геология и разведка
Preview

Proceedings of higher educational establishments. Geology and Exploration

Advanced search

Khanneshin - the Afghan carbonatite volcano, discovered in the office

https://doi.org/10.32454/0016-7762-2017-4-85-88

Abstract

The pétrographie and mineralogical laboratory study of the rock samples and the analysis of the geological setting in the sites of their collection (South Afghanistan) allowed suggesting the presence of the carbonatite volcano there. This assumption has been proved: a young carbonatite volcano, the first one known for that moment in the Central Asia, has been discovered and investigated, as well as the minerals, associated with the volcano.

About the Author

B. Ya. Vikhter
Central Research Institute of Geological Prospecting for Base and Precious Metals
Russian Federation


References

1. Вихтер Б.Я., Еременко Г.К., Чмырев В.М. Молодой вулканогенный карбонатитовый комплекс в Афганистане // Советская геология, 1975, № 10, С. 107-116.

2. Вихтер Б.Я., Еременко Г.К., Чмырев В.М., Абдулла Д. Плиоцен-четвертичный вулканизм Афганистана // Известия АН СССР. Серия геолог. 1977. № 9. С. 29-42.

3. Еременко Г.К., Вихтер Б.Я., Чмырев В.М., Хамиди Хабибулла. Четвертичный вулканический карбона титовый комплекс в Афганистане // Докл. АН СССР. 1975. Т. 223, № 2, С. 427-430.

4. Lang H.D. Uber das Jungtertiaar und Quatar in Sud-Afghanistan // Bull. Afgh. Miner. Survey ( Kabul). 1971. № 5.

5. Tucker R.D., Belkin H.E., Schutz K.J. et al. A major licht rere-earth element (LREE) resource in the Khanneshin caronatite complex, Southern Afghanistan // Economic Geology. 2012. V. 107. N. 2. P. 197-208.


Review

For citations:


Vikhter B.Ya. Khanneshin - the Afghan carbonatite volcano, discovered in the office. Proceedings of higher educational establishments. Geology and Exploration. 2017;(4):85-88. (In Russ.) https://doi.org/10.32454/0016-7762-2017-4-85-88

Views: 444


Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.


ISSN 0016-7762 (Print)
ISSN 2618-8708 (Online)