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

<table>Fe<sub>2</sub>O<sub>3</sub>/TiO<sub>2</sub> versus Al<sub>2</sub>O<sub>3</sub>/(Al<sub>2</sub>O<sub>3</sub> + Fe<sub>2</sub>O<sub>3</sub>) discrimination diagram indicating the formation environment of the siliceous rocks of the Bafangshan-Erlihe area (After [<a href="/journals/tswj/2014/780910/#B51">53</a>]).</table>

The Scientific World Journal

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Figure 10

Figure 10: Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 

Figure 10 | Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 