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Geochemical Constraints on Archean Mantle Dynamics S.W. Parman Durham University Collaborators: Stan Hart, Mark Kurz, Tim Grove, Mike Walter, Graham Pearson,

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Presentation on theme: "Geochemical Constraints on Archean Mantle Dynamics S.W. Parman Durham University Collaborators: Stan Hart, Mark Kurz, Tim Grove, Mike Walter, Graham Pearson,"— Presentation transcript:

1 Geochemical Constraints on Archean Mantle Dynamics S.W. Parman Durham University Collaborators: Stan Hart, Mark Kurz, Tim Grove, Mike Walter, Graham Pearson, Geoff Nowell, Jeroen van Hunen

2 Geochemistry and Geodynamics Historically has been focused on reservoirs (primitive mantle, EM1, EM2, HIMU,D”…) New data constrain ages and timescales of mantle processes

3 Main points Helium isotopes do not require a primitive mantle or layered mantle convection Mantle evolution is punctuated by large melting events in the Archean/Proterozoic The source of plumes (ocean islands) has ancient (> 2 Ga) heterogeneities in it Mixing time in the convecting mantle is < 2 Ga old

4 Pattern of Mantle Convection?

5 Layered mantle convection D He <<D U+Th Allegre, Kurz, Moreira, Porcelli…

6 Zindler and Hart, 1986

7 Graham, 2002

8 Ar constraints Allegre et al., 1996

9 So what’s the problem?

10 van der Hilst et al., 1997 lower mantle

11 Graham, 2002

12 Ellam and Stuart, 2004

13 Layered mantle convection D He <<D U+Th Allegre, Kurz, Moreira, Porcelli…

14 If He more compatible than U+Th… D He >D U+Th

15 Parman et al., Nature 2005

16 If He more compatible than U+Th… D He >D U+Th

17 Implications Primitive mantle not required by He isotopes Whole mantle convection is consistent with data Davies, 2002

18 He isotopes do not require the existence of primitive mantle

19 Xie & Tackley, 2004

20 If He more compatible than U+Th… D He >D U+Th

21 Database kindly provided by Atosa Abedini, USGS

22 Iceland and Hawaii Kemp et al., 2006 Condie, 1998

23 Parman, Nature, 2007

24 Davies, EPSL (1995)

25 Implications Mantle convection in Archean was punctuated by large melting events These events appear to have produced large areas of the continental crust Davies, EPSL (1995)

26

27 Davies, 2002 Where is plume source?

28 Burke & Torsvik, 2004

29 Wen, EPSL 2006

30 plume conv.

31 Pearson, Parman and Nowell, Nature, 2007

32 Implications Plume source is ancient Convecting mantle (MORB source) is <2 Ga old Ferrachat & Ricard, 1998

33 The End


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