1. Introduction. II. Previous literature. III.The stratigraphical succession in Tasmania. IV. The lithological characters of the Pre-Cambrian rocks. (a) Schists of aqueous origin. (b) Schists of igneous origin. V. The structural features of the Pre-Cambrian. Vl. The genesis, history, and present physiographical features of the Pre-Cambrian in Tasmania. VII. The distribution of the Pre-Cambrian in Tasmania. VIII. Nomenclature and correlation. APPENDIX: Notes in explanation of the plates. Table of the Pre-Cambrian succession in North America. PLATES: I. Map of Tasmania, showing the distribution of the Pre- Cambrian. II. Generalised sections
EXECUTIVE SUMMARY The principal aim of this project was to test the models of the Cambrian fault ...
A well-exposed middle Late Cambrian to Early Ordovician clastic sequence, herein referred to as the ...
In the Huskisson River area of western Tasmania the strat-igraphically important early Upper Cambria...
Tasmania, a small geological outlier of Eastern Australia, offers a highly interesting field to the...
At least 30 small bodies of dolerite have been found intruding sediments of the Pre-Cambrian Rocky C...
The Mt. Mary area (S. lat. 42° 12', long. 145°50') is underlain almost entirely by rocks of Pre-Cam...
An important Late Middle Cambrian fossil locality occurs 2 km west of St. Valentines Peak in north-w...
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...
The Denison Range Basin is one of several small basins along the Adamsfield Trough, a Cambrian euge...
In the Black Bluff region of Northwestern Tasmania, Cambrian sedimentary and volcanic rocks are dis...
Rocks of the Parmeener Super-group (Late Carboniferous to Late Triassic) of Tasmania rest with angu...
Interpretation of gravity and magnetic data in southeastern Tasmania indicates that blanketing post-...
A conformable succession in Palaeozoic rocks occurs at the Davey River at the southern end of the O...
The Precambrian quartzites and schists of the Davey River area are characterised by subvertical fol...
EXECUTIVE SUMMARY The principal aim of this project was to test the models of the Cambrian fault ...
A well-exposed middle Late Cambrian to Early Ordovician clastic sequence, herein referred to as the ...
In the Huskisson River area of western Tasmania the strat-igraphically important early Upper Cambria...
Tasmania, a small geological outlier of Eastern Australia, offers a highly interesting field to the...
At least 30 small bodies of dolerite have been found intruding sediments of the Pre-Cambrian Rocky C...
The Mt. Mary area (S. lat. 42° 12', long. 145°50') is underlain almost entirely by rocks of Pre-Cam...
An important Late Middle Cambrian fossil locality occurs 2 km west of St. Valentines Peak in north-w...
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...
The Denison Range Basin is one of several small basins along the Adamsfield Trough, a Cambrian euge...
In the Black Bluff region of Northwestern Tasmania, Cambrian sedimentary and volcanic rocks are dis...
Rocks of the Parmeener Super-group (Late Carboniferous to Late Triassic) of Tasmania rest with angu...
Interpretation of gravity and magnetic data in southeastern Tasmania indicates that blanketing post-...
A conformable succession in Palaeozoic rocks occurs at the Davey River at the southern end of the O...
The Precambrian quartzites and schists of the Davey River area are characterised by subvertical fol...
EXECUTIVE SUMMARY The principal aim of this project was to test the models of the Cambrian fault ...
A well-exposed middle Late Cambrian to Early Ordovician clastic sequence, herein referred to as the ...
In the Huskisson River area of western Tasmania the strat-igraphically important early Upper Cambria...