--> Figure 14. (A) Diagram showing the fluid-flow pathways (modified after Montañez, 1994). Recharge is in the Alleghenian highlands and flow is through the thrusted Paleozoic section, which contains the Knox Formation. Estimated relief based on conodont alteration, estimated overburden thickness, and fluid inclusion homogenization temperatures. (B) Detail of conceptual fluid-flow model.

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Figure 14. (A) Diagram showing the fluid-flow pathways (modified after Montañez, 1994). Recharge is in the Alleghenian highlands and flow is through the thrusted Paleozoic section, which contains the Knox Formation. Estimated relief based on conodont alteration, estimated overburden thickness, and fluid inclusion homogenization temperatures. (B) Detail of conceptual fluid-flow model.