NatureSir Norman Lockyer Macmillan Journals Limited, 2007 |
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Zadetki 1–3 od 11
Stran 55
... magma flow rates , producing changes in pressure and implosion and shattering of country rocks ) . Mitchell3 suggested that no single process could be responsible for the formation of the complex structure of kimberlites and diatremes ...
... magma flow rates , producing changes in pressure and implosion and shattering of country rocks ) . Mitchell3 suggested that no single process could be responsible for the formation of the complex structure of kimberlites and diatremes ...
Stran 56
... magma Rise speeds a few tens of metres per second Sharp pressure decrease Magma rise ~ 20 m s - 1 Gas rise CO2 >> 600 m s - 1 fluid Foam rise averages ~ 300 m s - 1 Magma- filled dyke e Stage 4 Magma f Stage 4 Magma g Stage 5 Becomes ...
... magma Rise speeds a few tens of metres per second Sharp pressure decrease Magma rise ~ 20 m s - 1 Gas rise CO2 >> 600 m s - 1 fluid Foam rise averages ~ 300 m s - 1 Magma- filled dyke e Stage 4 Magma f Stage 4 Magma g Stage 5 Becomes ...
Stran 303
... magma erupted at the Earth's surface is the end product of a complex series of processes , beginning with partial melting and melt extraction from a mantle source and ending with fractional crystallization and crustal assimilation at ...
... magma erupted at the Earth's surface is the end product of a complex series of processes , beginning with partial melting and melt extraction from a mantle source and ending with fractional crystallization and crustal assimilation at ...
Vsebina
ARTICLES | 53 |
LETTERS | 64 |
Chemical characterization of element 112 | 72 |
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