This article analyzes the tectonic and magmatic processes responsible for the formation of Noctis Labyrinthus on Mars. It presents a high-resolution structural map and identifies three main fault systems, linking their orientations and interactions to tectonic phases and magmatic influences. Pit chains are examined and classified into four evolutionary stages, suggesting a formation driven by both extensional tectonics and magmatic chamber deflation. The study proposes a deformational model involving early extension and magmatic plumbing as co-occurring drivers.