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Early carbonate diagenesis (view source)
Revision as of 14:02, 5 February 2014
, 14:02, 5 February 2014→Marine phreatic environment
==Marine phreatic environment==
==Marine phreatic environment==
The marine phreatic environment, in most cases, is where carbonate sediments originate and begin their diagenetic history. It can be divided into two distinct zones that represent two ends of a spectrum:<ref name=ch09r35>Longman, M., W., 1980, Carbonate diagenetic textures from nearsurface diagenetic environments: AAPG Bulletin, vol. 64, no. 4, p. 461–487.</ref>
The marine phreatic environment, in most cases, is where carbonate sediments originate and begin their diagenetic history. It can be divided into two distinct zones that represent two ends of a spectrum:<ref name=ch09r35>Longman, M., W., 1980, [http://archives.datapages.com/data/bulletns/1980-81/data/pg/0064/0004/0450/0461.htm Carbonate diagenetic textures from nearsurface diagenetic environments]: AAPG Bulletin, vol. 64, no. 4, p. 461–487.</ref>
* Active marine zone where water flow combined with other factors result in precipitation of aragonite or magnesium (Mg) calcite.
* Active marine zone where water flow combined with other factors result in precipitation of aragonite or magnesium (Mg) calcite.