Univrsity of Tehran Press Geopersia 2228-7817 8 1 2018 01 01 Provenance, Tectonic Setting & Geochemical Maturity of The Early Miocene Pyawbwe Formation, Sakangyi –Thayet Area, Magway Region, Myanmar. - 1 12 63298 10.22059/geope.2017.230212.648314 EN Mostafa Hamad Cairo university, Faculty of Science, Geology Department, Egypt Reda Mahmoud El-Gammal Consultant , Geology and Mining, GeoMine Mining Company, Cairo,Egypt. Soe Moe Lwin Geology Department, Faculty of Science, Yangon university, East Yangon. Myo Min Aung Geology Department, Faculty of Science, Yangon university, East Yangon. Journal Article 2017 04 12 Abstract<br /> The best exposed Early Miocene (820 m. thick. ) shales and interbedded silty sandstones beds of the Pyawbwe Formation at Sakangyi- Thayat area,Magway Region are investigated geochemically by using Siemens SRS- X Ray 303 AS XRF Spectrometer. Major and some trace element concentrations have been determined to achieve their provenance, tectonic setting ,paleoweathering , paleoclimate and sedimentation characteristics. The geochemistry of sediments is particularly valuable in the study of fine-grained rocks that are difficult to characterize through petrographic studies. Geochemical data revealed that the felsic granitic plutonic provenance of moderate relief of arc massif exposed on tectonically calm continental margin which is probably the Shan- Thai continental block eastern and northeastern Myanmar . Average values of both Chemical Index of weathering (CIW) and Chemical Index of Alteration (CIA) ( 77.4 and 67.3 respectively ) suggest a moderately chemical weathering condition prevailed during transportation and deposition on passive shallow margin as progressive mature sediments. https://geopersia.ut.ac.ir/article_63298_a9fe9d33a4fd8f4e64a6796b04bcb58d.pdf