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- W2040992867 abstract "Sampling in the Arumpo leases in southwest New South Wales over an area of 5 × 10 km has delineated the structure and composition of two large high-purity bentonite deposits, spatially adjacent but deriving from two separate volcanic events. They are overlain by fluvial and other sediments including later bentonite formations. All of the bentonite deposits are considered to be formed from volcanic ash falls deriving from lavas from related magma sources. Recent aeromagnetic surveys have shown the presence of extensive clusters of highly magnetic pipe-like structures, presumably volcanic plugs, lying as close as 15 kilometres from the deposits. The two major deposits are generally flat-lying and 5 – 8 m thick with Na and Mg as the dominant exchange cations, with minor exchangeable K and Ca. They constitute an Na – Mg variety of bentonite as compared with Na- or Ca-dominant bentonites elsewhere in the world. The deeper deposit lies in a graben near the edge of the Neckarboo Fault, and presumably was deposit..." @default.
- W2040992867 created "2016-06-24" @default.
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- W2040992867 date "2008-03-01" @default.
- W2040992867 modified "2023-09-26" @default.
- W2040992867 title "Arumpo bentonite deposits: distinctive indicators of past volcanic events in the Murray Basin, southeastern Australia" @default.
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- W2040992867 doi "https://doi.org/10.1080/08120090701689357" @default.
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