Shirey, S. B. (2002) Diamond Genesis, Seismic Structure, and Evolution of the Kaapvaal-Zimbabwe Craton. Science, 297 (5587). 1683-1686 doi:10.1126/science.1072384

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

	Carlson, Richard W., Grove, Timothy L., De Wit, Maarten J., Gurney, John J. (1996) Program to study crust and mantle of the Archean craton in southern Africa. Eos, Transactions American Geophysical Union, 77 (29) 273 doi:10.1029/96eo00194
	D. E. James M. J. Fouch in Early Earth C. Ebinger M. Fowler C. J. Hawkesworth Eds. (Geological Society of London in press).
	James, D. E., Fouch, M. J., VanDecar, J. C., van der Lee, S., , (2001) Tectospheric structure beneath southern Africa. Geophysical Research Letters, 28 (13) 2485-2488 doi:10.1029/2000gl012578
	Carlson R. W., et al., GSA Today 10, 1 (2000).
	J. W. Harris in The Properties of Natural and Synthetic Diamond J. E. Field Ed. (Academic Press New York 1992) pp. 345–393.
	D. G. Pearson S. B. Shirey in Application of Radiogenic Isotopes to Ore Deposit Research and Exploration D. D. Lambert J. Ruiz Eds. (Society of Economic Geologists Denver CO 1999) vol. 12 pp. 143–172.
	BOYD, F. R., GURNEY, J. J. (1986) Diamonds and the African Lithosphere. Science, 232 (4749). 472-477 doi:10.1126/science.232.4749.472
	Janse A. J. A., Russ. Geol. Geophys. 33, 9 (1992).
	The Archean Eon extends from 3.8 Ga to 2.5 Ga. The Proterozoic Eon extends from 2.5 Ga to 544 Ma.
	Richardson, S. H., Gurney, J. J., Erlank, A. J., Harris, J. W. (1984) Origin of diamonds in old enriched mantle. Nature, 310 (5974). 198-202 doi:10.1038/310198a0
	Richardson, S. H., Harris, J. W., Gurney, J. J (1993) Three generations of diamonds from old continental mantle. Nature, 366 (6452). 256-258 doi:10.1038/366256a0
	Davis G. L., Krogh T. E., Erlank A. J., Carnegie Inst. Washington Year Book 75, 821 (1976).
	Davis G. L., Carnegie Inst. of Washington Year Book 76, 631 (1977).
	Smith C. B., Allsopp H. L., Kramers J. D., Hutchinson G., Roddick J. C., Trans. Geol. Soc. S. Africa 88, 249 (1985).
	Harzburgitic diamonds have low Ca and high Cr garnet inclusions named after harzburgite a depleted mantle rock. Lherzolitic diamonds have higher Ca and lower Cr content garnet and clinopyroxene inclusions named after lherzolite a less depleted mantle rock. Both diamond types are called “P-type” after peridotite the general name for harzburgite and lherzolite. Other P-type diamonds contain Fe-sulfide inclusions that are high in Ni. Eclogitic diamonds (“E-type”) have pyrope-almandine garnet omphacitic clinopyroxene or Fe-sulfide inclusions with low Ni content characteristic of eclogite a high-pressure metamorphosed basalt.
	Richardson, Stephen H. (1986) Latter-day origin of diamonds of eclogitic paragenesis. Nature, 322 (6080). 623-626 doi:10.1038/322623a0
	Richardson, S. H., Erlank, A. J., Harris, J. W., Hart, S. R. (1990) Eclogitic diamonds of Proterozoic age from Cretaceous kimberlites. Nature, 346 (6279). 54-56 doi:10.1038/346054a0
	S. H. Richardson I. L. Chinn J. W. Harris in The P. H. Nixon Volume J. J. Gurney J. L. Gurney M. D. Pascoe S. H. Richardson Eds. (Red Roof Design Cape Town 1999) pp. 734–736.
	Pearson, D.G., Shirey, S.B., Harris, J.W., Carlson, R.W. (1998) Sulphide inclusions in diamonds from the Koffiefontein kimberlite, S Africa: constraints on diamond ages and mantle Re–Os systematics. Earth and Planetary Science Letters, 160 (3) 311-326 doi:10.1016/s0012-821x(98)00092-2
	Richardson, S.H., Shirey, S.B., Harris, J.W., Carlson, R.W. (2001) Archean subduction recorded by Re–Os isotopes in eclogitic sulfide inclusions in Kimberley diamonds. Earth and Planetary Science Letters, 191 (3) 257-266 doi:10.1016/s0012-821x(01)00419-8
	Shirey, Steven B., Carlson, Richard W., Richardson, Stephen H., Menzies, Andrew, Gurney, John J., Pearson, D. Graham, Harris, Jeffrey W., Wiechert, Uwe (2001) Archean emplacement of eclogitic components into the lithospheric mantle during formation of the Kaapvaal Craton. Geophysical Research Letters, 28 (13) 2509-2512 doi:10.1029/2000gl012589
	P. Cartigny thesis Universite de Paris VII (1998).
	Cartigny, P. (1998) Eclogitic Diamond Formation at Jwaneng: No Room for a Recycled Component. Science, 280 (5368). 1421-1424 doi:10.1126/science.280.5368.1421
	Deines, Peter, Harris, J.W., Gurney, J.J. (1993) Depth-related carbon isotope and nitrogen concentration variability in the mantle below the Orapa kimberlite, Botswana, Africa. Geochimica et Cosmochimica Acta, 57 (12) 2781-2796 doi:10.1016/0016-7037(93)90390-i
	Deines, Peter, Gurney, J.J, Harris, J.W (1984) Associated chemical and carbon isotopic composition variations in diamonds from Finsch and Premier kimberlite, South Africa. Geochimica et Cosmochimica Acta, 48 (2) 325-342 doi:10.1016/0016-7037(84)90254-0
	Deines, Peter, Harris, J.W. (1995) Sulfide inclusion chemistry and carbon isotopes of African diamonds. Geochimica et Cosmochimica Acta, 59 (15) 3173-3188 doi:10.1016/0016-7037(95)00205-e
	Deines, Peter, Harris, J.W, Gurney, J.J (1987) Carbon isotopic composition, nitrogen content and inclusion composition of diamonds from the Roberts Victor kimberlite, South Africa: Evidence for 13C depletion in the mantle. Geochimica et Cosmochimica Acta, 51 (5) 1227-1243 doi:10.1016/0016-7037(87)90215-8
	Deines, Peter, Harris, J.W, Gurney, J.J (1991) The carbon isotopic composition and nitrogen content of lithospheric and asthenospheric diamonds from the Jagersfontein and Koffiefontein kimberlite, South Africa. Geochimica et Cosmochimica Acta, 55 (9) 2615-2625 doi:10.1016/0016-7037(91)90377-h
	Deines, Peter, Harris, J.W, Spear, P.M, Gurney, J.J (1989) Nitrogen and 13C content of Finsch and Premier diamonds and their implications. Geochimica et Cosmochimica Acta, 53 (6) 1367-1378 doi:10.1016/0016-7037(89)90069-0
	Deines, Peter, Harris, J.W., Gurney, J.J. (1997) Carbon isotope ratios, nitrogen content and aggregation state, and inclusion chemistry of diamonds from Jwaneng, Botswana. Geochimica et Cosmochimica Acta, 61 (18) 3993-4005 doi:10.1016/s0016-7037(97)00199-3
	J. J. Gurney in Kimberlites and Related Rocks J. Ross et al. Eds. (Geological Society of Australia Sydney Australia 1989) vol. 14 pp. 935–965.
	Kirkley, Melissa B., Gurney, John J., Levinson, Alfred A. (1991) Age, Origin, and Emplacement of Diamonds: Scientific Advances in the Last Decade. Gems & Gemology, 27 (1) 2-25 doi:10.5741/gems.27.1.2
	Diamonds with no or low (<20 ppm) N are termed Type II. Diamonds with spectroscopically detectable N (termed Type Ia Table 1) show a N distribution that progresses from C-centers (single N) through A-centers (paired N) to B-centers (clusters of four N and a vacancy) in proportion with geological time (hundreds of Ma) temperature and nitrogen content. Of these three variables N aggregation will be sensitive chiefly to temperature. See ( 49 ) for details.
	Not Yet Imported: The Mantle Sample: Inclusion in Kimberlites and Other Volcanics - book-chapter : 10.1029/SP016p0104 If you would like this item imported into the Digital Library, please contact us quoting Journal ID
	Jones, M. Q. W. (1988) Heat flow in the Witwatersrand Basin and environs and its significance for the South African Shield Geotherm and lithosphere thickness. Journal of Geophysical Research, 93. 3243 doi:10.1029/jb093ib04p03243
	Not Yet Imported: The Mantle Sample: Inclusion in Kimberlites and Other Volcanics - book-chapter : 10.1029/SP016p0001 If you would like this item imported into the Digital Library, please contact us quoting Journal ID
	R. W. Carlson et al. in The J. B. Dawson Volume J. J. Gurney J. L. Gurney M. D. Pascoe S. H. Richardson Eds. (Red Roof Design Cape Town 1999) pp. 99–108.
	Irvine, Gordon J., Pearson, D. Graham, Carlson, Richard W. (2001) Lithospheric mantle evolution of the Kaapvaal Craton: A Re-Os isotope study of peridotite xenoliths from Lesotho kimberlites. Geophysical Research Letters, 28 (13) 2505-2508 doi:10.1029/2000gl012411
	Walker, R.J, Carlson, R.W, Shirey, S.B, F.R, Boyd (1989) Os, Sr, Nd, and Pb isotope systematics of southern African peridotite xenoliths: Implications for the chemical evolution of subcontinental mantle. Geochimica et Cosmochimica Acta, 53 (7) 1583-1595 doi:10.1016/0016-7037(89)90240-8
	Canil, Dante, Wei, Kejian (1992) Constraints on the origin of mantle-derived low Ca garnets. Contributions to Mineralogy and Petrology, 109 (4) 421-430 doi:10.1007/bf00306546
	Stachel, Thomas, Viljoen, K.Stephanus, Brey, Gerhard, Harris, Jeff W (1998) Metasomatic processes in lherzolitic and harzburgitic domains of diamondiferous lithospheric mantle: REE in garnets from xenoliths and inclusions in diamonds. Earth and Planetary Science Letters, 159 (1) 1-12 doi:10.1016/s0012-821x(98)00064-8
	Walter, M. J. (1998) Melting of Garnet Peridotite and the Origin of Komatiite and Depleted Lithosphere. Journal of Petrology, 39 (1) 29-60 doi:10.1093/petroj/39.1.29
	Parman, S. W., Grove, T. L., Dann, J. C. (2001) The production of Barberton komatiites in an Archean Subduction Zone. Geophysical Research Letters, 28 (13) 2513-2516 doi:10.1029/2000gl012713
	Haggerty, Stephen E. (1986) Diamond genesis in a multiply-constrained model. Nature, 320 (6057). 34-38 doi:10.1038/320034a0
	Arndt, Nicholas T., Kerr, Andrew C., Tarney, John (1997) Dynamic melting in plume heads: the formation of Gorgona komatiites and basalts. Earth and Planetary Science Letters, 146 (1) 289-301 doi:10.1016/s0012-821x(96)00219-1
	M. D. Schmitz thesis Massachusetts Institute of Technology (2002).
	Valley, John W., Kinny, Peter D., Schulze, Daniel J., Spicuzza, Michael J. (1998) Zircon megacrysts from kimberlite: oxygen isotope variability among mantle melts. Contributions to Mineralogy and Petrology, 133 (1) 1-11 doi:10.1007/s004100050432
	Cartigny, Pierre, Harris, Jeff W, Javoy, Marc (2001) Diamond genesis, mantle fractionations and mantle nitrogen content: a study of δ13C–N concentrations in diamonds. Earth and Planetary Science Letters, 185 (1) 85-98 doi:10.1016/s0012-821x(00)00357-5
	O. Navon in The P.H. Nixon Volume J. J. Gurney J. L. Gurney M. D. Pascoe S. H. Richardson Eds. (Red Roof Design Cape Town 1999) pp. 584–604.
	P. E. Janney R. W. Carlson S. B. Shirey D. R. Bell A. P. le Roex paper presented at the Ninth Annual V. M. Goldschmidt Conference Cambridge MA 22 to 26 August 1999.
	J. W. Harris unpublished data.
	Deines, Peter, Harris, J.W., Robinson, D.N., Gurney, J.J., Shee, S.R. (1991) Carbon and oxygen isotope variations in diamond and graphite eclogites from Orapa, Botswana, and the nitrogen content of their diamonds. Geochimica et Cosmochimica Acta, 55 (2) 515-524 doi:10.1016/0016-7037(91)90009-t
	Milledge, H. J., Mendelssohn, M. J., Seal, M., Rouse, J. E., Swart, P. K., Pillinger, C. T. (1983) Carbon isotopic variation in spectral type II diamonds. Nature, 303 (5920). 791-792 doi:10.1038/303791a0
	Deines, Peter, Viljoen, Fanus, Harris, J.W. (2001) Implications of the carbon isotope and mineral inclusion record for the formation of diamonds in the mantle underlying a mobile belt: Venetia, South Africa. Geochimica et Cosmochimica Acta, 65 (5) 813-838 doi:10.1016/s0016-7037(00)00569-x
	Smith, C.B, Gurney, J.J, Harris, J.W, Otter, M.L, Kirkley, M.B, Jagoutz, E (1991) Neodymium and strontium isotope systematics of eclogite and websterite paragenesis inclusions from single diamonds, Finsch and Kimberley Pool, RSA. Geochimica et Cosmochimica Acta, 55 (9) 2579-2590 doi:10.1016/0016-7037(91)90374-e
	S. H. Richardson unpublished data.
	S. Shirey et al. unpublished data.
	Discussions with D. Bell R. Carlson I. Chinn D. G. Pearson and K. Westerlund are greatly appreciated as is the assistance of T. Mock and M. Horan in the DTM mass spectrometry and chemistry labs respectively. We appreciate V. Anderson E. van Blerk R. Ferraris R. Hamman W. Moore A. Ntidisang G. Parker and others at Harry Oppenheimer House Kimberley for their skill in selecting specimens and we thank the De Beers Diamond Trading Company for making them available. The manuscript was improved by the reviews of F. Boyd K. Burke R. Carlson E. Hauri T. Stachel and E. Vicenzi. Support was chiefly from NSF EAR Continental Dynamics Grant 9526840.

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