-
RB 60/00022 Palynological observations on Eocene sediments from two bores in the northern Adelaide Plains.
Microfloras from Eocene marine and non-marine sediments, intersected in two deep bores in the Adelaide Plains Basin, can be placed within two distinct assemblage units. The correlative value of these as time-stratigraphic units is discussed.-
Document
Published: 03 Feb 1965
-
RB 60/00051 Stratigraphy and micropalaeontology of three deep bores, Hd Port Gawler.
Three relatively deep bores, drilled recently on the northern Adelaide Plains in the Hundred of Port Gawler, about 20 miles north of Adelaide, have intersected useful complementary sections of the Cainozoic succession, ranging from 560 feet to 1148...-
Document
Published: 15 Mar 1965
-
RB 87/00057 Middle Eocene age of the megafossil flora at Golden Grove, South Australia - A preliminary report, and comparison with the Maslin Bay flora.
Presents results from 2 samples from a clay lens in a Monier Golden Grove sand pit. 2 other samples from the leaf bearing beds at Maslin Bay were examined to determine if the fossils from the 2 sites are of similar age and if the host sediments are...-
Document
Published: 01 Mar 1987
-
RB 89/00054 Preliminary palynological dating of North Maslin Sand at One Tree Hill.
Fifteen grab and drill core samples were assigned an uppermost Middle Eocene or lowermost Late Eocene age (correlated with North Maslin Sand) from a fluvial channel and flood plain backswamp sedimentary environment.-
Document
Published: 01 Jul 1989
-
RB 91/00075 Tertiary occurrence of the fern Lygodium (Schizaeaceae) in Australia and New Zealand.
Fossil Lygodium leaves including sterile and fertile pinnules of the climbing fern are described from Dinmore (Queensland), Maslin Bay and Golden Grove (South Australia), Anglesea (Victoria) and other localities in southern Australia and New Zealand....-
Document
Published: 01 Jul 1991
-
RB 91/00053 Middle Eocene palynofloras from the One Tree Hill area, St. Vincent Basin, South Australia.
Palynofloras from an outlier of North Maslin Sands are Middle Eocene in age. The palynofloras are non-marine and correlate with the Lower Nothofagidites asperus Zone of the Gippsland Basin and the 'Proteacidites pachypolus' Zone of south-central...-
Document
Published: 01 May 1991
-
RB 69/00114 Early Middle Eocene age of the Maslin Bay flora, South Australia.
There is no abstract created for this record-
Document
Published: 01 Jan 1969
-
RB 74/00031 Biostratigraphy of two boreholes near the northern margin of the Willunga Sub-basin.
Boreholes B2/73, B3/73 intersected (i) thin Quarternary units over ?Plio-Pleistocene Carisbrooke Sand, uncomformably overlying (without intervening Port Willunga Beds) (ii) an Eocene succession (correlated with the lower part of Reynolds' standard...-
Document
Published: 01 Jan 1974
