Late Palaeozoic and Early Mesozoic rocks of the Parmeener Super-Group are subdivided on a strict lithostratigraphical basis, and not in the time terms 'Permian' and 'Triassic'
The end-Permian was marked by multiple environmental perturbations that ultimately resulted in the g...
The upper Paleozoic–lower Mesozoic strata in the northeastern Galilee Basin are important for their ...
A conformable succession in Palaeozoic rocks occurs at the Davey River at the southern end of the O...
In Tasmania, the lower (Permo-Carboniferous) rocks of the Parmeener Supergroup are almost everywher...
The Cygnet Coal Measures is a unit of carbonaceous shale, coal and feldspathic sandstone in Tasman...
Rocks of the Parmeener Super-group (Late Carboniferous to Late Triassic) of Tasmania rest with angu...
Rocks of the Parmeener Super-group (Late Carboniferous to Late Triassic) of Tasmania rest with angu...
A section 236.8 m in thickness of Late Palaeozoic (Late Carboniferous-Permian) rocks of the Lower Pa...
Rocks of the Parmeener Super-group (Late Carboniferous to Late Triassic) of Tasmania rest with angu...
The two systems for the purposes of this paper are grouped as one under the term Carboniferous sys...
An unbroken succession of Permian sediments about 1430 feet thick on the northern flanks of Mt. Na...
Recent research in eastern Australia has established that rather than being a single, long-lived epo...
In south-eastern Tasmania the Ferntree Group, which · is the thickest and most persistent of all Tas...
Recent research in eastern Australia has established that rather than being a single, long-lived epo...
The end-Permian was marked by multiple environmental perturbations that ultimately resulted in the g...
The end-Permian was marked by multiple environmental perturbations that ultimately resulted in the g...
The upper Paleozoic–lower Mesozoic strata in the northeastern Galilee Basin are important for their ...
A conformable succession in Palaeozoic rocks occurs at the Davey River at the southern end of the O...
In Tasmania, the lower (Permo-Carboniferous) rocks of the Parmeener Supergroup are almost everywher...
The Cygnet Coal Measures is a unit of carbonaceous shale, coal and feldspathic sandstone in Tasman...
Rocks of the Parmeener Super-group (Late Carboniferous to Late Triassic) of Tasmania rest with angu...
Rocks of the Parmeener Super-group (Late Carboniferous to Late Triassic) of Tasmania rest with angu...
A section 236.8 m in thickness of Late Palaeozoic (Late Carboniferous-Permian) rocks of the Lower Pa...
Rocks of the Parmeener Super-group (Late Carboniferous to Late Triassic) of Tasmania rest with angu...
The two systems for the purposes of this paper are grouped as one under the term Carboniferous sys...
An unbroken succession of Permian sediments about 1430 feet thick on the northern flanks of Mt. Na...
Recent research in eastern Australia has established that rather than being a single, long-lived epo...
In south-eastern Tasmania the Ferntree Group, which · is the thickest and most persistent of all Tas...
Recent research in eastern Australia has established that rather than being a single, long-lived epo...
The end-Permian was marked by multiple environmental perturbations that ultimately resulted in the g...
The end-Permian was marked by multiple environmental perturbations that ultimately resulted in the g...
The upper Paleozoic–lower Mesozoic strata in the northeastern Galilee Basin are important for their ...
A conformable succession in Palaeozoic rocks occurs at the Davey River at the southern end of the O...
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