basaltic magma वाक्य
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- The solubility of water is higher in rhyolite than in basaltic magma.
- Eruptions of basaltic magma often transition between effusive and explosive eruption patterns.
- However early formed crystals in basaltic magma can also form harzburgite within the mantle.
- Partial melting of spinel lherzolite is one of the primary sources of basaltic magma.
- Basaltic magma rose along these fractures to create effusive eruptions.
- Basaltic magma is formed from lherzolites in the mantle.
- No non-basaltic magmas have been erupted at Longgang.
- The multiple andesite flows were probably derived from basaltic magma by the crystallization of the magma material.
- The second time, between 9 225 million years ago, started with basaltic magma eruptions, and ended with pyroclastic eruptions.
- Water released from the subducting plate triggers the formation of basaltic magmas that are then injected into the crust.
- The andesites and dacites may have formed from basaltic magma by asthenospheric mantle, lithospheric components may have contributed however.
- During volcanic activity a fibrous material may be drawn by vigorous wind from molten basaltic magma called Pele's hair.
- Nakhlites are igneous rocks that are rich in augite and were formed from basaltic magma about 1.3 billion years ago.
- Many researchers have argued that anorthosites are the products of basaltic magma, and that mechanical removal of mafic minerals has occurred.
- As the oceanic Yangtze Craton subducted under the continental North China Craton, magmatic activities result in the formation of hydrated mafic basaltic magma.
- Possibly, the magma chamber of stage I had almost solidified when the injection of basaltic magma at depths of over triggered a remelting.
- The key factors in generating a Hawaiian eruption are basaltic magma and a low percentage of dissolved water ( less than one percent ).
- A typical theory is as follows : partial melting of the mantle generates a basaltic magma, which does not immediately ascend into the crust.
- Where hotspots occur under continental crust, basaltic magma is trapped in the less dense continental crust, which is heated and melts to form rhyolites.
- Volcanic activity was most likely triggered by the injection of basaltic magma into the felsic magma chamber days or weeks before the actual eruption.
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