Zobrazeno 1 - 10
of 21
pro vyhledávání: '"B. J. Franklin"'
Publikováno v:
Australian Journal of Earth Sciences. 61:351-362
This paper deals with the scientific assessment of the physical properties of sandstone used in the conservation of Sydney's historic heritage sandstone buildings. The local Hawkesbury Sandstone has been widely used for all manner of constructions si
Publikováno v:
Behavioural Pharmacology. 14:517-523
We have shown previously that 15 mg/kg pentobarbital induces a conditioned place preference (CPP), but it is unsuitable for intracranial administration. Since the long-acting barbiturate, sodium barbital, is soluble at a neutral pH, we tested whether
Autor:
Jana Podhorna, Keith B. J. Franklin
Publikováno v:
Behavioral Neuroscience. 113:550-557
Autor:
Mary C. Olmstead, Keith B. J. Franklin
Publikováno v:
Behavioral Neuroscience. 111:1324-1334
Autor:
Mary C. Olmstead, Keith B. J. Franklin
Publikováno v:
Behavioral Neuroscience. 111:1313-1323
Publikováno v:
Journal of Geophysical Research: Planets. 101:26119-26130
Two independent methods, with no common assumptions, have been used to estimate the extension across the heavily deformed Tempe Terra province of the Tharsis region of Mars. One method uses measurements of normal fault scarp width with average scarp
Publikováno v:
Mineralogy and Petrology. 57:129-150
Many small podiform chromitite deposits occur within two alpine-type serpentinite belts (of uncertain age) in southern NSW. Most of these deposits are enclosed in massive serpentinised chromite-rich dunite which cross-cuts primary layering within the
Remobilization of PGE in podiform chromitite in the Coolac Serpentinite Belt, Southeastern Australia
Publikováno v:
Australian Journal of Earth Sciences. 39:365-371
The Coolac Serpentinite Belt (CSB) is a subvertical, alpine‐type ultramafic body within the Palaeozoic Lachlan Fold Belt of eastern Australia. Platinum‐group elements (PGE) exist in two podiform chromitite bodies within the CSB. Brecciated chromi
Publikováno v:
Australian Journal of Earth Sciences. 39:127-140
The Mooney Mooney Fault System and Coolac ophiolite suite separate the Tumut Synclinorial Zone and Young Anticlinorial Zone in southeastern Australia. The Tumut Synclinorial Zone has been interpreted as an inverted rift basin and the Coolac ophiolite
Publikováno v:
Geology. 24:1111
New SHRIMP ion microprobe data provide constraints on the age of formation of ophiolitic rocks from the Tumut region of the Lachlan fold belt, southeastern Australia. Magmatic zircons from plagiogranites within both the Coolac serpentinite belt and W