The Chelyablinsk meteor entered at a very shallow angle & was a chondrite with little internal strngth, so it disintegrated over a longer distance forming a “line burst” rather than a single point airburst.
Had it entered more steeply, then it would have concentrated it’s KE over a much smaller area, causing much more damage.
A nuclear bomb may take a few ms, but after a few 100ms, you’ve got a dense, hot plasma in a small volume. Sounds a lot like the result of a metorite airburst! And indeed, people use the same codes that are used to model nuclear explosions to model meteor airbursts.
Even though an atomic bomb blast is not applicable because of the historic absence of atomic explosions in the area, an atomic blast produces a wide range of melt products that are morphologically indistinguishable from the melted material found at TeH (Fig. 51). These include shocked quartz64; melted and decorated zircon grains (Fig. 51a, b); globules of melted material (Fig. 51c, d); meltglass containing large vesicles lined with Fe-rich crystals likely deposited by vapor deposition (Fig. 51e, f); spherules embedded in a meltglass matrix (Fig. 51g, h). Also, atomic detonations can replicate the physical destruction of buildings, the human lethality, and the incineration of a city, as occurred in World War II.
added: though, I forget to mention, that they also found many chemical elements and compositions that are hard to find under normal conditions (atomic bomb tests included as I understood), but abundant in meteorites.