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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >U-Pb geochronology and Sr/Nd isotope compositions of groundmass perovskite from the newly discovered Jurassic Chidliak kimberlite field, Baffin Island, Canada
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U-Pb geochronology and Sr/Nd isotope compositions of groundmass perovskite from the newly discovered Jurassic Chidliak kimberlite field, Baffin Island, Canada

机译:来自加拿大巴芬岛侏罗纪奇德利亚克金伯利岩田的地钙钛矿的U-Pb年代学和Sr / Nd同位素组成

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摘要

We report the U-Pb age and Sr/Nd isotope composition for perovskite isolated from forty six kimberlite samples located in the newly discovered Chidliak field on Baffin Island, Canada. The minimum duration of kimberlite magmatism in this field was 17.9 m.y. from 157.0 to 139.1 Ma and represents a new Jurassic kimberlite field in NE Canada. The most prolific period of kimberlite magmatism occurred between 152 and 142 Ma (80% of dated kimberlites). Kimberlitic perovskite from these intrusions display a range in Sr-87/Sr-86 (0.7043 to 0.7030) and epsilon NdT values (+3.9 to -0.4), overlapping the isotopic field previously defined for southern African Group I kimberlites.
机译:我们从位于加拿大巴芬岛新发现的奇德里亚克油田的四十六个金伯利岩样品中分离出来的钙钛矿报告了钙钛矿的U-Pb年龄和Sr / Nd同位素组成。该区域金伯利岩岩浆作用的最小持续时间为17.9m.y。从157.0到139.1 Ma,代表加拿大东北部新的侏罗纪金伯利岩田。金伯利岩岩浆作用的最多产期发生在152至142 Ma之间(占过时金伯利岩的80%)。来自这些侵入的金伯利特钙钛矿显示出Sr-87 / Sr-86的范围(0.7043至0.7030)和εNdT值(+3.9至-0.4),与先前为南部非洲I类金伯利岩定义的同位素场重叠。

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