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Offshore high-grade limemud resources of west coast of India:Economic potential and industrial applications
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作者 Anil Kumar Adukadukkam Rachna Pillai Mamatha Puthiyathara Kanakamma 《Deep Underground Science and Engineering》 2024年第2期163-170,共8页
Limestone is one of the essential raw materials in the cement,paint,steel,ceramic,glass,chemical,pharmaceutical,paper,and fertilizer industries.In India,only 8%of the limestone resources are placed under the reserve c... Limestone is one of the essential raw materials in the cement,paint,steel,ceramic,glass,chemical,pharmaceutical,paper,and fertilizer industries.In India,only 8%of the limestone resources are placed under the reserve category,of which 97%is of cement grade.Thus,India depends on imports to bridge the demand‐supply gap of steel,blast furnace,and chemical‐grade limestone.Efforts of Geological Survey of India(GSI)to locate alternate sources for limestone led to the discovery of enormous quantities of carbonate minerals called limemud from the continental shelf margin of the west coast of India.GSI carried out systematic studies to explore the nature of the disposition,quality,quantity,and suitability of the offshore limemud for various industrial applications.A preliminary estimate of resources using high‐resolution subbottom profiling and sediment core sample studies established the occurrence of more than 172 billion tonnes of high‐grade(The content of CaCO3 is greater than 80 wt%)limemud in 0.4–28.0m thick stratified sediment layers spread over an area of 18000 km2.Chemical,physical,mineralogical,beneficiation,and agglomeration studies found the offshore limemud as a potential replacement for limestone in the cement,filler,blast furnace,steel melting shop,lime production,paint,and Grade‐I steel industries.An assessment of mining and transportation costs indicates that the offshore limemud(USD 5–6/ton)is more cost‐effective than that imported from other countries(USD16‐18/ton).With several advantageous factors like low impurity,mode of occurrence in overburden‐free stratified form,fine‐grained slurry nature,and shallow water depth,sustainable mining of offshore limemud could be a future reality with controllable technological,economic,and environmental challenges. 展开更多
关键词 beneficiation industrial grade offshore limemud west coast of India
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陕北盐盆奥陶系马家沟组沉积相特征与沉积演化 被引量:9
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作者 施立志 王卓卓 +3 位作者 张永生 苏奎 邢恩袁 桂宝玲 《地质学报》 EI CAS CSCD 北大核心 2015年第11期2122-2133,共12页
本文主要依据陕北盐盆地的镇钾1井等8口基干井,通过岩心观察、测井解释、镜下薄片鉴定,同时结合区域构造资料并参考前人研究成果,对陕北盐盆奥陶系马家沟组岩石类型、沉积相、沉积演化进行了研究。结果表明岩石类型以碳酸盐岩和蒸发岩为... 本文主要依据陕北盐盆地的镇钾1井等8口基干井,通过岩心观察、测井解释、镜下薄片鉴定,同时结合区域构造资料并参考前人研究成果,对陕北盐盆奥陶系马家沟组岩石类型、沉积相、沉积演化进行了研究。结果表明岩石类型以碳酸盐岩和蒸发岩为主,碎屑岩等其他沉积岩发育较少。主要发育碳酸盐岩台地相,可进一步划分出开阔台地和局限蒸发台地两种亚相,开阔台地可识别出灰泥丘微相;局限蒸发台地可识别出云坪、盐湖、膏湖、淡化泻湖等微相。沉积演化表明,马一期-马六期,陕北盐盆经历了三次海进-海退旋回,沉积演化为陕北盐盆及钾岩的形成创造了良好的成盐古地理环境,海进期,海水提供充足的成钾物质补给,海退期形成的继承性盐盆,四周隆起,又处在有利的低纬度干旱蒸发气候环境,十分有利于钾岩的形成。陕北盐盆奥陶系马家沟组五段六亚段沉积期,盆底总体表现为"两坳夹一隆"的构造样式,即自西向东依次为呈NNE向展布的西部盐坳、中部隆起和东部盐坳,"西部盐坳"可进一步分为3个次级盐凹,自北向南依次为"西一盐凹"、"西二盐凹"和"西三盐凹";"东部盐坳"可进一步分为2个次级盐凹,即北部的"东一盐凹"和南部的"东二盐凹",这5个盐凹的盐系地层厚度大于150m,是陕北盐盆最佳成钾盐凹,也是优先进行钾盐探井部署的有利目标区。 展开更多
关键词 陕北盐盆 马家沟组 沉积 灰泥丘
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