Referencias bibliográficas

Referencias bibliográficas que se citan en este sitio Web:

  • Alpern, B., Bouroz, A., Delattre, Ch., Dollé, P., Mériaux, E., Nöel R. and Quinot, E. 1970. Pétrologie des charbons. Ann. Soc. Géol. Nord, 90 (4), 203-222.
  • Cohen, A.D., Spackman, W. and Raymond, R., 1987. Interpreting the characteristics of coal seams from chemical, physical and petrographic studies of peat deposits. In: A.C. Scott (Editor), Coal and Coal-Bearing Strata: Recent Advances. Geol. Soc. Spec. Publ., 32: 107-125.
  • Diessel, C.F.K., 1986. On the correlation between coal facies and depositional environments. Proc.20th Syrup., Dep. Geol., Univ. Newcastle, N.S.W., pp. 19-22.
  • Diessel, C.F.K. (1992). Coal-bearing depositional systems. Springer-Verlag Berlin Heidelberg, 721 p.
  • Hower, J.C., Esterle, J.S., Wild, G.D., and Pollock, J.D. (1990). Perspectives on coal lithotype analysis: Journal of Coal Quality, 9, 48-52.
  • International Committee for Coal Petrology (1957). International Glossary of Coal Petrology. CNRS, Paris.
  • International Organization for Standardization (ISO) 2005. Classification of coals. -ISO 11760: 2005, ISO, Geneva.
  • International Organization for Standardization (ISO) 2009. Methods for the petrographic analysis of coal. Part 3: Method of determining maceral group composition. –ISO 7404-3: 2009, ISO, Geneva.
  • Jennifer M.K. O’Keefe, Achim Bechtel, Kimon Christanis, Shifeng Dai ,William A. Di Michele, Cortland F. Eble, Joan S. Esterle ,Maria Mastalerz, Anne L. Raymond, Bruno V. Valentim, Nicola J. Wagner, Colin R. Ward, James C. Hower (2013). On the fundamental difference between coal rank and coal type. International Journal of Coal Geology, 118, 58-87.
  • Littke, R. and Rullköter, J. (1987). Mikroskopische und makroskopische Unterschiede zwischen Profilen unreifen und reifen Posidonienschiefers aus der Hilsmulde. Facies, 17, 171-180.
  • Mackowsky (1982). Minerales and trace elements occurring in coal. In: Stach’s Textbook of Coal Petrology, Gebr. Borntraeger, Berlin-Stuttgart, 356-361.
  • Porta, J., López-Acevedo, M. and Roquero, C. (2003). Edafología para la Agricultura y el Medio Ambiente. 3ª Edición. Mundi-Prensa. 929 pp
  • Rahmani, R.A. and Flores, R.M. eds. (1984). Sedimentology of Coal and Coal-Bearing Sequences. The International Association of Sedimentologist. Wiley, Oxford.
  • Smyth, M., 1984. Coal microlithotypes related to sedimentary environments in the Cooper Basin, Australia. Spec Publ., Int. Assoc. Sediment., 7, 333-347.
  • Stach, E. (1935). Lehrbuch der kohlenpetrographie. Borntraeger, Berlin,293 pp.
  • Stach, E. (1964). Zur Untersuchung des Sporinits in Kohlen-Anschliffen. Fortschr. Geol., Rheinld, u. Westf., 12, 403-420.
  • Stopes, M.C. (1919). On the four visible ingredients in banded bituminous coal. Proc. Royal Soc. 90B, 470-487.
  • Sotpes, M.C. (1935). On the petrology of banded bituminous coals. Fuel, 14, 4-13.
    Taylor, G.H. and Cook A.C. (1962). Sclerotinite in coal and other organic-rich rocks. Fuel, 66, 1269-1273.
  • Taylor G.H. and Liu, S.Y. (1987). TEM and coal structure. In: Moulijn, J.A. et al (Eds): Int. Conf. on Coal Science, Maastricht, The Netherlands, Elsevier, 29-32.
  • Taylor G.H., Teichmüller, M., Davis, A., Diessel, C.F.K., Littke R. and Robert, P. (1998). Organic Petrology: a new handbook incorporating some revised parts of Stach’s Textbook of Coal Petrology. Gebrüder Borntraeger, Berlin, Stuttgart, 704 p.
  • Teichmüller, M. (1944). Zur Petrographie zweier oberschlesischer Flöze mit ähnlichem Inkohlungsgrad, aber verschiedenen Kokungseigenschaften. Z. prakt. Geol, 52, 1-6.
  • Teichmüller, M. (1974). Über neue Macerale der Liptinit-Gruppe und die Entstehung von Micrinit. Fortschr. Geol. Rheinld. u. Westf., 24, 37-64.
  • Teichmüller, M. (1989). The genesis of coal from the viewpoint of coal Petrology. International Journal of Coal Geology, 12, 1-87.
  • Thomas, L. (2013). Coal Geology (2ª Ed). Wiley-Blackwell, Oxford, 444 p.
  • Ward, C.R. (1984). Coal Geology and Coal Technology, Balckwell Scientific Publications, Oxford, 345 pp.