Time-Dependent CO<sub>2</sub>-Brine-Rock Interaction Effect on Sand Onset Prediction: A Case Study of Dolomite-Rich Sandstone in Air Benakat Formation, South Sumatra, Indonesia. [PDF]
Abdul Aziz P +3 more
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Sedimentary conditions drive modern pyrite burial flux to exceed oxidation. [PDF]
Mertens C, Paradis S, Hemingway JD.
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Evolution of carbonate platforms in the northeast Red Sea during the last 23Â million years. [PDF]
Pensa T +5 more
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Oblique distribution patterns and the underlying mechanical model of orebody groups controlled by structures at different scales. [PDF]
Han R, Wu J, Zhang Y, Chen Q, Sun B.
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Dolomitization and the causes of dolomitization dolomite reservoir
Chinese Journal of Geochemistry, 2012This paper utilizes multi-methods, such as core observation, slice identification, isotope analysis, trace element analysis, fluid inclusion technique and so on, to study the causes of the dolomite in the Nanpu Sag and the origins of the dolomite reservoir.
Bojiang Fan +4 more
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Estimation of Dolomite Formation: Dolomite Precipitation and Dolomitization
Journal of the Geological Society of India, 2016Abstract: Reactive-transport models are developed here that produce dolomite via two scenarios: primary dolomite (no CaCO3 dissolution involved) versus secondary dolomite (dolomitization, involving CaCO3 dissolution). Using the available dolomite precipitation rate kinetics, calculations suggest that tens of meters of thick dolomite ...
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Chapter 7 Dolomites and Dolomitization
1979Publisher Summary This chapter discusses dolomites and dolomitization. There are numerous kinds of dolomite. According to numerous investigators, primary precipitation of dolomite crystals, particularly in marine environments, probably represented in Holocene carbonate sediments, is of little significance when considering the great bulk of ancient ...
George V. Chilingar +3 more
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Dolomitization, Dolomite Distribution, Reservoir Rocks: ABSTRACT
AAPG Bulletin, 1970Approximately 80% of the hydrocarbon reserves in carbonate rocks in North America are found in rock that is essentially pure dolomite. In many reservoirs the field limits are determined by the distribution of dolomite, because the dolomitization process is conducive to the production of a favorable reservoir rock.
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II.—Dolomitization and the Leicestershire Dolomites
Geological Magazine, 1918In the district north of Ashby-de-la-Zoueh dolomitized Carboniferous Limestone crops out where the Leicestershire border adjoins that of South Derbyshire. The dolomites, which attain a thickness of nearly 900 feet in this area, have hitherto received very little attention.
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