Study on the Mechanism of Organic Matter Enrichment in Early Cambrian Marine Shales in the Lower Yangtze Area, South China: An Example Using Well JXY1

<div>Through the Al-Fe-Mn ternary plot analysis, siliceous minerals from the Lower Cambrian Wangyinpu Formation in Well JXY1 contain excess siliceous minerals, which are derived from hydrothermal origins. See Figure <a href="../fig1/">1</a> for the well location.</div>

Geofluids

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Figure 5

Figure 5: Study on the Mechanism of Organic Matter Enrichment in Early Cambrian Marine Shales in the Lower Yangtze Area, South China: An Example Using Well JXY1 

Figure 5 | Study on the Mechanism of Organic Matter Enrichment in Early Cambrian Marine Shales in the Lower Yangtze Area, South China: An Example Using Well JXY1 