我国饰面用大理岩成矿区带划分和成矿规律

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我国饰面用大理岩资源丰富,品种多样.但地区分布不均,饰面用大理岩资源的50%以上分布在河北、甘肃、江西、安徽等地.本文通过全面收集、整理资料,总结了饰面用大理岩资源特征;充分利用前人研究成果,结合饰面用大理岩矿床分布特点、构造环境和原岩建造等,共划分20个饰面用大理岩成矿区带;总结了我国饰面用大理岩成矿时代主要为前寒武期、华力西期和燕山期,空间上主要分布于滨太平洋成矿域和古亚洲成矿域等成矿规律,研究了矿床主要赋存于前寒武纪、古生代地层的成矿专属性,为我国饰面用大理岩找矿勘查提供了参考.
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河北是国内饰面用花岗岩矿的重要产地之一,有太行山及燕山两大成矿带,已发现大中型矿床21处、小型矿床和矿化点70余处.通过对成矿地质背景、典型矿床、赋矿地质体及成矿构造的分析,将河北饰面用花岗岩矿床类型分为5类、15亚类,侵入岩型矿床类型有4类、11亚类,分布于以燕山期为主,晋宁期为次的酸性—超基性侵入岩中,受构造—侵入岩带控制;变质岩型矿床类型有1类、4亚类,形成于新太古代—古元古代混合岩化区域变质岩中.河北已形成冀中、冀北及冀东3大石材产业基地,石材品种达30余种,太行山中段的“中国黑”、冀北地区的“燕