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Information Journal Paper

Title

P-T TREND EVIDENCE FOR POLYMETAMORPHISM IN HIGH GRADE METAMORPHIC ROCKS IN THE CENTRAL ZONE OF A LIMPOPO COMPLEX (SOUTH AFRICA)

Pages

  43-60

Abstract

 P-T trends represent the single reliable source for thermal and dynamic record of metamorphic and igneous complexes and may serve as a basis for geodynamic models that simulate exhumation of such complexes from mantle. This study demonstrates that, knowledge of P-T TREND configuration in combination with isotopic geochronology makes it possible not only to ascertain the nature of POLYMETAMORPHISM but also to define a mechanism of rock exhumation. Analysis of P-T TRENDs has shown that, the Precambrian GRANULITE complex of LIMPOPO (South Africa) is repeatedly exhumed. First, this complex was accommodated within the crust and remained for long period of time (up to few hundred million years) and then, these rocks which were in a metastable state in the Earth’s gravity field were reactivated by the fluid and heat flow from the mantle plume which caused the reduction in viscosity and upward movement toward the surface.

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  • Cite

    APA: Copy

    TABATABAEIMANESH, S.M.. (2008). P-T TREND EVIDENCE FOR POLYMETAMORPHISM IN HIGH GRADE METAMORPHIC ROCKS IN THE CENTRAL ZONE OF A LIMPOPO COMPLEX (SOUTH AFRICA). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 29(3 (GEOLOGY)), 43-60. SID. https://sid.ir/paper/55918/en

    Vancouver: Copy

    TABATABAEIMANESH S.M.. P-T TREND EVIDENCE FOR POLYMETAMORPHISM IN HIGH GRADE METAMORPHIC ROCKS IN THE CENTRAL ZONE OF A LIMPOPO COMPLEX (SOUTH AFRICA). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2008;29(3 (GEOLOGY)):43-60. Available from: https://sid.ir/paper/55918/en

    IEEE: Copy

    S.M. TABATABAEIMANESH, “P-T TREND EVIDENCE FOR POLYMETAMORPHISM IN HIGH GRADE METAMORPHIC ROCKS IN THE CENTRAL ZONE OF A LIMPOPO COMPLEX (SOUTH AFRICA),” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 29, no. 3 (GEOLOGY), pp. 43–60, 2008, [Online]. Available: https://sid.ir/paper/55918/en

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