The Whitsunday Volcanic Province, Central Queensland, Australia: lithological and stratigraphic investigations of a silicic-dominated large igneous province

• Published in: Journal of Volcanology and Geothermal Research
• Main Authors: Bryan, S. E., Ewart, A., Stephens, C. J., Parianos, J., Downes, P. J.
• Other Authors: Professor Yoshiaki Ida
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier Science 2000
• Subjects: Geosciences; Multidisciplinary; Early Cretaceous; Large Igneous Province; Eastern Australia; Ignimbrite; Volcanic Evolution; New-zealand; Goboboseb Mountains; Etendeka Volcanism; West Antarctica; Geochronology; Complex; Namibia; Magmatism; Gondwana; Plateau; 260103 Vulcanology; C1; 780104 Earth sciences; New Zealand; Queensland; Antarc*; Antarctica
• Online Access: https://espace.library.uq.edu.au/view/UQ:139302

Contrary to general belief, not all large igneous provinces (LIPs) are characterised by rocks of basaltic composition. Silicic-dominated LIPs, such as the Whitsunday Volcanic Province of NE Australia, are being increasingly recognised in the rock record. These silicic LIPs are consistent in being: (1) volumetrically dominated by ignimbrite; (2) active over prolonged periods (40-50 m.y.), based on available age data; and (3) spatially and temporally associated with plate break-up. This silicic dominated LIP, related to the break-up of eastern continental Gondwana, is also significant for being the source of > 1.4 x 10(6) km(3) of coeval volcanogenic sediment preserved in adjacent sedimentary basins of eastern Australia. The Whitsunday Volcanic Province is volumetrically dominated by medium- to high-grade, dacitic to rhyolitic lithic ignimbrites. Individual ignimbrite units are commonly between 10 and 100 m thick, and the ignimbrite-dominated sequences exceed 1 km in thickness. Coarse lithic lag breccias containing clasts up to 6 m diameter are associated with the ignimbrites in proximal sections. Pyroclastic surge and fallout deposits, subordinate basaltic to rhyolitic lavas, phreatomagmatic deposits, and locally significant thicknesses of coarse-grained volcanogenic conglomerate and sandstone are interbedded with the ignimbrites. The volcanic sequences are intruded by gabbro/dolerite to rhyolite dykes (up to 50 m in width), sills and comagmatic granite. Dyke orientations are primarily from NW to NNE. The volcanic sequences are characterised by the interstratification of proximal/near-vent lithofacies such as rhyolite domes and lavas, and basaltic agglomerate, with medial to distal facies of ignimbrite. The burial of these near-vent lithofacies by ignimbrites, coupled with the paucity of mass wastage products such as debris-flow deposits indicates a low-relief depositional environment. Furthermore, the volcanic succession records a temporal change in: (1) eruptive styles; (2) the nature of source vents; and (3) erupted compositions. An early explosive dacitic pyroclastic phase was succeeded by a later mixed pyroclastic-effusive phase producing an essentially bimodal suite of lavas and rhyolitic ignimbrite. From the nature and distribution of volcanic lithofacies. the volcanic sequences are interpreted to record the evolution of a multiple vent, low-relief volcanic region, dominated by several large caldera centres. (C) 2000 Elsevier Science B.V. All rights reserved.