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

<table>Cross-sections of ore body and siliceous rock in the Bafangshan-Erlihe Cu-Pb-Zn ore deposit. For location see Figure <a href="../fig3/">3</a> (After-[<a href="/journals/tswj/2014/780910/#B12">12</a>]).</table>

The Scientific World Journal

fig4

Figure 4

Figure 4: Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 

Figure 4 | Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 