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Flashcards

ES201

Nilesh Mayank Inglês 16 flashcards

Flashcards do conjunto (16)

  1. 1proportions of the dominant components of the condensate?early condensates or refractories-- 5%
    metals-- 20%
    silicates-- 40%
  2. 2relationship between basalts and the mantle indicateMantle samples with the most primitive compositions will be those that have
    NOT experienced the extraction of basaltic magma
  3. 3U, Th and K are incompatible elements (i.e. they are preferentially partitioned into silicate liquids) where will they be concentrated?The elements U, Th and K (and their radiogenic isotopes) are particularly
    concentrated in the silicate-dominated outer layers of the Earth, and in
    particular within the continental crust.
  4. 4What process raised siderophile element abundances in the silicate mantle following core formation?Continued accretion of meteoritic materials from new impacts of meteorites with chondritic proportions of the siderophile elements.
  5. 5HighlandAnorthosite (rich in PLAGIOCLASE FELDSPAR 90%; 10% MAFIC MINERALS)
    ~ 4.4 Ga
  6. 6MariaBASALTIC in composition
    ~ 3.8-4.2 Ga
  7. 7Achondrites-reminiscent of terrestrial Igneous rocks.
  8. 8Mantle -- compositionilicates composition-
    achondrite-rich in Mg
  9. 9xenoliths --green colour contrast with the grey black colour of the host volcanic rocks.
  10. 10Peridotites -rich in minerals olivine and pyroxene silicates rich in magnesium and iron.
    density 3200 kg m−3
  11. 11Ophiolites --obducted oceanic crust.
    edimentary rocks overlie rocks of basaltic composition, overlie peridotite.
  12. 12Siderophiles --found in the metallic phase.
    2.0 < E < 2.4
    D >1
    compatible
  13. 13lithophiles --bond with oxygen, especially in silicate or oxide
    E <1.6
    D <1
    incompatible
  14. 14Chalcophiles --form covalent bonds with elements such as S.
    1.6 < E < 2.0
  15. 15Upper Crust -- Granodioritegranite containing plagioclase and alkali feldspar 1:1 & 20% quartz
  16. 16Lower Crust -- Granulitesmetamorphic rocks that have been subjected to high pressures and temperatures lost volatile components and their mineralogy is plagioclase feldspar, pyroxenes and garnets

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Basic Introduction
Criado por
Nilesh Mayank
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