Desiccation thermograms for disperse materials moistened by various liquids

Kazanskii, M. F.; Kazanskii, V. M.; Lutsyk, R. V.; Mel'nikova, A. F.

doi:10.1007/bf00832215

Cited by 2 publications

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“…Paleomagnetic study of the SG-6 superdeep drill-hole has shown that the initial volcanic rocks are as old as latest Late Permian (upper part of the Late Tatatrian) (Kazanskii et al, 2000). Fig.…”

Section: Timing Of Initial Eruptions Within the Siberian Traps Fbpmentioning

confidence: 99%

Evaluation of different models for the origin of the Siberian Traps

Ivanov¹

2007

Special Paper 430: Plates, Plumes and Planetary Processes

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Various evidence, including size and volume of the Siberian Traps, timing and duration of eruptions, paleotectonic and paleogeographic reconstructions, lithospheric structure, heat flow, trace element and radiogenic isotope compositions of lava are reviewed in this chapter.The major evidence may be summarized as follows. The Siberian Traps erupted in a number of brief volcanic events from the Late Permian until the end of the Middle Triassic. They In radiogenic isotope and trace element coordinates, mixing trends between these two types of magma are absent or, at least, not evident. Some volcanic rocks contain primary magmatic mica. These are considered in light of different models. Each model can explain, or was thought to explain, particular observations. However, some evidence can be fatal for some models. For example, the enormous size and volume cannot be explained in the framework of impact and edge-driven convection models, and is problematic for lithospheric delamination models. Plume models face problems explaining the uplift/subsidence pattern and the absence of mixing curves between expected high-Ti primary plume melts and contaminated low-Ti

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Section: Timing Of Initial Eruptions Within the Siberian Traps Fbpmentioning

confidence: 99%