The northern part of the Tasman Fold Belt System in Queensland comprises three segments,
the Thomson, Hodgkinson-Broken River, and New England Fold Belts. The evolution of …

The New England Fold Belt forms the easternmost, youngest part of the Tasman Fold Belt
System. For much of Late Palaeozoic time, it was a convergent plate margin at the edge of …

Potential asbestos-bearing rocks account for about 0.2% of the land area of eastern
Australia. The main mode of occurrence is as narrow cross fibre and slip fibre veins of …

The eastern part of the Tasman Orogenic Zone (or Fold Belt System) comprises the
Hodgkinson—Broken River Orogen (or Fold Belt) in the north and the New England Orogen …

Isotopic dating of igneous rocks in eastern Queensland south of Bowen has indicated
phases of granite emplacement in the Devonian (360 my), Carboniferous (310 and 285 my) …

In easternmost Australia, the New England Orogen contains a geological record dominated
by subduction-related rocks, with plate convergence during the Late Devonian to Triassic …

Summary The New England Orogen in eastern Australia consists essentially of two pre‐
Permian terranes which form a subduction‐related forearc basin‐accretionary wedge …

K-Ar and Rb-Sr ages were measured on rapidly cooled igneous rocks from Kinnekulle,
Sweden (Ordovician bentonite), the Cerberean Cauldron, Australia (late Devonian felsic …

Regional cross sections of the northern New England Orogen and eastern Bowen Basin in
eastern Queensland indicate that the climactic Permian‐Triassic deformation involved thin …

New late Cainozoic faunal assemblages are preliminarily identified and described from
central eastern Queensland. Biocorrelation of the sites has determined that the oldest faunal …