Andradite-Morimotoite Garnets as Promising U-Pb Geochronometers for Dating Ultrabasic Alkaline Rocks

被引:20
作者
Salnikova, E. B. [1 ]
Stifeeva, M. V. [1 ]
Nikiforov, A. V. [2 ]
Yarmolyuk, V. V. [2 ]
Kotov, A. B. [1 ]
Anisimova, I. V. [1 ]
Sugorakova, A. M. [3 ]
Vrublevskii, V. V. [4 ]
机构
[1] Russian Acad Sci, Inst Precambrian Geol & Geochronol, St Petersburg 199034, Russia
[2] Russian Acad Sci, Inst Geol Ore Deposits Petrog Mineral & Geochem, Moscow 119017, Russia
[3] Russian Acad Sci, Siberian Branch, Tuva Inst Complex Explorat Nat Resources, Kyzyl 667007, Russia
[4] Natl Res Tomsk State Univ, Tomsk 634050, Russia
基金
俄罗斯科学基金会; 俄罗斯基础研究基金会;
关键词
GEOCHRONOLOGY; EXTRACTION; URANIUM; AGE;
D O I
10.1134/S1028334X18060168
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
U-Pb geochronological studies of garnet of the andradite-morimotoite series and Sm-Nd geochronological studies of this garnet and apatite from the Chikskii Massif (Tuva-Mongolia microcontinent) were carried out. The garnet studied is characterized by relatively high concentrations of U (14-16 ppm) and by a low level of common Pb (Pb-N/Pb-t = 0.07-0.1). The concordia age of garnet is 492 +/- 2 Ma (MSWD = 0.01, probability 92%) and matches within the error with the Sm-Nd age determined by the isochrone for apatite, garnet, and bulk rock (489 +/- 9 Ma, MSWD = 0.86). This allows us to consider calcic garnets of the andradite-morimotoite series as promising mineral geochronometers for U-Pb dating of ultrabasic alkaline rocks.
引用
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页码:778 / 782
页数:5
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