黑色页岩的成岩成矿作用一直以来都是地学界研究的热点。扬子地台南、北缘均大规模出露成矿元素组合非常类似的下寒武统黑色页岩。尽管前人已对这两个黑色页岩带的成矿过程及氧化还原沉积环境完成了大量重要探索，但赋存其中的钒矿成矿机制依旧存在争论，早寒武世扬子地台南、北缘古海洋沉积环境的异同性也尚未得到很好的揭示。本项目以扬子地台南缘江古钒矿和北缘千家坪钒矿的下寒武统富钒黑色页岩为对比研究对象，运用扫描电镜、激光拉曼等技术手段开展岩相学观察和有机质分析，并联合应用微量元素、O-Si同位素、Re-Os同位素以及Mo-U非传统同位素等技术方法，探讨钒矿的成矿物质来源，查明扬子地台南、北缘早寒武世古海洋沉积环境的异同以及与钒矿化的关系，确定成矿机制，建立早寒武世扬子地台周缘钒矿成矿模型和古海洋演化模型，发展和完善黑色页岩成矿理论。

Diagenesis and metallogenesis study associated with black shales has been a hot topic for a long history. Two huge black shale metallogenic belts with very similar mineral assemblage are exposed along the southern and northern margin of the Yangtze Platform. Although previous studies have greatly promoted understandings on the mineralization processes and redox geochemistry of Early Cambrian seawater, metal source of vanadium-rich black shales and its mineralization processes are still controversial. In addition, the paleo-redox conditions of the southern and northern margin sea of the Yangtze Platform during Early Cambrian still needs better constraints. This study compares Jianggu and Qianjiaping V deposits that are hosted by the Early Cambrian black shales along the southern and northern margin of the Yangtze Platform, respectively. In this study, SEM and laser raman will be used for detailed mineral observation and TOC analysis. In combination with diagnostic trace element geochemistry, O-Si isotope, Re-Os isotope, and Mo-U non-traditional isotope techniques, we wish to identify the source of metals in V-rich black shales, and to compare the redox conditions of Early Cambrian seawater of the southern and northern margin sea of the Yangtze Platform. Finally, we will establish a genetic model for the V mineralization and reveal the Early Cambrian seawater redox condition that across the integrated Yangtze Platform. These studies will provide insight into the Early Cambrian earth evolution history and will have general implications for developing the metallgenic theory associated with black shales.