The Siberian Traps - Research at Leicester |
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Recently, we have been studying the age and composition of basalts from the West Siberian Basin. Reichow et al. (2002) confirmed that basalts from boreholes in the WSB are the same age, within error of the technique, as basalts from the Noril'sk and Putorana regions. In a later paper, we showed that compositionally they are similar to the Nadezhdinsky Suite at Noril'sk (Reichow et al., 2005). These results were reported widely in the media, including the BBC, Nature and Geotimes. In addition, we have been using seismic profiles, borehole data, and information from the Russian literature, to study the rifting and subsidence history of the West Siberian Basin (Saunders et al., 2005). The study indicated that the Basin was a region of positive relief during the Permian, and that it underwent rifting during the Triassic, mostly after the basaltic volcanism. Subsidence of the basin floor appears to have been delayed throughout the Triassic. These observations are consistent with a thermal anomaly beneath the basin during the Permian and Triassic. Recent publicity and news: |
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Figure Caption: Basaltic lavas exposed on the Putorana Plateau. Photo courtesy of NHK, Japan. |
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Current: A NERC grant has enabled us to study the extent and environmental impact of the Siberian Traps. We have undertaken a major dating programme using Ar-Ar techniques, in collaboration with SUERC and Dr Malcolm Pringle at MIT. Some of the data have recently been published (Reichow et al., 2009). |
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