Synthesis of Pyrope Garnet with High Samarium Content at 5 GPa and 1300 °C
УДК 539.89.:620.22
Abstract
In natural garnets associated with diamonds, an increased content of "light" rare-earth elements, especially samarium, is often noticed. There are various estimates of the composition of the crystallization medium. Experimental data on the synthesis of Cr-rich garnets containing rare-earth elements are still scarce. The experiments were carried out on a multi-anvil apparatus of the “split-sphere” type (BARS) at a pressure of 5 GPa and a temperature of 1300 °С. The high pressure cell was made of Zr02 and CaO. A tubular graphite element was used as a heater. The measurement error of pressure and temperature was ± 0.2 GPa and ± 25 °С. The starting materials for the experiments were natural serpentine-antigorite, chromium spinel, and corundum. As a result of the experiments, pyrope crystals with a high content of samarium were synthesized in the range of 0.77 to 2.34 wt% Sm2O3. The study demonstrates that the interaction of components in the serpentine-chromite-corundum-Sm system in the presence of fluid leads to crystallization of pyrope garnet with samarium content exceeding the values known for natural garnets associated with diamond.
Downloads
Metrics
References
Shimizu N., Sobolev N.V. Young peridotitic diamonds from the Mir kimberlite pipe. Nature, 1995. Vol. 375.
Stachel T., Viljoen K.S., Brey G., Harris J.W. Metasomatic processes in lherzolitic and harzburgitic domains of diamondiferous lithospheric mantle: REE in garnets from xenoliths and inclusions in diamonds. Earth and Planetary Science Letters, 1998. Vol. 159.
Stachel Т., Aulbach S., Brey G.P., Harris J.W, Leost I., Tappert R., Viljoen K.S. The trace element composition of silicate inclusions in diamonds: a review. Lithos, 2004. Vol. 77 (1-4).
Gibson S.A. On the nature and origin of garnet in highly-refractory Archean lithospheric mantle: constrains from garnet exsolved in Kaapvaal craton orthopyroxenes. Mineralogical Magazine, 2017. Vol. 81 (4).
Chepurov A.A., Faryad S.W., Agashev A.M., Strnad L., Jedlicka R., Turkin A.I., Mihaljevic M., Lin VV Experimental crystallization of a subcalcic Cr-rich pyrope in the presence of REE-bearing carbonatite. Chemical Geology, 2019. Vol. 509.
Bobrov A.V, Litvin Yu.A., Kuzyura A.V, Dymshits A.M., Jeffries T., Bindi L. Partitioning of trace elements between Na-bearing majoritic garnet and melt at 8.5 GPa and 1500-1900 °C. Lithos, 2014. Vol. 189.
Лин В.В., Чепуров A.A., Жимулев Е.И. Особенности строения и состава гранатсодержащих образцов, синтезированных в системе с самарием при высоком давлении и температуре // Известия АлтГУ 2021. № 4. С. 43-46.
Chepurov A.I., Zhimulev E.I., Chepurov A.A., Sonin VM. Where did the largest diamonds grow? The experiments on percolation of Fe-Ni melt through olivine matrix in the presence of hydrocarbons. Lithos, 2021. Vol. 404-405.
Ulmer P., Trommsdorff V. Serpentine stability to mantle depths and subduction-related magmatism. Science, 1995. Vol. 268. № 5212.
Соболев Н.В., Лаврентьев Ю.Г., Поспелова Л.Н., Соболев Е.В. Хромовые пиропы из алмазов Якутии // Доклады Академии наук СССР. 1969. Т. 189. № 1.
Соболев Н.В., Ефимова Э.С., Логвинова А.М., Суходольская О.В., Солодова Ю.П. Распространенность и состав минеральных включений в крупных алмазах Якутии // Доклады Академии наук. 2001. Т. 376. № 3.
Copyright (c) 2023 Владимир Валерьевич Лин , Алексей Анатольевич Чепуров , Егор Игоревич Жимулев , Александр Иванович Туркин
This work is licensed under a Creative Commons Attribution 4.0 International License.
Izvestiya of Altai State University is a golden publisher, as we allow self-archiving, but most importantly we are fully transparent about your rights.
Authors may present and discuss their findings ahead of publication: at biological or scientific conferences, on preprint servers, in public databases, and in blogs, wikis, tweets, and other informal communication channels.
Izvestiya of Altai State University allows authors to deposit manuscripts (currently under review or those for intended submission to Izvestiya of Altai State University) in non-commercial, pre-print servers such as ArXiv.
Authors who publish with this journal agree to the following terms:
- Authors retain copyright and grant the journal right of first publication with the work simultaneously licensed under a Creative Commons Attribution License (CC BY 4.0) that allows others to share the work with an acknowledgement of the work's authorship and initial publication in this journal.
- Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgement of its initial publication in this journal.
- Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See The Effect of Open Access).