Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model

<table>Trace element discrimination diagram indicating mostly hydrothermal genesis for siliceous rocks from the Bafangshan-Erlihe area (After-[<a href="/journals/tswj/2014/780910/#B61">63</a>]).</table>

The Scientific World Journal

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Figure 12

Figure 12: Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 

Figure 12 | Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 