Russell S. Harmon , P. Louis Lu , Adam C. Curry , Russell M. Murray , Daniel D. Richter
{"title":"LIBS作为锂伟晶岩勘探和前景评价的工具:卡罗莱纳锡锂辉石带土壤云母和土壤分析","authors":"Russell S. Harmon , P. Louis Lu , Adam C. Curry , Russell M. Murray , Daniel D. Richter","doi":"10.1016/j.apgeochem.2025.106534","DOIUrl":null,"url":null,"abstract":"<div><div>Lithium is an essential element along the pathway to a high-technology future. Being able to efficiently explore for Li deposits and fully assess prospects is necessary to reduce exploration costs, shorten time between discovery and production, and minimize environmental impacts of exploration and production. Laser-induced breakdown spectroscopy (LIBS) is an analytical technology for real-time geochemical analysis in both the laboratory and the field that has potential to enhance current capabilities for Li pegmatite exploration and prospect evaluation. This study was conducted in a portion of the Carolina Tin-Spodumene Belt in Gaston County, NC at one of the largest Li-pegmatite prospects in the USA. Analysis by handheld LIBS first observed the same Li–K/Rb systematics for individual mica grains in soil as for mica in both barren quartz-feldspar and spodumene-bearing pegmatites, suggesting that soil mica analysis might be used for geochemical vectoring towards mineralized pegmatite. The contents of Li, K, and Rb in Bt horizons of residual Kanhapludult soil were determined in the field from matrix-matched LIBS calibrations along five transects across an area where a subsurface spodumene pegmatite dike was known from drilling to be present at ∼15-m depth. Unlike the situation for mica, no systematic variation was observed for soil K and Rb abundances, with K/Rb ratios not reflective of the presence of subsurface mineralization. By contrast, soil Li content spiked sharply where a sampling transect passed directly over the spodumene mineralized dike. It was also noted that soil Li abundances are significantly elevated across the domain of the Carolina Tin-Spodumene Belt of pegmatite mineralization on a regional scale compared to other Piedmont and Coastal Plain soils. Thus, there is potential for rapid soil geochemical analysis by LIBS in Li-pegmatite exploration at both local and regional spatial scales.</div></div>","PeriodicalId":8064,"journal":{"name":"Applied Geochemistry","volume":"191 ","pages":"Article 106534"},"PeriodicalIF":3.4000,"publicationDate":"2025-08-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"LIBS as a tool for Li-pegmatite exploration and prospect evaluation: Soil mica and soil analysis from the Carolina Tin-Spodumene Belt\",\"authors\":\"Russell S. Harmon , P. Louis Lu , Adam C. Curry , Russell M. Murray , Daniel D. Richter\",\"doi\":\"10.1016/j.apgeochem.2025.106534\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Lithium is an essential element along the pathway to a high-technology future. Being able to efficiently explore for Li deposits and fully assess prospects is necessary to reduce exploration costs, shorten time between discovery and production, and minimize environmental impacts of exploration and production. Laser-induced breakdown spectroscopy (LIBS) is an analytical technology for real-time geochemical analysis in both the laboratory and the field that has potential to enhance current capabilities for Li pegmatite exploration and prospect evaluation. This study was conducted in a portion of the Carolina Tin-Spodumene Belt in Gaston County, NC at one of the largest Li-pegmatite prospects in the USA. Analysis by handheld LIBS first observed the same Li–K/Rb systematics for individual mica grains in soil as for mica in both barren quartz-feldspar and spodumene-bearing pegmatites, suggesting that soil mica analysis might be used for geochemical vectoring towards mineralized pegmatite. The contents of Li, K, and Rb in Bt horizons of residual Kanhapludult soil were determined in the field from matrix-matched LIBS calibrations along five transects across an area where a subsurface spodumene pegmatite dike was known from drilling to be present at ∼15-m depth. Unlike the situation for mica, no systematic variation was observed for soil K and Rb abundances, with K/Rb ratios not reflective of the presence of subsurface mineralization. By contrast, soil Li content spiked sharply where a sampling transect passed directly over the spodumene mineralized dike. It was also noted that soil Li abundances are significantly elevated across the domain of the Carolina Tin-Spodumene Belt of pegmatite mineralization on a regional scale compared to other Piedmont and Coastal Plain soils. Thus, there is potential for rapid soil geochemical analysis by LIBS in Li-pegmatite exploration at both local and regional spatial scales.</div></div>\",\"PeriodicalId\":8064,\"journal\":{\"name\":\"Applied Geochemistry\",\"volume\":\"191 \",\"pages\":\"Article 106534\"},\"PeriodicalIF\":3.4000,\"publicationDate\":\"2025-08-25\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Applied Geochemistry\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0883292725002574\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Geochemistry","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0883292725002574","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
LIBS as a tool for Li-pegmatite exploration and prospect evaluation: Soil mica and soil analysis from the Carolina Tin-Spodumene Belt
Lithium is an essential element along the pathway to a high-technology future. Being able to efficiently explore for Li deposits and fully assess prospects is necessary to reduce exploration costs, shorten time between discovery and production, and minimize environmental impacts of exploration and production. Laser-induced breakdown spectroscopy (LIBS) is an analytical technology for real-time geochemical analysis in both the laboratory and the field that has potential to enhance current capabilities for Li pegmatite exploration and prospect evaluation. This study was conducted in a portion of the Carolina Tin-Spodumene Belt in Gaston County, NC at one of the largest Li-pegmatite prospects in the USA. Analysis by handheld LIBS first observed the same Li–K/Rb systematics for individual mica grains in soil as for mica in both barren quartz-feldspar and spodumene-bearing pegmatites, suggesting that soil mica analysis might be used for geochemical vectoring towards mineralized pegmatite. The contents of Li, K, and Rb in Bt horizons of residual Kanhapludult soil were determined in the field from matrix-matched LIBS calibrations along five transects across an area where a subsurface spodumene pegmatite dike was known from drilling to be present at ∼15-m depth. Unlike the situation for mica, no systematic variation was observed for soil K and Rb abundances, with K/Rb ratios not reflective of the presence of subsurface mineralization. By contrast, soil Li content spiked sharply where a sampling transect passed directly over the spodumene mineralized dike. It was also noted that soil Li abundances are significantly elevated across the domain of the Carolina Tin-Spodumene Belt of pegmatite mineralization on a regional scale compared to other Piedmont and Coastal Plain soils. Thus, there is potential for rapid soil geochemical analysis by LIBS in Li-pegmatite exploration at both local and regional spatial scales.
期刊介绍:
Applied Geochemistry is an international journal devoted to publication of original research papers, rapid research communications and selected review papers in geochemistry and urban geochemistry which have some practical application to an aspect of human endeavour, such as the preservation of the environment, health, waste disposal and the search for resources. Papers on applications of inorganic, organic and isotope geochemistry and geochemical processes are therefore welcome provided they meet the main criterion. Spatial and temporal monitoring case studies are only of interest to our international readership if they present new ideas of broad application.
Topics covered include: (1) Environmental geochemistry (including natural and anthropogenic aspects, and protection and remediation strategies); (2) Hydrogeochemistry (surface and groundwater); (3) Medical (urban) geochemistry; (4) The search for energy resources (in particular unconventional oil and gas or emerging metal resources); (5) Energy exploitation (in particular geothermal energy and CCS); (6) Upgrading of energy and mineral resources where there is a direct geochemical application; and (7) Waste disposal, including nuclear waste disposal.