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It's taken me a while, but here is my first interferogram of the Venezuela earthquakes from Sentinel-1. It's an ascending track to the west of the epicenter, and the pattern of displacements is consistent with slip on a fault that runs close to and parallel to the coast.

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The symmetry of the pattern means it's almost certainly horizontal movement here. Each fringe is 2.8 cm of line-of-sight displacement, and assuming it's horizontal motion on an E-W fault represent about 4-5 cm of E-W displacement each.

This captures where the fault rupture ended (where the fringes pinch together, more or less). I would expect a lot more displacement in the data to the east.