As, the crust eroded due to the plume (Sobolev et al. 2011), the eruptive sequences transitioned to basaltic lava flows, these are believed to have also been episodic, according to Self et al. (2014) with pulses of magma production and lava eruptions.
The map below shows the distribution of sill intrusions, pyroclasts and lava of the Siberian Traps.
Image source: IAVCEI - the red are sill intrusions, the light purple are pyroclasts and the dark purple is lava.
References
Black et al. 2014, Sulfur isotopic evidence for sources of volatiles in Siberian Traps magmas, Earth and Planetary Science Letters
Bryan and Ferrari, 2013, Large igneous provinces and silicic large igneous provinces: Progress in our understanding over the last 25 years, Geological Society of America Bulletin
Jerram et al. 2013, What happened at the start of the Siberian Traps? Understanding the onset of flood volcanism, American Geophysical Union, Fall Meeting 2013
Self et al. 2014, Emplacement characteristics, time scales, and volcanic gas release rates of continental fl ood basalt eruptions on Earth, The Geological Society of America Special Paper 505
Sobolev et al. 2011, Linking mantle plumes, large igneous provinces and environmental catastrophes, Nature