Evolution of a post-batholith dike swarm in central coastal Queensland, Australia: arc-front to backarc?

A swarm of felsic and mafic dikes cuts a Late Carboniferous-Permian batholith called the Urannah Suite in central coastal Queensland. Late Permian-Triassic westward thrusting (Hunter-Bowen Orogeny) exposed this mid-crustal Suite and the crosscutting dikes, thus enabling examination of dikes that range in age from syn- to post-batholithic. Although both mafic and felsic dikes have the same dominant northerly strike, field, geochronologic and geochemical examination reveal that the swarm is composite; felsic dikes are older (285 Ma) and geochemically and isotopically distinct from mafic dikes (similar to 273-229 Ma). Dike compositions are compared to those of the host plutonic rocks, and to volcanic rocks the same age as the dikes, Whereas the felsic (older) dikes are compositionally similar to their host granites (initial (87)Sr/(86)Sr > 0.7045), the mafic (younger) dikes are isotopically (Sr, Nd, Pb) less radiogenic. Moreover, several different types of mafic dikes are evident based on geochemistry; most of these have mixed characteristics in terms of tectonic classification. All but two dikes of basalt and basaltic andesite composition classify as 'with-in plate' on Ti-Zr-Y tectonic classification plots. Many of the basalts have high TiO(2) contents (1.5-3.0 wt.%). Most of these have REE and spider diagram patterns like calc-alkaline tholeiites, the exceptions being a few all;ali basalts recognized by their alkali content, and high Ti, Ce, Nh and Zr contents. When put into the context of all plutonic rocks in the area (late Paleozoic and Mesozoic), these dikes record a transition at similar to 280 Ma, after which time, all magnatism in the region is less isotopically evolved (initial (87)Sr/(86)Sr = 0.7033-0.7044). A model of slab retreat and hinge movement to the east in the latest Permian explains the change of geochemical signature from are-front to backare at about 280 Ma. (C) 2000 Elsevier Science B.V. All rights reserved.