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Information Journal Paper

Title

MINERALOGY AND GEOCHEMISTRY OF THE JURASSIC COALS FROM THE GHESHLAGH MINE, EASTERN ALBORZ

Pages

  369-383

Abstract

 IntroductionThe Alborz structural zone in northern Iran is the host of a number of important COAL deposits. The GHESHLAGH COAL mine is one of them, which is located 35 km southeast of Azadshahr. COAL bearing strata in the GHESHLAGH mining district occur in the middle part of the Lower Jurassic Shemshak Formation which consists mainly of shales, siltstones and sandstones. The Geshlagh COALs have a low sulfur content and a low ash yield. The ash content of COAL and its geochemical character depends on the environment of deposition and subsequent geological history (Yazdi and Esmaeilnia, 2004). The purpose of this study was to investigate the texural and mineralogical characteristcs of the Ghashlagh COALs and to identify the GEOCHEMISTRY of the major and TRACE ELEMENTS and their relationship to specific mineralogical components. These results are necessary to improve the understanding of COAL characterization and to relate the MINERALOGY of different materials to their potential for producing acidic or alkaline mine waters associated with mining and preparation processes.

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    APA: Copy

    SHAMANIAN, GHOLAM HOSSEIN, & HOSSEINI ASHLAGHI, FATEMEH. (2016). MINERALOGY AND GEOCHEMISTRY OF THE JURASSIC COALS FROM THE GHESHLAGH MINE, EASTERN ALBORZ. JOURNAL OF ECONOMIC GEOLOGY, 7(2), 369-383. SID. https://sid.ir/paper/180540/en

    Vancouver: Copy

    SHAMANIAN GHOLAM HOSSEIN, HOSSEINI ASHLAGHI FATEMEH. MINERALOGY AND GEOCHEMISTRY OF THE JURASSIC COALS FROM THE GHESHLAGH MINE, EASTERN ALBORZ. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2016;7(2):369-383. Available from: https://sid.ir/paper/180540/en

    IEEE: Copy

    GHOLAM HOSSEIN SHAMANIAN, and FATEMEH HOSSEINI ASHLAGHI, “MINERALOGY AND GEOCHEMISTRY OF THE JURASSIC COALS FROM THE GHESHLAGH MINE, EASTERN ALBORZ,” JOURNAL OF ECONOMIC GEOLOGY, vol. 7, no. 2, pp. 369–383, 2016, [Online]. Available: https://sid.ir/paper/180540/en

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