Schneibster,
I was with you, I thought, when you said that the impact might have generated gamma rays. I wasn't sure that there would be a significant amount but I thought your point was that the radiation created would follow a black body curve and there would be some gamma radiation in the tail.
Now it seems that you were saying that radiation might have peaked in the gamma range? That seems doubtful as your calculation of 115,000,000 degrees suggested to me, but maybe I am completely confused either by what you meant or the actual physics.
I didn't complete the thought.
Let's follow the logic from the other end. To create a nuclear explosion in the tens of megatons, the initial temperature of the exploding core has to be on the close order of hundreds of millions of degrees in a device on the close order of tens of meters in size. This is of the same or one lesser order of magnitude than the thirty meter object estimated for Tunguska. To create a 15Mt explosion, then, the temperature has to have briefly been on the close order of tens to hundreds of millions of degrees; any less and there will not be sufficient energy to create an explosion so large from an object so small.
I have never touched the physics of how such a high temperature could come to be; I'm pretty certain that to get a result that's within even multiple orders of magnitude of the correct one, you're going to need numerical simulations, which ain't happenin' on this here cute little laptop anytime this year.

To give you an idea of what's involved, first we need to remember that at the speeds such an object is moving, the compression wave in front of it is basically going to consist of trapped air, incapable of escaping due to the speed of the oncoming object; so you can model the bolide as cylindrical column of compression. The pressure increases extremely quickly, driving the temperature very high. As temperature rises, the bolide vaporizes from the front, adding to the material available, but absorbing heat as latent heat of liquifaction and vaporization.
Basically, the Tunguska object encountered the top of the troposphere as a solid barrier which caused it to vaporize at impact; the vaporized bolide, along with a comparatively small amount of superheated, ionized air then formed a gas jet that struck the surface of the Earth at hypersonic velocity. The heat pulse from the impact with the troposphere would have briefly been in the hundreds of millions of degrees, generating a blackbody radiation peak in the gamma; the bulk of this pulse would have been absorbed by the atmosphere and bolide body, and turned to lower frequencies and re-emitted.
Some of the gamma, however, would escape the region where the bolide was being vaporized, and even a small percentage would yield a fairly powerful gamma pulse. Obviously, however, the bulk of the gamma rays were absorbed by material in the immediate vicinity, because otherwise not enough energy would remain to create the gas jet.
It's likely that anyone looking directly at the explosion at any distance from which it would be visible on the surface would be at minimum temporarily flash blinded (which is what happens when you look at a light so bright it consumes all the photosensitive dye in your retina; the dye is regenerated, but it takes a while). If they were close, retinal burns and permanent blindness would result, but it's possible being blinded would be the least of their problems since third-degree flash burns would also be a likely result of being that close. In 1908, third-degree flash burns over any significant portion of the body would likely be a death sentence. Being actually inside or even in direct line-of-sight of the fireball's impact with the surface would result in instant personal vaporization. Effects in between would range in severity.
I suspect that anyone who could get enough gamma radiation to cause radiation sickness would have far worse problems than that; whether other physical effects of the radiation would linger would depend on the material affected. Gamma doesn't make things radioactive the way neutrons do, so it would just be the one pulse. Without any other source of radiation, I'm not sure wood, water, or stone could retain anything measurable a hundred years later, but it's not impossible.
To conclude, basically, from a distance, your "tail" of gamma is about what you'd see; most of the gamma and X-ray radiation created at tropospheric impact would be absorbed in the immediate vicinity of the impact, and contribute to the temperature of the fireball, which would then shoot down to the surface. But inside the fireball, at the moment of its creation, you'd get very high gamma or X-ray flux, just as you do at the detonation of a nuclear weapon. Everything else that happened would just be the aftereffects of that pulse, again, just as it is in a nuclear explosion.
Is that clearer?
And again, I still invite criticism and the detection of any holes in the reasoning. There are folks here other than me who can contribute to our understanding of what happened if they choose.