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

<div>(a) Example of fracture tip interaction, where the front of the iron oxide precipitates (black, dashed line) curves out where the fracture tips overlap; Hokianga, New Zealand. (b) Example of how iron oxide precipitates respond to fracture-tip interaction: the front of the iron oxide precipitates (black, dashed line) narrows as the fractures (white arrows) tip out; Hokianga, New Zealand.</div>

Geofluids

fig4

Figure 4

Figure 4: The Relationship between Fluid Flow, Structures, and Depositional Architecture in Sedimentary Rocks: An Example-Based Overview 