贵州开阳磷矿洋水矿区实物资料特征及采集意义
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摘要
贵州开阳磷矿床是我国生物化学沉积型磷矿床的典型代表,具有规模大、矿层厚、品位高等特征,2016年被国家实物地质资料馆列为I类实物地质资料采集的典型矿床。其中该磷矿之洋水矿区地质工作周期长,工作程度较高,形成的实物地质资料丰富,能够客观、系统的反映矿床地质特征。采集的该区实物地质资料具有重要的档案价值和科普意义,对指导进一步指导找矿和地质科学研究提供了详实的基础性实物地质资料。
Kaiyang P deposit,Guizhou is the typical representative of biochemical sedimentary P deposit in China,characterized by the large scale,very thick and high grade,etc.,which was placed into the typical deposit of material object geological data collection grade 1 by the state material object geological archives in 2016.In Yangshui orefield,the geological work period is long,study degree high,with abundant material object geological data,able to reflect objectively and systematically the geological feature of deposit.The collection of material object geological data in it have the important archives and popular science significance,and can provide the detailed basic material object geological data,guide the future prospecting and geological scientific study.
Kaiyang P deposit,Guizhou is the typical representative of biochemical sedimentary P deposit in China,characterized by the large scale,very thick and high grade,etc.,which was placed into the typical deposit of material object geological data collection grade 1 by the state material object geological archives in 2016.In Yangshui orefield,the geological work period is long,study degree high,with abundant material object geological data,able to reflect objectively and systematically the geological feature of deposit.The collection of material object geological data in it have the important archives and popular science significance,and can provide the detailed basic material object geological data,guide the future prospecting and geological scientific study.
引文
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[3]刘天忠.贵州省开阳县洋水地区磷矿地质特征及成因浅析[J].华东科技(学术版),2016,(04).
[4]邹忠远等.开阳县永温磷矿矿床地质特征与岩相古地理关系初析[J].低碳世界,2014,(10).
[5]吴文明等.开阳县永温磷矿稀土地球化学特征对沉积环境的指示[J].内蒙古煤炭经济,2015,(10).
[6]杨光亮等.贵州开阳地区洋水矿区洋水背斜东翼深部晚震旦世陡山沱期磷矿地质特征及成因浅析[J].企业技术开发(学术版),2017,(1).
[7]王槐山.贵州开阳磷矿地质特征及深部延伸找矿实践[J].中国媒炭地质,2017,29(5).
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