The Relationship between Fluid Flow, Structures, and Depositional Architecture in Sedimentary Rocks: An Example-Based Overview

Figure 9

(a) Digitized map of the fracture network at Ras ir Raheb, Malta, with iron oxide precipitates shown as red dashed lines. (b) The branch intensity map indicates higher density in the areas of segment linkage. (c) Map of the connecting node frequency, which also increases in the areas where fault segments link indicating higher connectivity in linkage areas.