D.P.
Volume	75
Issue number	2
State	Published - 1984

All Science Journal Classification (ASJC) codes

General Environmental Science
General Earth and Planetary Sciences

Cite this

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title = "Origin and geochemistry of Cretaceous deep-sea black shales and multi-colored claystones, with emphasis on Deep Sea Drilling Project site 530, Southern Angola Basin.",

abstract = "The deposits are rich in organic carbon and occur in cycles of sedimentation that range from 10420 000-100 000 years but average 09640 000-50 000 years. The organic carbon-rich lithologies are commonly enriched in Cr, Ni, V, Cu, Zn and Mo. The slowly deposited oxidized shales are enriched in Fe, Mn, Zn and Cu.-K.A.R.",

author = "Dean, \{W. E.\} and Arthur, \{M. A.\} and Stow, \{D. A.V.\}",

year = "1984",

language = "English (US)",

volume = "75",

pages = "819--844",

journal = "Initial Reports of the D.S.D.P.",

number = "2",

}

TY - JOUR

T1 - Origin and geochemistry of Cretaceous deep-sea black shales and multi-colored claystones, with emphasis on Deep Sea Drilling Project site 530, Southern Angola Basin.

AU - Dean, W. E.

AU - Arthur, M. A.

AU - Stow, D. A.V.

PY - 1984

Y1 - 1984

N2 - The deposits are rich in organic carbon and occur in cycles of sedimentation that range from 10420 000-100 000 years but average 09640 000-50 000 years. The organic carbon-rich lithologies are commonly enriched in Cr, Ni, V, Cu, Zn and Mo. The slowly deposited oxidized shales are enriched in Fe, Mn, Zn and Cu.-K.A.R.

AB - The deposits are rich in organic carbon and occur in cycles of sedimentation that range from 10420 000-100 000 years but average 09640 000-50 000 years. The organic carbon-rich lithologies are commonly enriched in Cr, Ni, V, Cu, Zn and Mo. The slowly deposited oxidized shales are enriched in Fe, Mn, Zn and Cu.-K.A.R.

UR - https://www.scopus.com/pages/publications/0021338148

UR - https://www.scopus.com/pages/publications/0021338148#tab=citedBy

M3 - Article

AN - SCOPUS:0021338148

VL - 75

SP - 819

EP - 844

JO - Initial Reports of the D.S.D.P.

JF - Initial Reports of the D.S.D.P.

IS - 2

ER -

Origin and geochemistry of Cretaceous deep-sea black shales and multi-colored claystones, with emphasis on Deep Sea Drilling Project site 530, Southern Angola Basin.

Abstract

All Science Journal Classification (ASJC) codes

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