EXPERIMENTAL AND THEORETICAL MODELING OF DIAMONDIFEROUS PLUMES
We consider thermochemical mantle plumes with thermal power 1.6·1010 W<N<2.7·1010 W (relative thermal power 1.15<Ka<1.9) as plumes with an intermediate thermal power. Such plumes are formed at the core–mantle boundary beneath cratons in the absence of horizontal free‐conv...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Institute of the Earth's crust, Siberian Branch of RAS
2019-06-01
|
| Series: | Geodinamika i Tektonofizika |
| Subjects: | |
| Online Access: | https://www.gt-crust.ru/jour/article/view/840 |