Advanced Search

Indexed by SCI、CA、РЖ、PA、CSA、ZR、etc .

Volume 21 Issue 5
Oct 2010
Turn off MathJax
Article Contents
Journal of Earth Science  > 2010  >  21(5): 635-640.
Benxun Su, Hongfu Zhang, Sakyi Patrick Asamoah, Kezhang Qin, Yanjie Tang, Jifeng Ying, Yan Xiao. Garnet-Spinel Transition in the Upper Mantle: Review and Interpretation. Journal of Earth Science, 2010, 21(5): 635-640. doi: 10.1007/s12583-010-0117-x
Citation: Benxun Su, Hongfu Zhang, Sakyi Patrick Asamoah, Kezhang Qin, Yanjie Tang, Jifeng Ying, Yan Xiao. Garnet-Spinel Transition in the Upper Mantle: Review and Interpretation. Journal of Earth Science, 2010, 21(5): 635-640. doi: 10.1007/s12583-010-0117-x
shu

Garnet-Spinel Transition in the Upper Mantle: Review and Interpretation

doi: 10.1007/s12583-010-0117-x
  • 1.

    Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

  • 2.

    State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

  • 3.

    Graduate University of Chinese Academy of Sciences, Beijing 100049, China

  • 4.

    Department of Earth Science, University of Ghana, Legon-Accra, Ghana

Funds:

the Special Research Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences 1008

the National Natural Science Foundation of China 90714008

More Information
  • Corresponding author: Zhang Hongfu, hfzhang@mail.igcas.ac.cn
  • Received Date: 20 May 2010
  • Accepted Date: 25 Jun 2010
  • Publish Date: 01 Oct 2010
    Abstract
  • This study carried out a comprehensive review of mantle-derived garnet peridotites on the basis of their garnet-spinel compositional relationships. The P-T estimates of the garnet peridotites of both orogenic and xenolithic derivations confirm previously established two garnet-spinel transition (GST) zones. Results of natural samples and experimental studies of all the garnet peridotites plot below the first GST at low P (< 2 GPa). The second GST at high P (6-10 GPa), obtained from the experimental system (MgO-Cr2O3-SiO2), was firstly evidenced from natural samples in this study and may imply a challenge to our understanding of Cr-rich and Al-poor mineral phase transition under ultrahigh P condition. Based on the data and our estimates, we propose the existence of another GST within the garnet peridotite discontinuous zone and a potential spinel-phase peridotite zone in the upper mantle.

     

    • FullText(HTML)
  • loading
    • References(33)
  • Asimov, P. D., Hirschmann, M. M., Ghiorso, M. S., et al., 1995. The Effect of Pressure Induced Solid-Solid Phase Transitions on Decompression Melting of the Mantle. Geochimica et Cosmochimica Acta, 59: 4489-4506 doi: 10.1016/0016-7037(95)00252-U
    Chen, L., Zheng, T. Y., Xu, W. W., 2006. A Thinned Lithospheric Image of the Tanlu Fault Zone, Eastern China: Constructed from Wave Equation Based Receiver Function Migration. Journal of Geophysical Research, 111: 1-15
    Falloon, T. J., Green, D. H., 1988. Anhydrous Partial Melting of Peridotite from 8 to 35 kb and the Petrogenesis of MORB. Journal of Petrology, (Suppl. ): 379-414
    Fan, Q. C., Liu, R. X., Xie, H. S., et al., 1997. Experimental Study of Spinel-Garnet Phase Transition in Upper Mantle and Its Significance. Science in China (Ser. D), 27: 109-114
    Gasparik, T., Newton, R. C., 1984. The Reversed Alumina Contents of Orthopyroxene in Equilibrium with Spinel and Forsterite in the System MgO-Al2O3-SiO2. Contributions to Mineralogy and Petrology, 85: 186-196 doi: 10.1007/BF00371708
    Green, D. H., Ringwood, A. E., 1967. The Stability Field of Aluminous Pyroxene Peridotite and Garnet Peridotite and Their Relevance in Upper Mantle Structure. Earth and Planetary Science Letters, 3: 151-160 doi: 10.1016/0012-821X(67)90027-1
    Griffin, W. L., O'Reilly, S. Y., 1987. Is the Continental Moho the Crust-Mantle Boundary? Geology, 15: 241-244 doi: 10.1130/0091-7613(1987)15<241:ITCMTC>2.0.CO;2
    Hales, A. L., 1969. A Seismic Discontinuity in the Lithosphere. Earth and Planetary Science Letters, 7: 44-46 doi: 10.1016/0012-821X(69)90009-0
    Klemme, S., O'Neill, H. S. C., 2000. The Effect of Cr on the Solubility of Al in Orthopyroxene: Experiments and Thermodynamic Modelling. Contributions to Mineralogy and Petrology, 140: 84-98 doi: 10.1007/s004100000140
    Klemme, S., 2004. The Influence of Cr on the Garnet-Spinel Transition in the Earth's Mantle: Experiments in the System MgO-Cr2O3-SiO2 and Thermodynamic Modeling. Lithos, 77: 639-646 doi: 10.1016/j.lithos.2004.03.017
    LaTourette, T. K., Kennedy, A. K., Wasserburg, G. J., 1993. Thorium-Uranium Fractionation by Garnet: Evidence for a Deep Source and Rapid Rise of Oceanic Basalts. Science, 261: 739-742 doi: 10.1126/science.261.5122.739
    MacGregor, I. D., 1965. Stability Fields of Spinel and Garnet Peridotites in the Synthetic System MgO-CaO-Al2O3-SiO2. Year b. -Carnegie Institute Washington, 64: 126-134
    MacKenzie, J. M., Canil, D., Johnston, S., et al., 2005. First Evidence for Ultrahigh-Pressure Garnet Peridotite in the North American Cordillera. Geological Society of America, 33: 105-108
    Menzies, M. A., Chazot, G., 1995. Fluid Processes in Diamond to Spinel Facies Shallow Mantle. Journal of Geodynamics, 20: 387-415 doi: 10.1016/0264-3707(95)00018-5
    O'Hara, M. J., Richardson, S. W., Wilson, G., 1971. Garnet-Peridotite Stability and Occurrence in Crust and Mantle. Contributions to Mineralogy and Petrology, 32: 48-68 doi: 10.1007/BF00372233
    O'Neill, H. S. C., 1981. The Transition between Spinel Lherzolite and Garnet Lherzolite, and Its Use as a Geobarometer. Contributions to Mineralogy and Petrology, 77: 185-194 doi: 10.1007/BF00636522
    Pavlenkova, N. I., 1997. General Features of the Upper Mantle Structure from Seismic Data. In: Fuchs, K., ed., Upper Mantle Heterogeneities from Active and Passive Seismology. Kluwer Academic Publishing, Netherlands. 225-236
    Robinson, J. A. C., Wood, B. J., 1998. The Depth of the Garnet/Spinel Transition in Fractionally Melting Peridotite. Earth and Planetary Science Letters, 164: 277-284 doi: 10.1016/S0012-821X(98)00213-1
    Salters, V. J. M., 1996. The Generation of Mid-Ocean Ridge Basalts from the Hf and Nd Isotope Perspective. Earth and Planetary Science Letters, 141: 109-123 doi: 10.1016/0012-821X(96)00070-2
    Salters, V. J. M., Hart, S. R., 1989. The Hafnium Paradox and the Role of Garnet in the Source of Mid-Ocean-Ridge Basalts. Nature, 342: 420-422 doi: 10.1038/342420a0
    Schiano, P., Eiler, J. M., Hutcheon, I. D., et al., 2000. Primitive CaO-Rich, Silica-Undersaturated Melts in Island Arcs: Evidence for the Involvement of Clinopyroxene-Rich Lithologies in the Petrogenesis of Arc Magmas. Geochemistry, Geophysic, Geosystems, 1: 1999GC000032
    Sen, G., Keshav, S., Bizimis, M., 2005. Hawaiian Lithosphere and Magmas: Composition and Thermal Characteristics of the Lithosphere beneath Oahu: Insights from Mantle Xenoliths. American Mineralogist, 90: 871-887 doi: 10.2138/am.2005.1731
    Shimamura, H., Asada, T., 1976. Apparent Velocity Measurements on Oceanic Lithosphere. Physics of the Earth and Planetary Interiors, 13: 15-22 doi: 10.1016/0031-9201(76)90102-3
    Stachel, T., Harris, J. W., 1997. Syngenetic Inclusions in Diamond from the Birim Field (Ghana)—A Deep Peridotitic Profile with a History of Depletion and Re-enrichment. Contributions to Mineralogy and Petrology, 127: 336-352 doi: 10.1007/s004100050284
    Stachel, T., Harris, J. W., Brey, G. P., et al., 2000. Kankan Diamonds (Guinea): II. Lower Mantle Inclusion Parageneses. Contributions to Mineralogy and Petrology, 140: 16-27 doi: 10.1007/s004100000174
    Stachel, T., Viljoen, K. S., Brey, G. P., et al., 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: 1-12 doi: 10.1016/S0012-821X(98)00064-8
    Su, B. X., Zhang, H. F., Sakyi, P. A., et al., 2010a. Compositionally Stratified Lithosphere and Carbonatite Metasomatism Recorded in Mantle Xenoliths from the Western Qinling (Central China). Lithos, 116: 111-128 doi: 10.1016/j.lithos.2010.01.004
    Su, B. X., Zhang, H. F., Tang, Y. J., et al., 2010b. Geochemical Syntheses among the Cratonic, Off-Cratonic and Orogenic Garnet Peridotites and Their Tectonic Implications. International Journal of Earth Sciences, doi: 10.1007/s00531-010-0527-0
    Su, B. X., Zhang, H. F., Wang, Q. Y., et al., 2007. Spinel-Garnet Phase Transition Zone of Cenozoic Lithospheric Mantle beneath the Eastern China and Western Qinling and Its T-P Condition. Acta Petrologica Sinica, 23: 1313-1320 (in Chinese with English Abstract)
    Su, B. X., Zhang, H. F., Ying, J. F., et al., 2009. Nature and Processes of the Lithospheric Mantle beneath the Western Qinling: Evidence from Deformed Peridotitic Xenoliths in Cenozoic Kamafugite from Haoti, Gansu Province, China. Journal of Asian Earth Sciences, 34: 258-274 doi: 10.1016/j.jseaes.2008.05.009
    Walter, M., Katsura, T., Kubo, A., et al., 2002. Spinel-Garnet Lherzolite Transition in the System CaO-MgO-Al2O3-SiO2 Revisited: An In Situ X-Ray Study. Geochimica et Cosmochimica Acta, 66: 2109-2121 doi: 10.1016/S0016-7037(02)00845-1
    Webb, S. A. C., Wood, B. J., 1986. Spinel-Pyroxene-Garnet Relationship and Their Dependence on Cr/Al Ratio. Contributions to Mineralogy and Petrology, 77: 185-194
    Xu, Y. G., Lin, C. Y., Shi, L. B., et al., 1995. Upper Mantle Geotherm for Eastern China and Its Geological Implications. Science in China (Ser. B), 38: 1482-1492
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(2)

    Get Citation
    PDF
    XML

    Article Metrics

    Article views(779) PDF downloads(52) Cited by()
    Proportional views
    Related

    Copyright © 2013-2020 Journal of Earth Science 鄂ICP备15021562号-2

    Tel: +86-27-67885075 Fax: +86-27-67885075 E-mail: xbb@cug.edu.cn

    Address: Editorial Office of Journal, China University of Geosciences, Yujiashan, Wuhan, Hubei 430074, P. R. China

    Supported by: Beijing Renhe Information Technology Co. Ltd  E-mail: info@rhhz.net  

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return