| Plural | magmas |
magma chamber
magma chamber
The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.
Matukio ya metallogenic yalitokea kutoka kwa magma ya basalti ya alkali ya miguu, na uchunguzi wa pulsatory ulikuwa mali ya muhimu ya kondishoni ya metallogenic ya mafuta.
The magma of porphyritic moyite-monzogranite series in the middle stage mainly originated from the lower crust, being the product of collision-orogeny.
Magma ya serikali ya moyite-monzogranite ya porphyritic katika mipangi ya mwinga ilihusika kwa asili ya kichwa chini, inayotumia matokeo ya collision-orogeny.
Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
Kwa makumbi ya modeli ya crystallization ya fractional, uunganishaji wa magma ya granit ya mafuta ya Fluorine ni njia muhimu ya kujenga pegmatite na pegmatite type deposit.
Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.
Kwa hiyo, kwa madini kuchambishwa kwenye miamba mingine, wakati kuna aina zote za mwanzo na xenolith, magma, mantle na kadhalika, umri wa tukio fulani unaweza kupatikana.
The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.
Majeni ya matokeo yana miongo ya differential metasomatism katika magma ya mwinga, prosesi ya hydrothermal ya pneumatolytic, prosesi ya pegmatite, matokeo ya mabaki na matokeo ya placer.
The volcano erupted, spewing hot magma everywhere.
Jiromo lililipaka, kuvua magma ya mafuta kila wanao.
Geologists study the composition and behavior of magma.
Wajisiti wanaangalia ujumbe na uwekwa wa magma.
Magma can solidify to form igneous rocks like granite.
Magma inaweza kushikamkama kujenga roki ya igneous kama granite.
The magma chamber beneath the volcano is expanding.
Kichwa cha magma chini ya jiromo kinaendelea kushuka.
Magma can reach temperatures of over 1,000 degrees Celsius.
Magma inaweza kusafiri kwa mizani zaidi ya 1,000 daraja ya Celsius.
The cooling of magma leads to the formation of crystals.
Ukamwangia wa magma hujengwa kwa matokeo ya mizani.
Magma is a mixture of molten rock, gases, and solids.
Magma ni mizani ya mafuta ya mafuta, mafuta na mizani.
Magma rising to the surface can trigger volcanic eruptions.
Magma inayotembea kwa mizani ya mafuta inaweza kujenga eruptions ya jiromo.
The movement of magma beneath the Earth's crust causes earthquakes.
Ukamwangia wa magma chini ya kichwa cha ardhi inajenga mizigo ya mizigo.
Minerals dissolved in magma can crystallize as it cools.
Mizani zilizosafiri katika magma inaweza kushikamkama kama yeye ukamwangia.
magma chamber
magma chamber
The metallogenic material was from deep alkalic basaltic magma, and the pulsatory invasion was the necessary metallogenic condition of the ore deposit.
Matukio ya metallogenic yalitokea kutoka kwa magma ya basalti ya alkali ya miguu, na uchunguzi wa pulsatory ulikuwa mali ya muhimu ya kondishoni ya metallogenic ya mafuta.
The magma of porphyritic moyite-monzogranite series in the middle stage mainly originated from the lower crust, being the product of collision-orogeny.
Magma ya serikali ya moyite-monzogranite ya porphyritic katika mipangi ya mwinga ilihusika kwa asili ya kichwa chini, inayotumia matokeo ya collision-orogeny.
Beside fractional crystallization model,liquid immiscibility of Fluorine-rich granite magma is an important mechanism to form pegmatite and pegmatite type deposit.
Kwa makumbi ya modeli ya crystallization ya fractional, uunganishaji wa magma ya granit ya mafuta ya Fluorine ni njia muhimu ya kujenga pegmatite na pegmatite type deposit.
Hence, for the minerals to be analyzed in some rocks, when there are all sorts of genesis with xenolith, magma, mantle and so on in them,the age of a certain single event can be respectively got.
Kwa hiyo, kwa madini kuchambishwa kwenye miamba mingine, wakati kuna aina zote za mwanzo na xenolith, magma, mantle na kadhalika, umri wa tukio fulani unaweza kupatikana.
The types of deposits basically are differential metasomatism in the later magma, pneumatolytic hydrothermal process, pegmatite process, residual deposits and placer deposits.
Majeni ya matokeo yana miongo ya differential metasomatism katika magma ya mwinga, prosesi ya hydrothermal ya pneumatolytic, prosesi ya pegmatite, matokeo ya mabaki na matokeo ya placer.
The volcano erupted, spewing hot magma everywhere.
Jiromo lililipaka, kuvua magma ya mafuta kila wanao.
Geologists study the composition and behavior of magma.
Wajisiti wanaangalia ujumbe na uwekwa wa magma.
Magma can solidify to form igneous rocks like granite.
Magma inaweza kushikamkama kujenga roki ya igneous kama granite.
The magma chamber beneath the volcano is expanding.
Kichwa cha magma chini ya jiromo kinaendelea kushuka.
Magma can reach temperatures of over 1,000 degrees Celsius.
Magma inaweza kusafiri kwa mizani zaidi ya 1,000 daraja ya Celsius.
The cooling of magma leads to the formation of crystals.
Ukamwangia wa magma hujengwa kwa matokeo ya mizani.
Magma is a mixture of molten rock, gases, and solids.
Magma ni mizani ya mafuta ya mafuta, mafuta na mizani.
Magma rising to the surface can trigger volcanic eruptions.
Magma inayotembea kwa mizani ya mafuta inaweza kujenga eruptions ya jiromo.
The movement of magma beneath the Earth's crust causes earthquakes.
Ukamwangia wa magma chini ya kichwa cha ardhi inajenga mizigo ya mizigo.
Minerals dissolved in magma can crystallize as it cools.
Mizani zilizosafiri katika magma inaweza kushikamkama kama yeye ukamwangia.
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