Three-dimensional potential field modelling of a multi-vent maar-diatreme - The Lake Coragulac maar, Newer Volcanics Province, south-eastern Australia

被引:33
作者
Blaikie, Teagan N. [1 ]
Ailleres, Laurent [1 ]
Cas, Ray A. F. [1 ]
Betts, Peter G. [1 ]
机构
[1] Monash Univ, Sch Geosci, Clayton, Vic 3800, Australia
关键词
Maar; Diatreme; Gravity; Magnetic; Potential field inversions; Newer Volcanics Province; WESTERN GAWLER CRATON; VENT COMPLEX; COOMBS-HILLS; PHREATOMAGMATIC VOLCANOS; SUBSTRATE; ERUPTION; STRATIGRAPHY; GEOMETRY; GRAVITY; HUNGARY;
D O I
10.1016/j.jvolgeores.2012.05.002
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
High resolution gravity and magnetic data have been acquired across Lake Coragulac, a Quatemary maar volcano located in the Newer Volcanics Province of south-eastem Australia. A gravity low is observed across the maar crater, with several local gravity highs identified in the centre of the crater, often with corresponding magnetic anomalies. Geophysical data has been integrated with geologic observations and subjected to 2D forward and 3D inverse potential field modelling. Modelling has revealed a complex subsurface maar structure with four coalesced diatremes and several intrusive dykes identified. The modelled diatremes are shallow (maximum of 290 m deep) with the margins having a similar density to the host rock, while the diatreme centre is often denser, indicating that higher volumes of volcanic debris are present. Deposits of the maar rim sequence show frequent transitions between phreatomagmatic and magmatic fragmentation styles, a result of fluctuations in magma rise rate and interactions with external water. The complex nature of the underlying maar-diatreme suggests that the maar formed from at least four vents which migrated laterally during the eruption. (C) 2012 Elsevier B.V. All rights reserved.
引用
收藏
页码:70 / 83
页数:14
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