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"Devonian–Carboniferous regional deformation in the northeastern Lachla" by C. L. Fergusson and G. P. Colquhoun


Abstract
The timing of regional deformation of the turbiditic Silurian–Devonian Hill End Trough in the northeastern Lachlan Orogen has been a contentious issue with one view ascribing the regional north–south folds and axial planar foliation to Middle Devonian basin inversion. Alternatively, it has been argued that given the low-angle discordance between Lower and Upper Devonian units on the Capertee and Molong highs, and the development of a dominant episode of folding mapped from the Hill End Trough into the adjoining highs, the major regional deformation is latest Devonian to early Carboniferous and predates intrusion of Bathurst-type granites at 358–314 Ma. We have approached the problem by analysing the gentle, upright, southeast-trending folds and deformation patterns in Devonian units of the northern Capertee High (Cudgegong area), drawing a cross-section across the Hill End Trough and reviewing the structure of two areas in the Molong High (west of Orange, and so ....

New South Wales , New Zealand General , New Zealand , Hill End , Lachlan Orogen , Devonian Hill End Trough , Middle Devonian , Upper Devonian , Hill End Trough , Capertee High , Molong High , Plate Devonian , Animblan Orogeny , Lachlan Orogen , Egional Deformation , புதியது தெற்கு வேல்ஸ் , புதியது ஜீலாந்து ஜநரல் , புதியது ஜீலாந்து , மலை முடிவு , நடுத்தர டெவோனியன் , மேல் டெவோனியன் , மலை முடிவு தொட்டி , தாமதமாக டெவோனியன் ,