Microfossils from a newly discovered Precambrian stromatolitic iron formation in Western Australia

M. R. Walter; A. D T Goode; W. D M Hall

doi:10.1038/261221a0

Microfossils from a newly discovered Precambrian stromatolitic iron formation in Western Australia

M. R. Walter^*, A. D T Goode, W. D M Hall

^*Corresponding author for this work

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

73 Citations (Scopus)

Abstract

THE Nabberu Basin is a newly discovered sedimentary basin of probable early Proterozoic age in Western Australia^1-3 (Fig. 1). It covers an area of ∼60,000 km², and contains ∼6,000 m of shallow-water clastic and chemical sediments. It is essentially unmetamorphosed in the south-east but is metamorphosed to granulite facies in the west, where folding and deformation are more pronounced.

Original language	English
Pages (from-to)	221-223
Number of pages	3
Journal	Nature
Volume	261
Issue number	5557
DOIs	https://doi.org/10.1038/261221a0
Publication status	Published - 1976
Externally published	Yes

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title = "Microfossils from a newly discovered Precambrian stromatolitic iron formation in Western Australia",

abstract = "THE Nabberu Basin is a newly discovered sedimentary basin of probable early Proterozoic age in Western Australia1-3 (Fig. 1). It covers an area of ∼60,000 km2, and contains ∼6,000 m of shallow-water clastic and chemical sediments. It is essentially unmetamorphosed in the south-east but is metamorphosed to granulite facies in the west, where folding and deformation are more pronounced.",

author = "Walter, \{M. R.\} and Goode, \{A. D T\} and Hall, \{W. D M\}",

year = "1976",

doi = "10.1038/261221a0",

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pages = "221--223",

journal = "Nature",

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AU - Walter, M. R.

AU - Goode, A. D T

AU - Hall, W. D M

PY - 1976

Y1 - 1976

N2 - THE Nabberu Basin is a newly discovered sedimentary basin of probable early Proterozoic age in Western Australia1-3 (Fig. 1). It covers an area of ∼60,000 km2, and contains ∼6,000 m of shallow-water clastic and chemical sediments. It is essentially unmetamorphosed in the south-east but is metamorphosed to granulite facies in the west, where folding and deformation are more pronounced.

AB - THE Nabberu Basin is a newly discovered sedimentary basin of probable early Proterozoic age in Western Australia1-3 (Fig. 1). It covers an area of ∼60,000 km2, and contains ∼6,000 m of shallow-water clastic and chemical sediments. It is essentially unmetamorphosed in the south-east but is metamorphosed to granulite facies in the west, where folding and deformation are more pronounced.

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U2 - 10.1038/261221a0

DO - 10.1038/261221a0

M3 - Article

AN - SCOPUS:0007941773

SN - 0028-0836

VL - 261

SP - 221

EP - 223

JO - Nature

JF - Nature

IS - 5557

ER -

Microfossils from a newly discovered Precambrian stromatolitic iron formation in Western Australia

Abstract

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