首页> 外文会议>International Conference on Mining and Metallurgy >DEPOSIT OF THE LISINA PHOSPHATES LIKE THE BASE OF RAW MATERIALS FOR PRODUCTION THE NATURAL MINERAL FERTILIZERS
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DEPOSIT OF THE LISINA PHOSPHATES LIKE THE BASE OF RAW MATERIALS FOR PRODUCTION THE NATURAL MINERAL FERTILIZERS

机译:像生产天然矿物肥料的原料底座一样沉积Lisina磷酸盐

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Deposit of the Lisina phosphates is in the southeast of Serbia, on the territory of the community Bosilegrad, close to Serbian-Bulgarian border. Genetically, the deposit of the Lisina phosphates belongs to the metamorphic deposits. Narrow area of the deposit is built by metamorphk formations with intensively presence of granitoids rocks. Phosphorites are in the contact zone of'he Meta sandstone which is the floor of sericile-chlorite slates with intercalations of marble and kalkshist in the roof Raw phosphates can be. applied as fertilizers with the positive effect: on the territory of Serbia where are mostly the acid soils on more than 50% of the territory.
机译:Lisina磷酸盐沉积在塞尔维亚的东南部,在社区博塞尔莱格勒境内,靠近塞尔维亚 - 保加利亚边境。遗传上,Lisina磷酸盐的沉积属于变质沉积物。沉积物的狭窄区域由MetyMoRPHK地层构建,具有浓度存在的花岗岩岩石。磷酸盐在HE'HE砂岩的接触区中,是浆液 - 氯酸盐板块的地板,屋顶原料磷酸盐的大理石和kalkshist嵌入。用积极效应施用肥料:在塞尔维亚境内,大多数酸性土壤超过50%的境内。

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