The role of fluid for diamond-free UHP dolomitic marble from the kokchetav massif

International Geology Review

Volumn 47, Issue 11, 2005, Pages 1178-1193

  Ogasawara, Yoshihide ^a   Aoki, Kazumasa ^a  

^a WASEDA UNIVERSITY   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

DOLOMITE; MARBLE; ULTRAHIGH PRESSURE METAMORPHISM;

ASIA; EASTERN HEMISPHERE; EURASIA; KAZAKHSTAN; KOKCHETAV MASSIF; WEST ASIA; WORLD;

EID: 27744592833     PISSN: 00206814     EISSN: 19382839     Source Type: Journal    
DOI: 10.2747/0020-6814.47.11.1178     Document Type: Article

References (34)

1. Akaishi, M., and Yamaoka, S., 2000. Crystallization of diamond from C-O-H fluids under high-pressure and high-temperature conditions. Journal of Crystal Growth, 209:999–1003.
2. Ayers, J. C., and Watson, E. B., 1993. Rutile solubility and mobility in supercritical aqueous fluids. Contributions to Mineralogy and Petrology, 114:321–330.
3. Claoue-Long, J. C., Sobolev, N. V., Shatsky, V. S., and Sobolev, A. V., 1991. Zircon response to diamondpressure metamorphism in Kokchetav massif. Geology, 19:710–713.
4. Dobretsov, N. L., Sobolev, N. V., Shatsky, V. S., Coleman, R. G., and Ernst, W. G., 1995. Diamondiferous paragenesis, northern Kazakhstan. The Island Arc, 4:267–279.
5. Harlow, G. E., 1997. K in clinopyroxene at high pressure and temperature:An experimental study. American Mineralogist, 82:259–269.
6. Iizuka, Y., and Nakamura, E., Experimental study of the slab-mantle interaction and implications for formation of titanoclinohumite at deep subduction zone. Proceedings of the Japan Academy. Vol. 71, pp. 159–164.
7. Imamura, K., Ogasawara, Y., Yurimoto, Y., and Kusakabe, M., 2003. SIMS carbon isotope study of microdiamond in UHP dolomite marble from the Kokchetav Massif. EOS (Transactions of the American Geophysical Union), 84:F1532
8. Imamura, K., Yoshioka, N., and Ogasawara, Y., 2002. “ Morphology and distribution of microdiamond in dolomite marble from Kumdy-kol ”. In The diamond-bearing Kokchetav Massif, Kazakhstan, Edited by:Parkinson, C. D., Katayama, I., Liou, J. G., and Maruyama, S., 93–102. Tokyo, Japan:Universal Academy Press.
9. Ishida, H., Ogasawara, Y., Ohsumi, K., and Saito, A., 2003. Two-stage growth of microdiamonds in UHP dolomite marble from Kokchetav Massif, Kazakhstan. Journal of Metamorphic Geology, 21:515–522.
10. Kaneko, Y., Maruyama, S., Terabayashi, H., Yamamoto, H., 2000. Geology of the Kokchetav UHP-HP metamorphic belt, northern Kazakhstan. The Island Arc, 9:264–283.
11. Katayama, I., Muko, A., Iizuka, T., Maruyama, S., Terada, K., Tsutsumi, Y., Sano, Y., Zhang, R. Y., and Liou, J. G., 2003. Dating of zircon from Ti-clinohumitebearing garnet peridotite:Implication for timing metasomatism. Geology, 31:713–716.
12. 2O transport into the mantle. American Mineralogist, 88:229–234.
13. Katayama, I., Ohta, M., and Ogasawara, Y., 2002. Mineral inclusions in zircon from diamond-bearing marble in the Kokchetav massif, northern Kazakhstan. European Journal of Mineralogy, 14:1103–1108.
14. Katayama, I., Parkinson, C. D., Okamoto, K., Nakajima, Y., and Maruyama, S., 2000. Supersilicic clinopyroxene and silica exsolution in UHPM eclogite and pelitic gneiss from the Kokchetav massif, northern Kazakhstan. The Island Arc, 9:417–427.
15. Kretz, R., 1983. Symbols for rock-forming minerals. American Mineralogist, 68:277–279.
16. 2 fluid at high pressure and high temperature. Journal of Crystal Growth, 213:203–206.
17. Luth, R. W., 1997. Experimental study of the system phlogopite-diopside from 3.5 to 17 GPa. American Mineralogist, 82:1198–1209.
18. Mukherjee, B. K., Sachan, H. K., Ogasawara, Y., Muko, A., and Yoshioka, N., 2003. Carbonate-bearing UHPM rocks from the Tso-Morari region, Ladakh, India:Petrological implications. International Geology Review, 45:49–69.
19. Muko, A., Okamoto, K., Yoshioka, N., Zhang, R. Y., Parkinson, C. D., Ogasawara, Y., and Liou, J. G., 2002. “ Petrogenesis of Ti-clinohumite-bearing garnetiferous ultramafic rocks from Kumdy-kol ”. In The diamond-bearing Kokchetav massif, Kazakhstan, Edited by:Parkinson, C. D., Katayama, I., Liou, J. G., and Maruyama, S., 343–359. Tokyo, Japan:Universal Academy Press.
20. Ogasawara, Y., Fluid control on metamorphic evolution of deeply subducted carbonates:The case of the Kokchetav UHP rocks [abs.]. Abstracts of the 11th Goldschmidt Conference. #3609
21. Ogasawara, Y., Fukasawa, K., and Maruyama, S., 2002. Coesite exsolution from supersilicic titanite in UHP marble from the Kokchetav Massif, northern Kazakhstan. American Mineralogist, 87:454–461.
22. Ogasawara, Y., and Ishida, H., Diamond, fluid and carbonates—stability and genesis of metamorphic diamond [abs.].:Abstracts of UHPM Workshop 2001. Fluid/slab/mantle interactions and ultrahigh-P minerals, pp. 1–5. Waseda University.
23. Ogasawara, Y., Ohta, M., Fukasawa, K., Katayama, I., and Maruyama, S., 2000. Diamond-bearing and diamond-free metacarbonate rocks from Kumdy-kol in the Kokchetav Massif, northern Kazakhstan. The Island Arc, 9:400–416.
24. Ogasawara, Y., Zhang, R. Y., and Liou, J. G., 1998. Petrogenesis of dolomitic marbles from Rongcheng in the Su-Lu ultrahigh-pressure metamorphic terrane, eastern China. The Island Arc, 7:82–97.
25. Okamato, K., Liou, J. G., and Ogasawara, Y., 2000. Petrology of the diamond-grade eclogite in the Kokchetav Massif, northern Kazakhstan. The Island Arc, 9:379–399.
26. Okamoto, K., and Maruyama, S., 1998. Multi-anvil reequilibration experiments of a Dabie Shan ultrahigh-pressure eclogite within the diamond-stability fields. The Island Arc, 7:52–69.
27. Schertl, H. P., and Okay, A. I., 1994. A coesite inclusion in dolomite in Dabie Shan, China:Petrological and rheological significance. European Journal of Mineralogy, 6:995–1000.
28. Sobolev, N. V., and Shatsky, V. S., 1990. Diamond inclusions in garnets from metamorphic rocks. Nature, 343:742–746.
29. Yoshioka, N., Muko, A., and Ogasawara, Y., Extremely high diamond concentration in dolomite marble [abs.].:Abstracts of UHPM Workshop 2001. Fluid/slab/mantle interactions and ultrahigh-P minerals, pp. 51–55. Waseda University.
30. Yoshioka, N., and Ogasawara, Y., 2004. Cathodoluminescence of microdiamond in dolomite marble from the Kokchetav Massif—Another evidence for two-stage growth of diamond. International Geology Review, in press
31. Zhang, R. Y., and Liou, J. G., 1996. Coesite inclusion in dolomite from eclogite in the southern Dabie Mountains, China:The significance of carbonate minerals in UHP rocks. American Mineralogist, 81:181–186.
32. Zhang, R. Y., and Liou, J. G., 2000. “ Exsolution lamellae in minerals from ultrahigh-pressure rocks ”. In Ultrahigh-pressure metamorphism and geodynamics in collision-type orogenic belts, International Book Series, v. 4 Edited by:Ernst, W. G., and Liou, J. G., 216–228. Columbia, MD:Bellwether Publishing, Geological Society of America.
33. Zhang, R. Y., and Liou, J. G., 2003. Clinopyroxenite from the Sulu ultrahigh-pressure terrane, eastern China:Origin and evolution of garnet exsolution in clinopyroxene. American Mineralogist, 88:1591–1600.
34. Zhang, R. Y., Liou, J. G., and Cong, B. L., 1994. Petrogenesis of garnet-bearing ultramafic rocks and associated eclogites in the Su-Lu ultrahigh-pressure metamorphic terrane, China. Journal of Metamorphic Geology, 12:169–186.