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Information Journal Paper

Title

PETROGRAPHY AND GEOCHEMISTY OF THE FRASNIAN ZEFREH SANDSTONE (NORTHEAST OF ESFAHAN)

Pages

  61-73

Abstract

 A sequence of the Upper Devonian age (Frasnian-Lower Famennian) on the western side of Zard Mountain is located near the Zefreh village. W of central Iran Basin (ca. 65 km NE of Esfahan). It is composed of five lithostratigraphic units, including two lowermost SANDSTONE and three uppermost carbonate unites. SANDSTONEs are mainly quartz arenite in composition. Low percentage of feldspar. Unstable minerals and presence of heavy minerals (Zircon and Turmaline) suggests high WEATHERING rate in source region, the high WEATHERING rate in samples. Revealed by petrographic studies and, CIW index as well, suggests a warm humid climate. The geochemical and modal data analysis of SANDSTONEs samples, plotted on the discriminate function diagrams determined the quartzose recycled PROVENANCE and reveals that the source material was deposited on a passive margin TECTONIC SETTING, after transport and recycling.

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  • Cite

    APA: Copy

    SANEI, SABA, HEJAZI, SEYED HASSAN, & HAIRAPETIAN, VACHIK. (2011). PETROGRAPHY AND GEOCHEMISTY OF THE FRASNIAN ZEFREH SANDSTONE (NORTHEAST OF ESFAHAN). JOURNAL OF THE EARTH, 6(21), 61-73. SID. https://sid.ir/paper/193040/en

    Vancouver: Copy

    SANEI SABA, HEJAZI SEYED HASSAN, HAIRAPETIAN VACHIK. PETROGRAPHY AND GEOCHEMISTY OF THE FRASNIAN ZEFREH SANDSTONE (NORTHEAST OF ESFAHAN). JOURNAL OF THE EARTH[Internet]. 2011;6(21):61-73. Available from: https://sid.ir/paper/193040/en

    IEEE: Copy

    SABA SANEI, SEYED HASSAN HEJAZI, and VACHIK HAIRAPETIAN, “PETROGRAPHY AND GEOCHEMISTY OF THE FRASNIAN ZEFREH SANDSTONE (NORTHEAST OF ESFAHAN),” JOURNAL OF THE EARTH, vol. 6, no. 21, pp. 61–73, 2011, [Online]. Available: https://sid.ir/paper/193040/en

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