Los peloides son aloquímicos que se componen de micrita, independientemente de su tamaño, forma u origen. Los dos tipos principales de peloides son los gránulos y los intraclastos. Otro tipo de peloide es el seudooolito.[1][2][3]
Referencias
- ↑ Folk, R.L. (1959) Practical petrographic classification of limestones. American Association of Petroleum Geologists Bulletin. 43, pp. 1-38.
- ↑ Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, J.A., eds. (2005) Glossary of Geology (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. ISBN 0-922152-76-4
- ↑ Scholle, P.A., and D.S. Ulmer-Scholle (2003) A Color Guide to the Petrography of Carbonate Rocks: Grains, textures, porosity, diagenesis. American Association of Petroleum Geologists Memoir no. 77. Tulsa, Oklahoma, American Association of Petroleum Geologists. 474 pp. ISBN 0-89181-358-6