Note on glauconitic sandstones in the Wairarapa, New Zealand

B. D. Webby; H. B. Van Den Heuvel

doi:10.1080/00288306.1965.10422132

Note on glauconitic sandstones in the Wairarapa, New Zealand

B. D. Webby
, H. B. Van Den Heuvel

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

2 Citations (Scopus)

Abstract

Cretaceous-Tertiary glauconitic sandstones near Flat Point, showing moderate to poor graded bedding, lamination, cross lamination, and flute marks, are tentatively considered to be turbidity-current deposits.These rocks contain an abundance of worm burrowings and tracks.

Original language	English
Pages (from-to)	81-84
Number of pages	4
Journal	New Zealand Journal of Geology and Geophysics
Volume	8
Issue number	1
DOIs	https://doi.org/10.1080/00288306.1965.10422132
Publication status	Published - 1965
Externally published	Yes

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10.1080/00288306.1965.10422132

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title = "Note on glauconitic sandstones in the Wairarapa, New Zealand",

abstract = "Cretaceous-Tertiary glauconitic sandstones near Flat Point, showing moderate to poor graded bedding, lamination, cross lamination, and flute marks, are tentatively considered to be turbidity-current deposits.These rocks contain an abundance of worm burrowings and tracks.",

author = "Webby, \{B. D.\} and \{Van Den Heuvel\}, \{H. B.\}",

year = "1965",

doi = "10.1080/00288306.1965.10422132",

language = "English",

volume = "8",

pages = "81--84",

journal = "New Zealand Journal of Geology and Geophysics",

issn = "0028-8306",

publisher = "John Wiley \& Sons",

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TY - JOUR

T1 - Note on glauconitic sandstones in the Wairarapa, New Zealand

AU - Webby, B. D.

AU - Van Den Heuvel, H. B.

PY - 1965

Y1 - 1965

N2 - Cretaceous-Tertiary glauconitic sandstones near Flat Point, showing moderate to poor graded bedding, lamination, cross lamination, and flute marks, are tentatively considered to be turbidity-current deposits.These rocks contain an abundance of worm burrowings and tracks.

AB - Cretaceous-Tertiary glauconitic sandstones near Flat Point, showing moderate to poor graded bedding, lamination, cross lamination, and flute marks, are tentatively considered to be turbidity-current deposits.These rocks contain an abundance of worm burrowings and tracks.

UR - https://www.scopus.com/pages/publications/84943292616

U2 - 10.1080/00288306.1965.10422132

DO - 10.1080/00288306.1965.10422132

M3 - Article

AN - SCOPUS:84943292616

SN - 0028-8306

VL - 8

SP - 81

EP - 84

JO - New Zealand Journal of Geology and Geophysics

JF - New Zealand Journal of Geology and Geophysics

IS - 1

ER -

Note on glauconitic sandstones in the Wairarapa, New Zealand

Abstract

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