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中国磷矿成矿规律与高效勘查技术组合OA

Metallogenic Regularity of Phosphate Deposits in China and the Efficient Exploration Techniques

中文摘要英文摘要

中国作为全球第二大磷矿资源国及主要消费国,磷矿资源对国家粮食安全与新能源产业发展具有不可替代的战略意义,亟需加强磷矿资源的勘查评价工作.成矿规律研究与高效勘查技术体系的建立是实现磷矿找矿突破的重要基础.本文在前人研究基础上,系统总结了中国磷矿的成因类型、成矿机制与时空分布规律,并研究归纳了针对不同类型磷矿的高效勘查技术方法及其应用实例.研究表明,中国磷矿资源丰富,储量大且分布集中,按成因可分为岩浆岩型、沉积型和变质型三类.其中岩浆岩型磷矿主要分布在华北克拉通东北部及塔里木盆地东北缘,成矿时代以三叠纪至白垩纪为主;沉积型磷矿广泛分布于扬子克拉通中西部,主要成矿期为震旦纪、寒武纪和泥盆纪;变质型磷矿则主要赋存于华北克拉通桐柏-大别成矿带和苏鲁成矿带,形成时代主要为元古宙和太古宙.当前磷矿勘查以地球物理方法为主、地球化学方法为辅.针对岩浆岩型磷矿,宜采用遥感构造解译、光谱测量、磁法与电法相结合的技术组合,并关注F、U、Th及稀土元素异常信息;沉积型磷矿应在岩相古地理研究基础上,综合音频大地电磁法、γ放射性测井,及V、Mn、Sr、Ba等元素异常分析;变质型磷矿宜采用使用重力、航磁与音频大地电磁法组合,结合Fe、P、Ti、V等元素异常进行综合圈定.未来磷矿勘查应遵循地质研究先行的原则,依据矿床类型与具体地质条件优选高效勘查技术组合,同时加强新型便捷勘查技术的研发与应用,以实现深部及覆盖区磷矿找矿的重大突破.

China is the world's second-largest holder of phosphate rock resources and also a major consumer.Phosphate plays an irreplaceable role in both national food security and the development of new energy industries.Therefore,there is an urgent need to strengthen exploration and evaluation efforts for phosphate resources.Research on metallogenic regularities and the establishment of an efficient exploration technology system are essential for achieving breakthroughs in phosphate prospecting.Based on previous studies,this work systematically summarized the genetic types,metallogenic mechanisms,and spatiotemporal distribution patterns of phosphate deposits in China.It also reviewed and synthesized efficient exploration techniques and their application examples tailored to different types of phosphate deposits.Research indicates that China is endowed with abundant phosphate resources,characterized by large reserves and concentrated distribution.These deposits can be classified into three genetic types:magmatic,sedimentary,and metamorphic.Magmatic-type phosphate deposits are mainly distributed in the northeastern North China Craton and the northeastern margin of the Tarim Basin,with their metallogenic epoch predominantly spanning the Triassic to Cretaceous.Sedimentary-type phosphate deposits are widely distributed in the central and western Yangtze Craton,primarily formed during the Sinian,Cambrian,and Devonian periods.Metamorphic-type phosphate deposits are mainly hosted within the Tongbai-Dabie metallogenic belt and the Sulu metallogenic belt in the North China Craton,with formation ages primarily in the Proterozoic and Archean.Currently,phosphate exploration relies predominantly on geophysical methods,supplemented by geochemical techniques.For magmatic-type deposits,a combination of remote sensing structural interpretation,spectral measurement,magnetic and electrical methods is recommended,with attention to anomalies of F,U,Th,and rare earth elements.For sedimentary-type deposits,exploration should integrate lithofacies and paleogeographic studies with audio-frequency magnetotelluric(AMT)methods and gamma-ray logging,supplemented by analysis of anomalies in elements such as V,Mn,Sr,and Ba.For metamorphic-type deposits,a combination of gravity,aeromagnetic,and AMT methods is advisable,coupled with comprehensive delineation based on anomalies of Fe,P,Ti,and V.Future phosphate exploration should adhere to the principle of prioritizing geological research,selecting efficient technical combinations based on deposit types and specific geological conditions,while also advancing the development and application of new rapid exploration technologies to achieve significant breakthroughs in prospecting deep-seated and covered phosphate deposits.

孙盼飞;李永胜;徐劲驰;李鑫杰;姚晓峰;孙海瑞

中国地质调查局发展研究中心,北京 100037||自然资源部矿产勘查技术指导中心,北京 100037中国地质调查局发展研究中心,北京 100037||自然资源部矿产勘查技术指导中心,北京 100037中国地质调查局发展研究中心,北京 100037||自然资源部矿产勘查技术指导中心,北京 100037中国地质调查局发展研究中心,北京 100037||中国地质大学(北京)地球科学与资源学院,北京 100083中国地质调查局发展研究中心,北京 100037||自然资源部矿产勘查技术指导中心,北京 100037中国地质调查局发展研究中心,北京 100037||自然资源部矿产勘查技术指导中心,北京 100037

天文与地球科学

磷矿成因类型成矿规律时空分布勘查技术找矿突破成矿机制

phosphate depositgenetic typesmetallogenic regularityspatiotemporal distributionexploration techniquesprospecting breakthroughore-forming mechanism

《地质与勘探》 2026 (3)

443-458,16

自然资源部部省合作试点项目(编号:2023ZRBSHZ059)和科技部科技基础资源调查专项(编号:2002FY101701)联合资助.

10.12134/j.dzykt.2026.03.001

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