Welcome to the forum.
There's no reason why a pallasite would be "found along with tektites and chondrites". They're three completely different things with differing origins. Tektites also have very specific geographical strewnfield localities and - unlike meteorites - are usually found some distance from the impact sites with which they are associated. Are you sure about the identity of these other specimens? Could we see them please and where exactly were these things found?
Pallasites belong to the stony iron group and so should have visible metal. I don't see it. They would also be strongly magnetic. Is your specimen magnetic? It's theoretically possible to find just the stony/olivine portions of a pallasite from which all the metal has rusted away and it then wouldn't necessarily look much different from terrestrial olivine, but that would be highly unusual... especially a piece as large as you are showing. Presumably the third picture is the same specimen pictured by reflected light rather than transmitted light. If it is, then it doesn't show anything with the typical appearance of pallasitic material.