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О температуре солидуса пород мантии
The accordance of the solidus temperature (Ts) of mantle rocks to a complex of petrological and geophysical data is considered. It is proved that the relation Ts = 1013 + 3.914H − 0.0037H2 , where H is the depth in km, corresponds to this information and can be used for the construction of model...
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| Main Authors: | , |
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| Format: | Article |
| Language: | Russian |
| Published: |
Видавничий дім "Академперіодика" НАН України
2007
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| Subjects: | |
| Online Access: | http://dspace.nbuv.gov.ua/handle/123456789/3170 |
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| Summary: | The accordance of the solidus temperature (Ts) of mantle rocks to a complex of petrological and
geophysical data is considered. It is proved that the relation Ts = 1013 + 3.914H − 0.0037H2
,
where H is the depth in km, corresponds to this information and can be used for the construction
of models of the deep processes and the sources of anomalies of physical fields. |
|---|