TY - JOUR ID - 40918 TI - Palaeoenvironmental conditions of Gheshlagh coal deposits (Eastern Alborz) based on evidences of petrography and facies JO - Scientific Quarterly Journal of Geosciences JA - GSJ LA - en SN - 1023-7429 AU - Rabani, T AU - Taghipour, N AU - Aharipour, R AD - M.Sc., School of Earth Sciences, Damghan University, Damghan, Iran AD - Assistant Professor, School of Earth Sciences, Damghan University, Damghan, Iran Y1 - 2016 PY - 2016 VL - 25 IS - 99 SP - 271 EP - 280 KW - Coal KW - Shemshak KW - Paleoenvironment KW - Gheshlagh KW - Eastern Alborz DO - 10.22071/gsj.2016.40918 N2 - Gheshlagh district contains coal deposits in a large syncline in Shemshak group sediments in East Alborz. To determine the palaeoenvironmental setting of the coal deposits based on organic and mineral components, eleven samples from coal seams from four active mines are collected. Minerals such as quartz, kaolinite, pyrite, siderite, biotite, montmorillonite and dolomite are identified in Gheshlagh coal mines. The Ground Water Index (GWI) suggests ombrotrophic hydrological conditions for coal layers in Gheshlagh coal region. K13 and k11 layers have much higher GWI among others due to its higher mineral content than other layers. Vegetation index (VI) of the Gheshlagh coals is less than 3, which could indicative of the dominance of aquatic/herbaceous plants in the formation of coal seams. Petrographic data on organic and inorganic matter with facies diagram suggest evidences of anaerobic to low oxygen, alkaline conditions and variations in water level with relative proximity to the marine environment. UR - http://www.gsjournal.ir/article_40918.html L1 - http://www.gsjournal.ir/article_40918_c49ee9a43e348aa54d8ee470d56ccf41.pdf ER -