{"title":"基于投影轨迹长度分析的磷灰石裂变径迹年龄谱","authors":"G.A. Wagner, E. Hejl","doi":"10.1016/0168-9622(91)90029-V","DOIUrl":null,"url":null,"abstract":"<div><p>Projected length analysis of surface tracks enables the calculation of length dispersive spectra of apatite fission track ages determined by the grain-population technique. Different <em>T</em>-<em>t</em> paths result in characteristic apparent age-spectra which reveal the low temperature ( < 140°C) history of rocks. The concept is successfully tested against geologic constraints.</p></div>","PeriodicalId":100231,"journal":{"name":"Chemical Geology: Isotope Geoscience section","volume":"87 1","pages":"Pages 1-9"},"PeriodicalIF":0.0000,"publicationDate":"1991-08-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0168-9622(91)90029-V","citationCount":"17","resultStr":"{\"title\":\"Apatite fission-track age-spectrum based on projected track-length analysis\",\"authors\":\"G.A. Wagner, E. Hejl\",\"doi\":\"10.1016/0168-9622(91)90029-V\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Projected length analysis of surface tracks enables the calculation of length dispersive spectra of apatite fission track ages determined by the grain-population technique. Different <em>T</em>-<em>t</em> paths result in characteristic apparent age-spectra which reveal the low temperature ( < 140°C) history of rocks. The concept is successfully tested against geologic constraints.</p></div>\",\"PeriodicalId\":100231,\"journal\":{\"name\":\"Chemical Geology: Isotope Geoscience section\",\"volume\":\"87 1\",\"pages\":\"Pages 1-9\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1991-08-16\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0168-9622(91)90029-V\",\"citationCount\":\"17\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chemical Geology: Isotope Geoscience section\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/016896229190029V\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Geology: Isotope Geoscience section","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/016896229190029V","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Apatite fission-track age-spectrum based on projected track-length analysis
Projected length analysis of surface tracks enables the calculation of length dispersive spectra of apatite fission track ages determined by the grain-population technique. Different T-t paths result in characteristic apparent age-spectra which reveal the low temperature ( < 140°C) history of rocks. The concept is successfully tested against geologic constraints.
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