贵州开阳以东震旦系陡山沱组磷矿富磷机制与“三位一体”预测找矿重大突破*
刘建中1,2, 王泽鹏1,3, 杜远生1,4, 张亚冠4,5, 吴文明1,3, 陈国勇2, 付芝康3, 万大学3, 王大福3, 谭代卫3

Enrichment mechanism of phosphorite deposits and significant breakthrough in “Triunity Model”for ore prospecting in the Sinian Doushantuo Formation of eastern Kaiyang region,Guizhou Province
Liu Jian-Zhong1,2, Wang Ze-Peng1,3, Du Yuan-Sheng1,4, Zhang Ya-Guan4,5, Wu Wen-Ming1,3, Chen Guo-Yong2, Fu Zhi-Kang3, Wan Da-Xue3, Wang Da-Fu3, Tan Dai-Wei3
开阳以东整装勘查区陡山沱组地层定量岩相等值线图与沉积期古地理图(据 王泽鹏等,2016 ;有修改) A—陡山沱组地层总厚度等值线图;B—陡山沱组地层磷矿层(B矿层)厚度等值线图;C—陡山沱组地层磷矿层(B矿层)品位等值线图;D—开阳地区陡山沱组沉积期岩相古地理图