Here is a fairly basic definition. This is not what we are seeing currently. We are seeing transient ridging episodes , but not a blocked flow.
"Blocking events are associated with long-lasting and slow-moving high-pressure systems that "block" westerly winds in the mid- and high-latitudes, causing the normal eastward progress of weather systems to stall."
When I see 50/50 lows flying northward into the upper latitudes, that tells me there is no NA block. That is not to say a bootleg/transient ridge in the NA with a 50/50 low is not beneficial, but because both are on the move, it requires more precise timing.