蚀变岩帽的特征成因以及在华南的分布探讨(10)

总体来说，现有的华南地区蚀变岩帽发育特征和成因研究表明，浙闽沿海至长江中下游地区广泛发育蚀变岩帽，指示该区可能存在一条巨型的斑岩-浅成低温矿床成矿带，具有非常好的找矿勘查前景，但目前无论从理论研究还是勘探程度方面，都需要重视和加强。对比国外蚀变岩帽的研究与勘查经验，深化华南地区蚀变岩帽的深入系统研究，可望为将来实现该区找矿上的新突破打下坚实的前期工作基础与准备。

致谢本文部分工作获得了中国国家留学基金委提供的奖学金资助，对此表示感谢。本文内容与世界著名斑岩-浅成低温热液矿床学家David Cooke, Richard Sillitoe, Jeffery Hedenquist, Greg Corbett, Richard Tosdal, Rachel Harrison和Adi Maryono，以及塔斯马尼亚大学CODES多位老师和同学进行过讨论，对他们的无私交流表示特别感谢。

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