Chemistry of the mantle - Universiteit Utrecht

Chemistry of the mantle - Universiteit Utrecht

Chemistry of the mantle Physical processes (subduction, convection) affect the chemistry of the mantle. Chemical processes occur mainly through melting. Resulting chemical differences are acted upon by physical processes.

Interaction physical-chemical state of the mantle. Mantle and crust contain minor or trace concentrations of virtually all elements. Comparison of concentrations shows that much of the mantle is a residue (extraction of

atmosphere, ocean continental crust) compared to primitive meteorites. Information on time scales is obtained from radioactive decay. Chemical heterogeneities (different magma sources) are more than 2 Gyears old.

Geochemical picture of the mantle 1. The mantle is depleted in those elements that are found to be concentrated in crust, hydrosphere and atmosphere, relative to the original composition of the mantle. 2. Some material from crust, hydrosphere and

atmosphere is re-injected into the mantle. 3. The depletion and re-enrichment are not uniform. 4. The shallowest mantle sampled by MORB, is the most depleted. 5. OIB, arising from melting of mantle plumes

(deeper), show less depletion and more variability. 6. Chemical heterogeneities are old (1-2 Gy) 7. All of the mantle that has been sampled has been modified from its original composition. 8. At least 5 reservoirs: continental crust (enriched), continental root (depleted),

MORB, OIB and IAB (+water = CC) Some definitions Major element composition: Mg-Fe silicates and lesser amounts of Al and Ca These elements determine the structure of the main minerals. Other elements have to fit in.

Less abundant elements: ores (solid solution in major minerals) Trace elements (much less than 1 %). Incompatible (trace) elements tend to go into the liquid phase. Mg2+ can easily be replaced Ni2+ in olivine

U4+ and U6+ are much larger and have difficulty to fit into olivine Ni is compatible and U is incompatible If part of the mantle melts, the liquid tends to remove the incompatible elements. Elements that tend to partition into a liquid iron

phase are called siderophile. Elements that tend to partition into sulphide phases are called chalcophile Mantel geochemistry largely exploits the radioactive decay of certain isotopes. The decay changes the isotope composition of parent and

daughter elements Characteristic fingerprints of melts Dating Fundamental relationship: D=D0+P0(1-e-t/), t is time and is T1/2/ln2 where T1/2 is the half life of the parent

Observations Trace elements The incompatible elements are concentrated in melts (plot above the primitive line) MORB: if is assumed that the melt is not modified during ascent, the MORB source can

be inferred. e.g. 10 % melting and most incompatible elements go into melt: VmantleCmantle = VmeltCmelt = 0.1 VmantleCmelt

Cmantle=Cmelt/10 MORB source depleted in Correction less secure for OIB 5 % melting ? correction of 20 EM-1, HIMU source enriched with respect to primitive mantle

Hawaii (more melting ?) close to primitive BUT all plume sources are less depleted than MORB. Continental crust strongly enriched, but difficult to understand because very heterogeneous. But remarkable correlation between CC and

MORB source: the enrichments of trace elements in the CC are to a first approximation complementary to their depletions in the MORB source. Primitive mantle MORB source + CC ??? Exceptions are Nb, Pb recycling

Observations Refractory element isotopes Melting has no effect on isotope ratios direct information on the source. MORB and OIB show similar variations, but the MORB signal is muted.

Observations Noble gas isotopes Noble gases are useful because they are unreactive (no recycling into mantle from atmosphere, no dissolution into melt minerals)

23 different isotopes e.g. He3 is primordial He4 from decay of U and Th Crust: low He3/He4 high radioactivity in CC Mantle: high He3/He4 also high radioactivity means a lot of He3 is still being outgassed.

MORB uniform He3 OIB tap sources with different concentrations of He3, but always higher than MORB PHEM Interpretation MORB shallow (passive source) depends on our understanding of the dynamics of plates and

plumes OIB deep (active source) again dynamics Sources have different signatures, but no information on topology of reservoirs Ages from isochrones Mass balance: MORB 40-94 %, OIB rest or some primitive mantle

Recently Viewed Presentations

  • Decolonizing Food, Consciousness, Culture and Community

    Decolonizing Food, Consciousness, Culture and Community

    Decolonize? Yes! Colonialism destroys the autonomy of communities for self determination around food, health, economy, public policy, livelihood. Decolonizing is a necessary aspect of the food sovereignty approach, which is not so well established in the U.S. or "global north"...
  • 1-MVA-4A-GrowOffice-CloudIntro

    1-MVA-4A-GrowOffice-CloudIntro

    250k customers. $1.5. billion. 2. 00. million licenses. Microsoft Cloud Growth FY14. We've come a long way with our cloud business coupled with incredible growth with Windows 8 fueling what is just the beginning of our pathway toward leadership with...
  • Physiology of Aging: Clinical Aspects

    Physiology of Aging: Clinical Aspects

    Good Luck in Your Future Careers GO BEARS!!! * Joint Arthritis Joint Stiffness loss of cartilage loss of joint contour angular deformities Synovial membrane less elastic as are adjacent ligament structure with less movement-joint (ligaments) contract to position Hyaline vs...
  • Teaching English - Narr

    Teaching English - Narr

    Teaching one standard language as a global tool of empowerment neglects the values of different varieties and different groups in a multicultural world. ... 2.5 Sociolinguistic, Sociocultural, and Interactionist Approaches: the social agent.
  • Diapositiva 1 - dspace.espol.edu.ec

    Diapositiva 1 - dspace.espol.edu.ec

    diagnostico, planificacion estratÉgica y diseÑo de una nueva estructura organizacional orientada a procesos, dentro de la empresa comercial "almacenes juanito"
  • Georgias History: World War I  2014 Brain Wrinkles

    Georgias History: World War I 2014 Brain Wrinkles

    America's entry into the war gave the Allies the . extra power . they needed to defeat the Central Powers. In . November 11, 1918, the Central Powers . surrendered. to the Allies and . signed an armistice . that...
  • Teaching new vocabulary - liceoberard.scuole.vda.it

    Teaching new vocabulary - liceoberard.scuole.vda.it

    CLIL Use flashcards, actions or objects Children need to repeat after the teacher (chorally/individually) Voice needs to vary (whisper/loud/high pitch/low pitch) Children can respond in their own way or copy your action Clap out the syllables and stress on words.
  • Multi fetal pregnancy

    Multi fetal pregnancy

    In the name of God