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

<table>Spatial distribution of total siliceous rocks in the COB (EKL: eastern Kunlun; M-SQ: Middle-South Qilian; NQ: North Qilian; WQL: Western Qinling; EQL: Eastern Qinling; SKC: Sino-Korean craton; YZB: Yangtze block; DB: Dabie orogenic belt; Data sources: [<a href="/journals/tswj/2014/780910/#B32">32</a>, <a href="/journals/tswj/2014/780910/#B37">37</a>–<a href="/journals/tswj/2014/780910/#B40">40</a>]).</table>

The Scientific World Journal

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Figure 7

Figure 7: Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 

Figure 7 | Distribution, Microfabric, and Geochemical Characteristics of Siliceous Rocks in Central Orogenic Belt, China: Implications for a Hydrothermal Sedimentation Model 