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作 者:HEHuaiyu WANGFei SANGHaiqing WANGYinglan BovenAriel ZHURixiang
机构地区:[1]nstituteofGeologyandGeophysics,ChineseAcademyofSciences,Beijing100029,China [2]LaboratoryofGeochronology,VrijeUniversiteitBrussel,Pleinlaan2,1050Brussels,Belgium
出 处:《Chinese Science Bulletin》2004年第18期1949-1952,共4页
摘 要:Ultra-Violet Laser Ablation Microprobe (UV-LAMP) extraction technique enables the direct investigation of Ar-Ar age profile in crystals, and yields more information on rates and durations of geological process than conven-tional single time snapshots. Phlogopite flakes from lampro-phyre at Pishan dyke in western Kunlun were dated by using an UV laser (l = 213 nm) microprobe with spot analyses. The results show good agreement with those from the conven-tional 40Ar/39Ar step heating experiments. This indicates that the Ar isotopes are distributed homogenously in the phlogopite and the UVLAMP can be a powerful tool in the study of thermal history.Ultra-Violet Laser Ablation Microprobe (UV-LAMP) extraction technique enables the direct investigation of Ar-Ar age profile in crystals, and yields more information on rates and durations of geological process than conven-tional single time snapshots. Phlogopite flakes from lampro-phyre at Pishan dyke in western Kunlun were dated by using an UV laser (l = 213 nm) microprobe with spot analyses. The results show good agreement with those from the conven-tional 40Ar/39Ar step heating experiments. This indicates that the Ar isotopes are distributed homogenously in the phlogopite and the UVLAMP can be a powerful tool in the study of thermal history.
关 键 词:激光探针 测量 ^40AR/^39AR 金云母 煌斑岩
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