The well-known southwest-to-northeast younging of stratigraphy over a present-day cross
strike distance of> 1500 km in the southern Tasmanides of eastern Australia has been used …

A robust geochronology based on U–Pb zircon ages in Australia (n= 158) and Europe (n=
376) provides a rigorous test of (1) the model of a climatic–tectonic cycle of a single …

The Quaternary beach sand of SE Australia, driven northward by southern swell, contains
zircons with dominant U–Pb ages of 700–500 Ma, model ages (T DMc) of 2.2 Ga to 1.0 Ga …

Abstract The Permo-Triassic granites of the New England Orogen, eastern Australia, were
emplaced into a volcanic arc complex accreted to the eastern Gondwana margin in the Late …

Zircon Hf isotopic data from six granite supersuites recognised in the New England Batholith
of eastern Australia indicate that magma mixing is present in all plutons. Apart from the S …

Most of the New England Orogen comprises a convergent margin, in which Middle
Devonian to latest Carboniferous continental margin arcs, forearc basin and subduction …

The map-view structure of the southern New England Orogen in the eastern Gondwanan
margin is characterised by four tight orogenic-scale curvatures: Texas, Coffs-Harbour …

Detrital zircon from the Carboniferous Girrakool Beds in the central Tablelands Complex of
the southern New England Orogen, Australia, is dominated by ca 350–320 Ma grains with a …

High-resolution airborne geophysical surveys of portions of the New England region of New
South Wales, performed as part of the Exploration NSW initiative, have provided a wealth of …

The main New England Batholith (NEB) extends from Barrington Tops, 120 km SSE of
Tamworth, to southern Queensland and consists of granite plutons (with associated …