Chemical mass balance in a reaction zone between serpentinite and metapelites in the Nishisonogi metamorphic rocks, Kyushu, Japan: Implications for devolatilization

Island Arc

Volumn 16, Issue 1, 2007, Pages 28-39

  Mori, Yasushi ^a   Nishiyama, Tadao ^b   Yanagi, Takeru ^c  

^a KITAKYUSHU MUSEUM OF NATURAL HISTORY AND HUMAN HISTORY   (Japan)

^b KUMAMOTO UNIVERSITY   (Japan)

^c KYUSHU UNIVERSITY   (Japan)

Author keywords

Fluid; Isocon; Metasomatism; Nishisonogi metamorphic rocks; Reaction zone; Serpentinite; Vein

Indexed keywords

FLUID INCLUSION; MASS BALANCE; METAPELITE; METASOMATISM; MUSCOVITE; PROTOLITH; SCHIST; SERPENTINE; TEMPERATURE EFFECT; VEIN (GEOLOGY);

ASIA; EURASIA; FAR EAST; JAPAN; KYUSHU;

EID: 33847052033     PISSN: 10384871     EISSN: 14401738     Source Type: Journal    
DOI: 10.1111/j.1440-1738.2007.00556.x     Document Type: Article

References (29)

1. Barnes J. D., Selverstone J. & Sharp Z. D. 2004. Interactions between serpentinite devolatilization, metasomatism and strike-slip strain localization during deep-crustal shearing in the Eastern Alps. Journal of Metamorphic Geology 22, 283-300.
2. Baumgartner L. P. & Olsen S. N. 1995. A least-squares approach to mass transport calculations using the isocon method. Economic Geology 90, 1261-70.
3. Beach A. 1977. Vein arrays, hydraulic fractures and pressure-solution structures in a deformed flysch sequence, S.W. England. Tectonophysics 40, 201-25.
4. Chidester A. H. 1968. Evolution of the ultramafic complexes of northwestern New England. In Zen E., White W. S. & Hadley J. B. (eds). Studies of Appalachian Geology: Northern and Maritime, pp. 343-54. John Wiley & Sons, New York.
5. Chidester A. H. & Cady W. M. 1972. Origin and emplacement of Alpine-type ultramafic rocks. Nature Physical Science 240, 27-31.
6. Cooper A. F. 1976. Concentrically zoned ultramafic pods from the Haast Schist Zone, South Island, New Zealand. New Zealand Journal of Geology and Geophysics 19, 603-23.
7. Curtis C. D. & Brown P. E. 1969. The metasomatic development of zoned ultramafic bodies in Unst, Shetland. Contributions to Mineralogy and Petrology 24, 275-92.
8. Curtis C. D. & Brown P. E. 1971. Trace element behavior in the zoned metasomatic bodies of Unst, Shetland. Contributions to Mineralogy and Petrology 31, 87-93.
9. Enami M., Wallis S. & Banno Y. 1994. Paragenesis of sodic pyroxene-bearing quartz schists: Implications for the P-T history of the Sanbagawa belt. Contributions to Mineralogy and Petrology 116, 182-98.
10. 40Ar and microtectonic constraints from the Nagasaki schists (western Kyushu), an extension of the Sanbagawa high-pressure belt. Earth and Planetary Science Letters 91, 105-16.
11. Grant J. A. 1986. The isocon diagram - A simple solution to Gresens' equation for metasomatic alteration. Economic Geology 81, 1976-82.
12. Hattori H. & Shibata K. 1982. Radiometric dating of pre-Neogene granitic and metamorphic rocks in northwest Kyushu, Japan - with emphasis on geotectonics of the Nishisonogi zone. Bulletin of Geological Survey of Japan 33, 57-84.
13. Hattori H., Inoue H. & Matsui K. 1993. Geology of the Konoura District. With Geological sheet map at 1:50000. Geological Survey of Japan, Tsukuba (in Japanese with English abstract).
14. H utchisonC. S. 1974. Laboratory Handbook of Petrographic Techniques. John Wiley & Sons, New York.
15. Jahns R. H. 1967. Serpentinites of the Roxbury district, Vermont. In Wyllie P. J. (ed.). Ultramafic and Related Rocks, pp. 137-60. John Wiley & Sons, New York.
16. 2 mixtures at elevated pressures and temperatures. American Journal of Science 281, 735-67.
17. Koons P. O. 1981. A study of natural and experimental metasomatic assemblages in an ultramafic-quartzofeldspathic metasomatic system from the Haast Schist, South Island, New Zealand. Contributions to Mineralogy and Petrology 78, 189-95.
18. Mori Y. & Mashima H. 2005. X-ray fluorescence analysis of major and trace elements in silicate rocks using 1:5 dilution glass beads. Bulletin of the Kitakyushu Museum of Natural History and Human History A3, 1-12.
19. Mori Y., Nishiyama T. & Yanagi T. 2003. Mass transfer and reaction paths in alteration zones around carbonate veins in the Nishisonogi Metamorphic Rocks, southwest Japan. American Mineralogist 88, 611-23.
20. Nishiyama T. 1989a. Petrologic study of the Nagasaki metamorphic rocks in the Nishisonogi peninsula - with special reference to the greenrock complex and the reaction-enhanced ductility. Memoirs of the Geological Society of Japan 33, 237-57 (in Japanese with English abstract).
21. Nishiyama T. 1989b. Kinetics of hydrofracturing and metamorphic veining. Geology 17, 1068-71.
22. 2-metasomatism of a metabasite block in a serpentinite melange from the Nishisonogi metamorphic rocks, southwest Japan. Contributions to Mineralogy and Petrology 104, 35-46.
23. Noda M. & Muta K. 1957. The geological structure of the Nishisonogi peninsula, Nagasaki prefecture. Report on Earth Sciences, Department of General Education, Kyushu University 4, 17-21 (in Japanese with English abstract).
24. Phillips A. H. & Hess H. H. 1936. Metamorphic differentiation at contacts between serpentinite and siliceous country rocks. American Mineralogist 21, 333-62.
25. Read H. H. 1934. On zoned associations of antigorite, talc, actinolite, chlorite, and biotite in Unst, Shetland Islands. Mineralogical Magazine 23, 519-40.
26. Sanford R. F. 1982. Growth of ultramafic reaction zones in greenschist to amphibolite facies metamorphism. American Journal of Science 282, 543-616.
27. Shigeno M., Mori Y. & Nishiyama T. 2005. Reaction microtextures in jadeitites from the Nishisonogi metamorphic rocks, Kyushu, Japan. Journal of Mineralogical and Petrological Sciences 100, 237-46.
28. Uchida Y. & Muta K. 1957. The talc deposits in northern Kyushu (1) -distribution and types of the talc deposits. Journal of Geological Society of Japan 63, 586-97 (in Japanese with English abstract).
29. Uchida Y. & Muta K. 1958. The talc deposits in northern Kyushu (2) - on the talc deposits of the Nishisonogi type. Journal of Geological Society of Japan 64, 494-515 (in Japanese with English abstract).