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There is a page named "Dolomite" on this wiki. See also the other search results found.
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- [[File:1280px-Dolomite-Magnésite- Navarre.jpg|thumb|300px|Dolomite et magnésite - Carrière Azcárate, Eugui, Esteribar, Navarre, Espagne. Ph ...disordered arrangement of ions occupies more volume than that of the ideal dolomite structure and is unstable with respect to an ordered phase.9 KB (1,409 words) - 19:14, 3 March 2016
File:1280px-Dolomite-Magnésite- Navarre.jpg Dolomite et magnésite - Carrière Azcárate, Eugui, Esteribar, Navarre, Espagne. Ph(1,280 × 995 (139 KB)) - 14:19, 20 November 2014- ...formation of dolomite is called dolomitization (Tucker and Wright, 1990). Dolomite is dominantly a marine mineral / rock but it can also be formed in continen The origin of dolomite is still debateable and different models have been proposed by different re38 KB (4,996 words) - 21:07, 21 April 2022
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File:CN24FG3.jpg ...ite, and such crystals are metastable with respect to ideal stoichiometric dolomite. Photograph by Richard Reeder. From Land, Lyndon S., 1982, Dolomitization:(496 × 611 (128 KB)) - 20:47, 15 July 2015File:Sem-xrd-cl-and-xf-methods fig5.png ...<sup>+2</sup> dolomite shows up as bright bands and higher Fe<sup>+2</sup> dolomite as dark bands. Copyright: W. J. Myers.(1,004 × 725 (583 KB)) - 22:29, 14 January 2014- ...189</ref> Limestone (calcium carbonate, CaCO<sub>3</sub>) is dissolved and dolomite (CaMg(CO<sub>3</sub>)<sub>2</sub>) is precipitated in the presence of magn592 bytes (87 words) - 20:42, 7 July 2016
- ...]. Carbonate rocks composed mainly of the mineral dolomite are also called dolomite (formerly [[dolostone]]). When metamorphosed both rocks become marble.708 bytes (95 words) - 20:42, 7 July 2016
File:1280px-Dolomite-Magnésite- Navarre.jpg Dolomite et magnésite - Carrière Azcárate, Eugui, Esteribar, Navarre, Espagne. Ph(1,280 × 995 (139 KB)) - 14:19, 20 November 2014File:Evaluating-diagenetically-complex-reservoirs fig1.png ...unty, Montana, showing extreme irregularities in the development of porous dolomite zones in the Red River Formation below the C-anhydrite. (From Longman et al(952 × 409 (46 KB)) - 18:46, 14 January 2014File:Full-waveform-acoustic-logging fig3.png ...(ΔΔT) against the core-measured permeability values for both the limestone-dolomite and the sand-shale examples. (After Burns et al., 1988.)(948 × 1,299 (12 KB)) - 14:23, 29 August 2014File:CN24FG1.jpg Schematic representation of the crystal structure of dolomite showing the alternation of cation and anion (carbonate) planes, and the alt(590 × 715 (71 KB)) - 20:14, 15 July 2015File:M91FG199.JPG ...diagram shows three tidal flat reservoir cycles in the Permian San Andres dolomite of the northern Delaware basin in New Mexico and Texas (after Shinn, 1983).(800 × 1,089 (126 KB)) - 13:11, 20 August 2015- [[File:1280px-Dolomite-Magnésite- Navarre.jpg|thumb|300px|Dolomite et magnésite - Carrière Azcárate, Eugui, Esteribar, Navarre, Espagne. Ph ...disordered arrangement of ions occupies more volume than that of the ideal dolomite structure and is unstable with respect to an ordered phase.9 KB (1,409 words) - 19:14, 3 March 2016
- ...ional environment]]) || Low variability [variations of [[limestone]] and [[dolomite]] ] ...lay]], and [[anhydrite]], etc. || [[Aragonite]], high- and low-Mg calcite, dolomite3 KB (425 words) - 17:11, 5 April 2022
- ...nersoc.org/pages/Archive-MM/Volume_53/53-373-547.pdf saddle]] or nonplanar dolomite, ferroan [http://encyclopedia2.thefreedictionary.com/poikilotopic poikiloto ...Sequence_boundaries|sequence boundary]] in the updip portion of the Midale dolomite. These [[Wikipedia:Mesoporous material|mesoporous]] dolomites downdip form5 KB (611 words) - 21:06, 4 February 2022
- | [[Dolomite]] || 2.876 || 3.0 ...in limestone units and the formation you wish to evaluate is sandstone or dolomite, then correct the log value by using the appropriate chart in a log interpr12 KB (1,763 words) - 16:18, 5 April 2022
- | Continuous-phase oil || Yes || Yes || <65 for Ss, <45 for Ls or [[dolomite]] || Moveable oil || Free oil or oil-cut fluids || Hydrocarbon gradient | Residual oil || Yes || Yes || >65 for Ss, >45 for Ls or dolomite || No moveable oil || No recovery || Hydrostatic gradient8 KB (1,130 words) - 17:09, 5 April 2022
- ...acterization#Dolomitization|dolomitization]]. || colspan = 2 | Secondary [[dolomite]] reservoirs; Form as a result of localized secondary dolomitization. ...= 3 | Diagenetic traps || rowspan = 2 | Diagenetic reservoirs || Secondary dolomite reservoirs || [[Hydrothermal diagenesis]] || colspan = 2 | Ascending hot br5 KB (645 words) - 16:14, 13 April 2022
- ...orous [[mudstone]]”) is locally laminated and burrowed peloidal lime and [[dolomite]] mudstones to wackestones. These tighter rocks originated on a low-energy ...cal characteristics of the main nonreservoir facies in the field: lime and dolomite mudstones to wackestones. ]]6 KB (842 words) - 18:50, 4 December 2023
- ...rocks can be found as a clastic limestone, carbonate framework (reef), and dolomite. ===== Dolomite =====12 KB (1,741 words) - 23:03, 30 June 2015
- ...cal characteristics of the main nonreservoir facies in the field: lime and dolomite mudstones to wackestones.]] ...:Microporous material|microporosity]] formed by silt-sized (10μ or less) [[dolomite]] rhombs. [[Capillary pressure]] and [[Scanning electron microscopy (SEM)|S5 KB (659 words) - 16:54, 12 April 2022
- ...rocks can be found as a clastic limestone, carbonate framework (reef), and dolomite. ===== Dolomite =====12 KB (1,822 words) - 02:27, 1 July 2015
- ..._fig21-5.png|Figure 1]], both [[lateral]] and top seals in the [[Carbonate|dolomite]] reservoir were created by [[anhydrite]] cementation during early diagenes2 KB (297 words) - 21:06, 3 February 2022