lithophile element sentence in Hindi
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- The lithophile elements include : W and the lanthanides.
- Lithophile elements mainly consist of the highly reactive metals of the s-and f-blocks.
- The less soluble lithophile elements are concentrated on ancient continental shields where all soluble minerals have been weathered.
- Besides having compositional effects on the upper mantle by replenishing the large-ion lithophile elements, volcanism affects the plate movement.
- Most lithophile elements form very stable ions with an electron configuration of a noble gas ( sometimes with additional f-electrons ).
- This is because, whereas lithophile elements require energy-intensive electrolysis for extraction, chalcophiles can be easily extracted by reduction with plate collisions.
- Boninites with 10 18 % MgO tend to have higher large-ion lithophile elements ( LILE : Ba, Rb, Sr ) than komatiites.
- Their strong affinity for oxygen causes lithophile elements to associate very strongly with silica, forming relatively low-density minerals that thus float to the crust.
- Because of their strong affinity for oxygen, most lithophile elements are enriched in the Earth's crust relative to their abundance in the solar system.
- Lithophile elements are those that remain on or close to the surface because they combine readily with oxygen, forming compounds that do not sink into the core.
- Because these sulfides are much denser than the silicate minerals formed by lithophile elements, chalcophile elements separated below the lithophiles at the time of the first crystallisation of the Earth's crust.
- After dehydration, solute-rich fluids are released from the slab and metasomatise the overlying mantle wedge of MORB-like asthenosphere, enriching it with volatiles and large ion lithophile elements ( LILE ).
- Manganese, iron and molybdenum " do " form strong bonds with oxygen but in the free state ( as they existed on the primitive Earth when free oxygen did not exist ) can mix so easily with iron that they do not concentrate in the siliceous crust as do true lithophile elements.
- One group includes elements having large ionic radius, such as potassium, rubidium, caesium, strontium, barium ( called "'LILE "', or large-ion lithophile elements ), and the other group includes elements of large ionic valences ( or high charges ), such as zirconium, niobium, hafnium, rare earth elements ( REE ), thorium, uranium and tantalum ( called "'HFSE "', or high field strength elements ).
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