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Interactions between slab melts and mantle wedge in
Archaean subductions:old and new views on TTG
Jean-François Moyen1 & Hervé Martin2
1- Univ. Claude-Bernard Lyon-I, France
2- Univ. Blaise-Pascal Clermont-Ferrand, France
Archaean TTG emplaced over a long period of time 2 Ga
From 4.5 to 2.5 Earth heat production decreased by about 3 times
Archaean TTG: mineralogy
quartz epidote
plagioclase biotite
« Grey gneisses »:
Orthogneisses of tonalitic and granodioritic composition
TTG define differentiation trends in Harker diagrams
At least one part of this differentiation is
due to fractional crystallization
Geochemical modelling for TTG parental magma
TTG source was basaltic:
Archaean tholeiites
Both garnet and hornblende were stable in the melting residue
Modern adakites analogues of Archaean TTG
Adakites are found only when young, hot lithosphere is subducted...
… i.e., when Archaean thermal conditions are (locally) recreated
Evolution of Mg# in TTG
• Fractional crystallization reduces Mg#
• For each period the higher Mg# represents TTG parental magma
• From 4.0 to 2.5 Ga Mg# regularly increased in TTG parental magmas
Evolution of Ni
and Cr in TTG
• Fractional crystallization reduces Ni and Cr contents
• For each period the higher Ni and Cr contents represent TTG parental magma
• From 4.0 to 2.5 Ga Ni and Cr contents regularly increased in TTG parental magmas
The MgO vs. SiO2 system
•MgO increases inTTG in course of time•SiO2 decreases inTTG in course of time
•Adakites have exactly the same evolution pattern as TTG
•For the same SiO2, experimental melts are systematically MgO poorer than TTG
•Mg, Ni and Cr enrichment(both in adakites and TTG)
•TTG are generated by
•Mg, Ni, Cr increased in course of time
•TTG source located under a mantle slice
•Degree on interactionincreases in course of time
PRELIMINARY CONCLUSIONS I
magma / mantle interaction
(reaction between peridotite and “slab melts”)
slab melting underplated basalt melting
degree on interaction increases
slab melting depth augments
Evolution of Sr in TTG
• Fractional crystallization reduces Sr contents
• For each period the higher Sr represents TTG parental magma
• From 4.0 to 2.5 Ga Sr regularly increased in TTG parental magmas
Evolution of
(Na2O + CaO)
and (Eu/Eu*) in TTG
• For each period the higher (Na2O + CaO) represent TTG parental magma
• From 4.0 to 2.5 Ga (Na2O + CaO) regularly increased in TTG parental magmas
• From 4.0 to 2.5 Ga positive Eu anomalies appear in TTG parental magmas
The Sr vs. (Na2O+CaO) system
•Sr and (Na2O+CaO) inTTG increase in course of time
•Adakites have exactly the same evolution pattern as TTG
•Sr content is directly correlated with stability of plagioclase in melting residue
•High Sr in TTG
PRELIMINARY CONCLUSIONS II
absence of residual plagioclase
diminution of residual plagioclase
Correlated with depth Shallow depth low Sr Great depth high Sr
Increase of melting depth in course of time
presence of residual plagioclase
•Sr and (Na2O+CaO) augmentation in TTG
Stability of plagioclaseResidual plagioclaseNo residual plagioclase
Sr and (Na2O+CaO) augmentation in TTG
Low Sr in TTG
High heat production High geothermal gradients Shallow depth slab melting
Plagioclase stable Sr poor TTG
Thin overlying mantle No or few magma/mantle interactions Low Mg-Ni-Cr TTG
Lower heat production Lower geothermal gradients Deep slab melting
Plagioclase unstable Sr-rich TTG
Thick overlying mantle important magma/mantle interactions High-Mg-Ni-Cr TTG
Low heat production Low geothermal gradients No slab but mantle wedge melting
EARLY ARCHAEANLATE ARCHAEANTODAY
INTERPRETATION
MORE EVIDENCES OF
SLAB MELT - MANTLE INTERACTIONS
•Sanukitoids
•« Closepet-type » granites
•Petrogenesis
•Conclusion
Sanukitoids: petrography
Diorites, monzodiorites and granodiorites
Lots of microgranular mafic enclaves
Qz + Pg + KF + Bt + Hb ± Cpx
Ap + Ilm + Sph + Zn
Porphyritic monzogranite
Associated with dioritic enclaves
Qz + KF + Pg + Bt + Hb ± Cpx
Ap + Ilm + Sph + Zn
Mixing between :
- mantle-derived diorite
- crustal, anatectic granite
« Closepet-type » granites
Diorite and monzonites
Nd(T) = -2 to 0
(enriched mantle)
Pg +KF + Bt + Hb ± Cpx
Ap + Ilm + Mt + Sph + Zn + All (all abundant)
« Closepet-type » dioritic facies
PRELIMINARY CONCLUSIONS III
Low melt/peridotite ratio
Strong melt/mantle interactions: sanukitoids
Diminushing melt/peridotite ratio over time (Earth secular cooling)
Onset of sanukitoids and Closepet-type at the end of the Archaean
Low melt/peridotite ratio
Cooling of the Earth
Increased depth of melting
Complete assimilation of melts: enriched mantle (Closepet)
Even lower melt/peridotite ratio
CONCLUSIONS
TTG were generated by basalt melting, under a mantle slice they were produced by subducted slab melting
From 4.0 to 2.5 Ga depth of slab melting increased :At 4.0 Ga : shallow depth melting,
plagioclase stable, no or few mantle/magma interactions
At 2.5 Ga : great depth melting, plagioclase unstable,
strong mantle/magma interactionsAppearance of new types of subduction-related rocks
These changes reflect the progressive cooling of our planet