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

<table>Trace element discrimination diagram demonstrating formation environment at a marginal sea basin for the siliceous rocks of the Bafangshan-Erlihe area (After-[<a href="/journals/tswj/2014/780910/#B44">46</a>]).</table>

The Scientific World Journal

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Figure 13

Figure 13: Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 

Figure 13 | Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 