Note on glauconitic sandstones in the Wairarapa, New Zealand
- 1 February 1965
- journal article
- research article
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 8 (1) , 81-84
- https://doi.org/10.1080/00288306.1965.10422132
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.Keywords
This publication has 4 references indexed in Scilit:
- Marl Diapirism Near Gisborne, New ZealandNew Zealand Journal of Geology and Geophysics, 1962
- Sedimentary structures and palaeocurrent directions from the Silurian rocks of KirkcudbrightTransactions of the Edinburgh Geological Society, 1962
- The geology of the flat point area, eastern WairarapaNew Zealand Journal of Geology and Geophysics, 1960
- TURBIDITES IN FLYSCH OF THE POLISH CARPATHIAN MOUNTAINSGSA Bulletin, 1959