Lorenzo, from your question I assume you are not familiar with this kind of data, so let me write down a few things that I hope get you on the way.
TVD, TVDSS and MD are both measures of position along the well track. They differ as follows:
MD is length along the well track reference from usually regerence from the KB (Kelly Bushing) point. For vertical wells MD - TVD is constant, and is the distance between their reference levels.
TVD is the depth of the well track, usually referenced from local ground level, downward*.
TVDSS is the depth of the well track, reference from the reference plane (sea level, or it's onshore equivalent), downward*.
*Disclaimer, for the sticklers, you occasionally see that TVD is provided positive upwards...
KB, and TD are points along your well track, in fact they are the starting and ending point of the well track, so they would define the geometry of your well track completely if the well is vertical. But,
KB is typically provided as an elevation above SS (sea level == geodetic datum).
TD is typically provided as a MD.
You need to verify these are indeed the definitions used in your dataset.
In the default situation (and it is up to you to verify if you are in the default situation), you can get to a well track definition in MD by setting the KB value to 0 (zero) and that seems the most straight forward solution to your question,
If your survey is in seismic time, (not depth) then you will also need to provide depth time relations as additional step and this will actually determine how your well stick relates to the seismic data. If you plan to post well markers, import well logs, or tie seismic data the depth-time relation needs to be fairly accurate, otherwise you can just get away by providing depth-time pairs for the end points of the well track, or stick with the constant velocity option provided in the track import.
Just heads up, I did not address this, but in general you need to be extra careful and specify some extra information, if your seismic reference level is not equal to the geodetic reference plane. This is often the case in onshore surveys.
I would recommend a good read of this
help entry, especially the image towards to bottom is very clarifying in addition to the explanation here.
Friso Brouwer
Geophysical Consultant