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Information Journal Paper

Title

ORIGINAL MINERALOGY AND DIAGENETIC PROCESSES OF THE SOLTANIEH FORMATION AT TYPE SECTION BASED ON GEOCHEMICAL STUDIES

Pages

  29-42

Abstract

 The SOLTANIEH FORMATION “Southeast Zanjan” consists mainly of carbonate and shale sequences. Geochemical studies such as sr/Ca and d18 values of shows that these carbonates were affected mostly by open system meteoric digenesis. Distribution of major and minor elements such as Sr/Na and Mn versus Na and d18 O and d13 C values of limestones in SOLTANIEH FORMATION indicates that the mineralogy of carbonate were originally aragonite. These data fall within the Mozduran limestone and Gordon limestone (Tasmania, Australia) fields due to similar aragonite mineralogy. Original aragonite mineralogy for Neoproterozoic limestones from other parts of the world has also been suggested and can support our interpretation. Light d13 (-4.57 0/00  VPDB) values in Soltanieh limestone support meteoric DIAGENESIS and Sr/Mn variation indicates high dissolution rate of limestone.Pale temperature calculations, d18 O values (-5.83 0/00 VPDB) and dw 3±1 , range between 23% - 31%c, respectively.

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    APA: Copy

    SIAB GHODSI, A.A., ADAABI, M.H., HAMDI, B.A.D., & SADEGHI, ABAS. (2006). ORIGINAL MINERALOGY AND DIAGENETIC PROCESSES OF THE SOLTANIEH FORMATION AT TYPE SECTION BASED ON GEOCHEMICAL STUDIES. IRANIAN JOURNAL OF GEOLOGY, 2(5), 29-42. SID. https://sid.ir/paper/129280/en

    Vancouver: Copy

    SIAB GHODSI A.A., ADAABI M.H., HAMDI B.A.D., SADEGHI ABAS. ORIGINAL MINERALOGY AND DIAGENETIC PROCESSES OF THE SOLTANIEH FORMATION AT TYPE SECTION BASED ON GEOCHEMICAL STUDIES. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2006;2(5):29-42. Available from: https://sid.ir/paper/129280/en

    IEEE: Copy

    A.A. SIAB GHODSI, M.H. ADAABI, B.A.D. HAMDI, and ABAS SADEGHI, “ORIGINAL MINERALOGY AND DIAGENETIC PROCESSES OF THE SOLTANIEH FORMATION AT TYPE SECTION BASED ON GEOCHEMICAL STUDIES,” IRANIAN JOURNAL OF GEOLOGY, vol. 2, no. 5, pp. 29–42, 2006, [Online]. Available: https://sid.ir/paper/129280/en

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