S. Turner , A. Dosseto , P.O. Suresh , M. Turner , H. Handley , P. Hesse
{"title":"沿澳大利亚东部从西向东的样带和弗林德斯山脉的一些基岩取样的尘埃U-Th同位素数据","authors":"S. Turner , A. Dosseto , P.O. Suresh , M. Turner , H. Handley , P. Hesse","doi":"10.1016/j.ringeo.2022.100016","DOIUrl":null,"url":null,"abstract":"<div><p>In this communication we present Uranium-Thorium (U-Th) isotope data for surficial dusts sampled along a west to east transect in eastern Australia and some selected bedrock samples from the Flinders Ranges near the western end of the transect. The dusts have lost <sup>238</sup>U and <sup>234</sup>U within the last 350 kyr implying a combination of chemical (bulk U loss) and physical (recoil loss of <sup>234</sup>U) weathering. Near-surface bedrock is not always in U-Th isotope secular equilibrium as commonly assumed in studies of weathering, erosion and soil production.</p></div>","PeriodicalId":101085,"journal":{"name":"Results in Geochemistry","volume":"6 ","pages":"Article 100016"},"PeriodicalIF":0.0000,"publicationDate":"2022-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S2666277922000028/pdfft?md5=ae11266c7bf706eda9c0bf5d5b602b52&pid=1-s2.0-S2666277922000028-main.pdf","citationCount":"0","resultStr":"{\"title\":\"U-Th isotope data for dust sampled along a west to east transect in eastern Australia and some bedrock from the Flinders Ranges\",\"authors\":\"S. Turner , A. Dosseto , P.O. Suresh , M. Turner , H. Handley , P. Hesse\",\"doi\":\"10.1016/j.ringeo.2022.100016\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>In this communication we present Uranium-Thorium (U-Th) isotope data for surficial dusts sampled along a west to east transect in eastern Australia and some selected bedrock samples from the Flinders Ranges near the western end of the transect. The dusts have lost <sup>238</sup>U and <sup>234</sup>U within the last 350 kyr implying a combination of chemical (bulk U loss) and physical (recoil loss of <sup>234</sup>U) weathering. Near-surface bedrock is not always in U-Th isotope secular equilibrium as commonly assumed in studies of weathering, erosion and soil production.</p></div>\",\"PeriodicalId\":101085,\"journal\":{\"name\":\"Results in Geochemistry\",\"volume\":\"6 \",\"pages\":\"Article 100016\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2022-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://www.sciencedirect.com/science/article/pii/S2666277922000028/pdfft?md5=ae11266c7bf706eda9c0bf5d5b602b52&pid=1-s2.0-S2666277922000028-main.pdf\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Results in Geochemistry\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S2666277922000028\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Results in Geochemistry","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2666277922000028","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
U-Th isotope data for dust sampled along a west to east transect in eastern Australia and some bedrock from the Flinders Ranges
In this communication we present Uranium-Thorium (U-Th) isotope data for surficial dusts sampled along a west to east transect in eastern Australia and some selected bedrock samples from the Flinders Ranges near the western end of the transect. The dusts have lost 238U and 234U within the last 350 kyr implying a combination of chemical (bulk U loss) and physical (recoil loss of 234U) weathering. Near-surface bedrock is not always in U-Th isotope secular equilibrium as commonly assumed in studies of weathering, erosion and soil production.