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  2. Magmatism - Wikipedia

    en.wikipedia.org/wiki/Magmatism

    Magmatism. Geological map showing the Gangdese batholith, which is a product of magmatic activity about 100 million years ago. Magmatism is the emplacement of magma within and at the surface of the outer layers of a terrestrial planet, which solidifies as igneous rocks. It does so through magmatic activity or igneous activity, the production ...

  3. Magmatic underplating - Wikipedia

    en.wikipedia.org/wiki/Magmatic_underplating

    Entrapment (or 'stalling out') of magmas within the crust occurs due to the difference in relative densities between the rising magma and the surrounding rock. Magmatic underplating can be responsible for thickening of the crust when the magma cools. [1] Geophysical seismic studies (as well as igneous petrology and geochemistry) utilize the ...

  4. Live/Hhaï - Wikipedia

    en.wikipedia.org/wiki/Live/Hhaï

    Live/Hhaï (also known as Magma Live, Live Köhntark, and Hhaï Live) is the first live album and fifth album in total by French rock group Magma. It was recorded in Paris between the 1st and 5 June 1975 at the Taverne de l'Olympia, [2] and was first released in 1975. The album has been re-released many times: in 1975 on Utopia Records, in 1978 ...

  5. 1001° Centigrades - Wikipedia

    en.wikipedia.org/wiki/1001°_Centigrades

    1001° Centigrades, alternative title 2, is the second album by French rock band Magma, released on 5 October 1971. Future reissues use both titles as 2: 1001° Centigrades . The first track, "Rïah Sahïltaahk", was later re-recorded as a full-length studio album, Rïah Sahïltaahk, in 2014, as Christian Vander did not consider himself ...

  6. There was once an ancient ocean filled with magma on the moon ...

    www.aol.com/once-ancient-ocean-filled-magma...

    The magma ocean is likely to have existed for tens to hundred million years, Santosh Vadawale, a professor in the Physical Research Laboratory and lead author of the study, told ABC News.

  7. Crystal mush - Wikipedia

    en.wikipedia.org/wiki/Crystal_mush

    A crystal mush is magma that contains a significant amount of crystals (up to 50% of the volume) suspended in the liquid phase (melt). [1] As the crystal fraction makes up less than half of the volume, there is no rigid large-scale three-dimensional network as in solids. [2] As such, their rheological behavior mirrors that of absolute liquids.

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