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Journal ArticleDOI

An isotopic study of siderites, dolomites and ankerites at high temperatures☆

J Rosenbaum, +1 more
- 01 Jun 1986 - 
- Vol. 50, Iss: 6, pp 1147-1150
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TLDR
In this paper, an empirically derived relationship between the chemical composition of a carbonate in the CaCO3-(Ca, Mg)(CO3)2-FeCO3 system and the function 103 In α at 100°C is 103 ∆ α = 8.94XCaCO3 + 9.29XMgCO3+ 8.77XFeCo3 where Xi is the mole percent of component i in the carbonate.
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This article is published in Geochimica et Cosmochimica Acta.The article was published on 1986-06-01. It has received 768 citations till now. The article focuses on the topics: Carbonate & Ankerite.

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Citations
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Isotopic signatures of deposition and transformation of Lower Cambrian saliferous rocks in the Irkutsk Amphitheater: Communication 3. Carbon and oxygen isotopic compositions in carbonates

TL;DR: In this paper, a similar conclusion was made from the strontium isotopic composition of carbonate rocks in the Irkutsk Amphitheater, and the major elements of the evolution of carbon isotope signature could be retained since the sedimentation stage.
Journal ArticleDOI

Processes Associated with Multiphase Dolomitization and Other Related Diagenetic Events in the Jurassic Samana Suk Formation, Himalayan Foreland Basin, NW Pakistan

TL;DR: In this paper , a comprehensive study on the diagenetic changes, particularly dolomitization patterns in the Jurassic carbonates (Samana Suk Fm) in the Lesser Himalayan fold and thrust belt, NW Pakistan, is presented.
Journal ArticleDOI

Aragonite–calcite veins of the ‘Erzberg’ iron ore deposit (Austria): Environmental implications from young fractures

TL;DR: In this paper, the growth dynamics and environmental dependencies of these vein fillings were analyzed, and these analyses were further complemented by modern water analyses from different Erzberg sections.
Journal ArticleDOI

Hydrothermal dolomitization of basinal deposits controlled by a synsedimentary fault system in Triassic extensional setting, Hungary

TL;DR: In this paper, the authors proposed a conceptual model of dolomitization in the Buda Hills and Danube-East blocks, which suggests that pervasive dolombization occurred not only within and near the fault zones, but also within the breccia zones of the underlying basement block.
Dissertation

Does oil emplacement stop diagenesis and quartz cementation in deeply buried sandstone reservoirs

TL;DR: In this paper, the authors used core samples, wireline logs and well reports collected from the oil and water legs and the transition zone of Upper Jurassic marine sandstones of the Ula and Tambar fields from the Norwegian North Sea.
References
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Journal ArticleDOI

Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxide

TL;DR: In this paper, Niee's and Solenhofen standards were compared to the Chicago PDB standard for carbon and oxygen isotope ratios, and the correction factors for instrumental effects and for the nature of the mass spectra were derived.
Journal ArticleDOI

On the Isotopic Chemistry of Carbonates and a Paleotemperature Scale

TL;DR: In this paper, the temperature variation of the fractionation of oxygen in exchange reactions between dissolved carbonate and water and between calcite and water was calculated on theoretical grounds, and checked experimentally.
Journal ArticleDOI

The use of bromine pentafluoride in the extraction of oxygen from oxides and silicates for isotopic analysis

TL;DR: In this paper, a technique was developed in which bromine pentafluoride was used as a reagent for quantitative liberation of oxygen from oxides and silicates, and the results of isotopic analyses were compared with measurements made in other laboratories by other procedures.
Journal ArticleDOI

Measurement of O18O16 ratios of total oxygen of carbonates

TL;DR: The commonly used phosphoric acid procedure for the determination of oxygen isotope abundances in carbonates involves a large kinetic isotope effect as mentioned in this paper, which leads to an overestimate of the dolomite-calcite oxygon isotope fractionation by 0.8 per mil.
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