Matches in DBpedia 2016-04 for { <http://wikidata.dbpedia.org/resource/Q3736526> ?p ?o }
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- Q3736526 subject Q7153706.
- Q3736526 subject Q7163795.
- Q3736526 subject Q8335573.
- Q3736526 subject Q8386873.
- Q3736526 subject Q8386875.
- Q3736526 subject Q8549587.
- Q3736526 subject Q8566423.
- Q3736526 abstract "Dolomitization is a process by which dolomite is formed when magnesium ions replace calcium ions in calcite. It is common for this mineral alteration into dolomite to take place due to evaporation of water in the sabkha area. Dolomitization involves substantial amount of recrystallization. This process is described by the stoichiometric equation:2 CaCO3(limestone) + Mg2+ ↔ CaMg(CO3)2(dolomite) + Ca2+Dolomitization depends on specific conditions which include low Ca:Mg ratio in solution, reactant surface area, the mineralogy of the reactant, high temperatures which represents the thermodynamic stability of the system, and the presence of kinetic inhibitors such as sulfate.If the kinetic inhibitors and high temperatures are compatible then dolomitization can take place in saline environments above thermodynamic and kinetic saturation with respect to dolomite. This type of environment includes, freshwater and seawater mixing zones, normal saline to hypersaline subtidal environments, schizohaline environments (fluctuating salinity: fresh-water to hypersaline conditions) and hypersaline supratidal environments. When requirements are fulfilled dolomitization can take place in alkaline environments which are those under the influence of bacterial reduction and fermentation processes, and areas with high input alkaline continental groundwaters. Environments with high temperatures (about 50 °C) such as subsurface and hydrothermal environments are conducive to dolomitization.".
- Q3736526 wikiPageWikiLink Q1036221.
- Q3736526 wikiPageWikiLink Q10876.
- Q3736526 wikiPageWikiLink Q1134814.
- Q3736526 wikiPageWikiLink Q167741.
- Q3736526 wikiPageWikiLink Q17103888.
- Q3736526 wikiPageWikiLink Q171917.
- Q3736526 wikiPageWikiLink Q172290.
- Q3736526 wikiPageWikiLink Q180621.
- Q3736526 wikiPageWikiLink Q213185.
- Q3736526 wikiPageWikiLink Q36496.
- Q3736526 wikiPageWikiLink Q41760.
- Q3736526 wikiPageWikiLink Q4649909.
- Q3736526 wikiPageWikiLink Q637600.
- Q3736526 wikiPageWikiLink Q660.
- Q3736526 wikiPageWikiLink Q706.
- Q3736526 wikiPageWikiLink Q7153706.
- Q3736526 wikiPageWikiLink Q7163795.
- Q3736526 wikiPageWikiLink Q82682.
- Q3736526 wikiPageWikiLink Q8335573.
- Q3736526 wikiPageWikiLink Q8386873.
- Q3736526 wikiPageWikiLink Q8386875.
- Q3736526 wikiPageWikiLink Q8549587.
- Q3736526 wikiPageWikiLink Q8566423.
- Q3736526 comment "Dolomitization is a process by which dolomite is formed when magnesium ions replace calcium ions in calcite. It is common for this mineral alteration into dolomite to take place due to evaporation of water in the sabkha area. Dolomitization involves substantial amount of recrystallization.".
- Q3736526 label "Dolomitization".