Lignite (ulminite reflectance Rr = 0.27%) from the Szczerców deposit (Central Poland) is dominated by huminite group macerals, containing a high proportion of attrinite and densinite. Densinite ulminite are more abundant in small aromatic units than attrinite, which may result their stronger gelification. The differences Raman spectral characteristics between pronounced Fusinite, comparison wit...

Coal contains a complex network of nano-, meso-, and macro-pore can store fluids allow to flow through it. Nanoporosity in coal is primarily result molecules that have aromatic molecular structures been preserved coal. Most adsorbate compounds, including gases, are stored here. The study area located South Sumatera, West Merapi Area, Lahat Regency. Geologically, the Sumatra Basin belongs Middle...

detailed organic petrography analysis were conducted on drill core and cutting samples from the nahr umr (middle albian), burgan (lower albian) and ratawi (hauterivian) formations on the soroosh and nowrooz fields, nw part of the iranian sector of the persian gulf. the thermal maturity of the middle albian nahr umr formation appears to have reached the top of the oil window. the underlying burg...

the petroleum potential of the seyahou (ordovician) and sarchahan (lower silurian) formations in northern bandar abbas has not been investigated sufficiently. these sediments crop out as thinly laminated shales and are about 100 meters thick. a number of thirty-five selected samples were subjected to rock-eval pyrolysis followed by transmitted, reflected and uv light microscopy together with cl...

the alborz coal basin is located in northern part of iran. the coal deposits of shahrood in eastern alborz, zirab in central alborz and abyek in western alborz were studied as typical coalfields of the basin. shemshak formation which is the main coal-bearing sequence was formed during the triassic-jurassic in the basin. it consists of sandstone, siltstone, shale and claystone, which variedly al...