{"title":"智利的硼酸盐矿床","authors":"G. Chong, J. Pueyo, Cecilia Demergasso","doi":"10.4067/S0716-02082000000100007","DOIUrl":null,"url":null,"abstract":"ABSTRACT The borate deposits in Chile . The boron resources of Chile are all located in the northern part of the country mainly in the evaporitic basins known as 'salares' (salt flats) and are genetically related to Upper Tertiary - Quaternary volcanic activity. The most important deposits are located in the Andean basins of the Altiplano at Surire, Ascotan, Aguas Calientes Norte, Quisquiro, Aguas Calientes Sur, Maricunga and Pedernales. In addition other Altiplano basins may have boron resources, but have yet to be evaluated. The borates are present primarily in horizons known as `barras' and usually form lenses which interdigitate with evaporitic and clastic detrital sediments. In other instances boron minerals form nodules referred to as `papas' which are up to decimeters in diameter. Economic accumulations of boron are always located within the first few meters of the saline deposits. The only Chilean economic boron-bearing mineral is ulexite, a Ca-Na borate; other minerals appear in minor amounts. Boron is also present in the lithium-rich brines of the Salar de Atacama from which boron can be recovered as by-product of lithium extraction (0,84 g/l as polyborates). A third, and far less important type of deposit, is present in the Pampa del Tamarugal within borate-rich horizons associated with paleosols. Finally, other boron accumulations, currently not exploitable, are associated with geothermal brines Rev. geol. Chile v.27 n.1 Santiago jul. 2000","PeriodicalId":140719,"journal":{"name":"Revista Geologica De Chile","volume":"8 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2000-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"23","resultStr":"{\"title\":\"Los yacimientos de boratos de Chile\",\"authors\":\"G. Chong, J. Pueyo, Cecilia Demergasso\",\"doi\":\"10.4067/S0716-02082000000100007\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"ABSTRACT The borate deposits in Chile . The boron resources of Chile are all located in the northern part of the country mainly in the evaporitic basins known as 'salares' (salt flats) and are genetically related to Upper Tertiary - Quaternary volcanic activity. The most important deposits are located in the Andean basins of the Altiplano at Surire, Ascotan, Aguas Calientes Norte, Quisquiro, Aguas Calientes Sur, Maricunga and Pedernales. In addition other Altiplano basins may have boron resources, but have yet to be evaluated. The borates are present primarily in horizons known as `barras' and usually form lenses which interdigitate with evaporitic and clastic detrital sediments. In other instances boron minerals form nodules referred to as `papas' which are up to decimeters in diameter. Economic accumulations of boron are always located within the first few meters of the saline deposits. The only Chilean economic boron-bearing mineral is ulexite, a Ca-Na borate; other minerals appear in minor amounts. Boron is also present in the lithium-rich brines of the Salar de Atacama from which boron can be recovered as by-product of lithium extraction (0,84 g/l as polyborates). A third, and far less important type of deposit, is present in the Pampa del Tamarugal within borate-rich horizons associated with paleosols. Finally, other boron accumulations, currently not exploitable, are associated with geothermal brines Rev. geol. Chile v.27 n.1 Santiago jul. 2000\",\"PeriodicalId\":140719,\"journal\":{\"name\":\"Revista Geologica De Chile\",\"volume\":\"8 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2000-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"23\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Revista Geologica De Chile\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.4067/S0716-02082000000100007\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Revista Geologica De Chile","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4067/S0716-02082000000100007","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 23
摘要
智利硼酸盐矿床。智利的硼资源都位于该国北部,主要位于被称为“salares”(盐滩)的蒸发盆地中,并与上第三纪-第四纪火山活动有关。最重要的矿床位于Altiplano的Surire、Ascotan、Aguas Calientes north、Quisquiro、Aguas Calientes Sur、Maricunga和Pedernales的安第斯盆地。此外,其他Altiplano盆地可能有硼资源,但尚未进行评估。硼酸盐主要存在于被称为“巴拉斯”的地层中,通常形成透镜,与蒸发物和碎屑碎屑沉积物相交叉。在其他情况下,硼矿物形成结核,称为“papas”,直径可达分米。硼的经济富集总是位于盐渍矿床的最初几米内。智利唯一具有经济价值的含硼矿物是无辉石,一种钙钠硼酸盐;其他矿物质的含量也很少。硼也存在于阿塔卡马盐湖的富锂盐水中,硼可以作为锂提取的副产品(0.84克/升的多硼酸盐)被回收。第三种矿床的重要性要小得多,它存在于塔马鲁加尔Pampa del Tamarugal,位于与古土壤相关的富含硼酸盐的地层中。最后,其他目前尚未开采的硼矿床与地热卤水有关。智利第27节2000年7月圣地亚哥
ABSTRACT The borate deposits in Chile . The boron resources of Chile are all located in the northern part of the country mainly in the evaporitic basins known as 'salares' (salt flats) and are genetically related to Upper Tertiary - Quaternary volcanic activity. The most important deposits are located in the Andean basins of the Altiplano at Surire, Ascotan, Aguas Calientes Norte, Quisquiro, Aguas Calientes Sur, Maricunga and Pedernales. In addition other Altiplano basins may have boron resources, but have yet to be evaluated. The borates are present primarily in horizons known as `barras' and usually form lenses which interdigitate with evaporitic and clastic detrital sediments. In other instances boron minerals form nodules referred to as `papas' which are up to decimeters in diameter. Economic accumulations of boron are always located within the first few meters of the saline deposits. The only Chilean economic boron-bearing mineral is ulexite, a Ca-Na borate; other minerals appear in minor amounts. Boron is also present in the lithium-rich brines of the Salar de Atacama from which boron can be recovered as by-product of lithium extraction (0,84 g/l as polyborates). A third, and far less important type of deposit, is present in the Pampa del Tamarugal within borate-rich horizons associated with paleosols. Finally, other boron accumulations, currently not exploitable, are associated with geothermal brines Rev. geol. Chile v.27 n.1 Santiago jul. 2000