is dolomite a secondary product of alteration of line

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  • carbonate an overview ScienceDirect Topics

    The most abundant carbonate minerals are calcite CaCO3 and dolomite CaMg CO3 2 Secondary minerals are anhydrite chert and quartz Accessory Ca and carbonate ions or by chemical alteration of line or calcareous mud dolomitization Typical products are alizarine red for staining calcite red colour

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  • History of Geology The Dolomite Mountains and the Dolomite

    Aug 31 2010 In the 19th century the genesis of both the Dolomite Mountains as the rock forming or a secondary product of alteration of common line

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  • Grain production terrigenous GEOL 4500 Sedimentary Geology

    Examples include quartz opal calcite dolomite and hematite Secondary minerals form at the site of weathering by the chemical Physical weathering involves the breakage of rocks into smaller fragments with no significant change in chemistry or mineralogy Sedimentary Rocks as Products of Subaerial Weathering

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  • Line Wikipedia

    Line is a sedimentary rock composed mainly of skeletal fragments of marine organisms such as coral forams and molluscs Its major materials are the minerals calcite and aragonite which are different Secondary calcite may be deposited by supersaturated meteoric waters groundwater that precipitates the

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  • Lecture Weathering

    Subaerial Physical Chemical Weathering Rates Products Submarine Soils characteristics of the parent rock or may be altered – chemical resistance Calcite carbon dioxide water ⇔ Calcium bicarbonate CaCO3 line parent rocks – residues 2 secondary minerals formed by in situ chemical

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  • ALTERATION OF THE BOOTSTRAP LINE NORTHERN

    the study area line diagenetic planar dolomite saddle dolomite ferroan dolomite and talc as alteration products Evans 2000 Emsbo et al 2003 A second has created secondary porosity in the tight Bootstrap line unit

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  • Dolomite occurrence evolution and economically Saltwork

    Dolomite is a metastable mineral early formed crystals can be replaced by later more stable phases with such replacements the Holocene to form extensive areas of secondary Ž dolomite an ion activity product of the order of 10y15 01 It tion of a line by modern seawater Hsu 1967 as conditions change

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  • University of Minnesota 39 s Mineral Pages Dolomite

    Dolostones that formed from the alteration of line rock can retain much of the to this is primary dolomite that forms in evaporitic settings as a relatively late product Secondary sedimentary dolomites can be broadly separated into two

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  • paleoenvironmental isotope geochemistry and paragenesis of

    sequence of palustrine and lacustrine line and dolostone freshwater to saline lake system primary or early secondary formation of micritic dolomite episodic exposure and destabilization and alteration of primary carbonate phases Flagstaff were likely the product of a lake that was already somewhat

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  • The Mysterious Microbial Origin of Mountains Scientific American

    Jun 21 2012 was if the dolomite rock or dolostone was a primary product of marine deposition or a secondary product of alteration of common line

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  • How can we explain the presence of calcite as secondary product

    line is a sedimentary rocks so it is not crystallization product of magma Prof Aiman Aiman Eid Al Rawajfeh 4 years ago In this case calcite is not secondary product Prof Aiman Alteration product of volcanic tuff calcic plagioclase

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  • Minerals of Vesuvius Mineralogical Society of America

    I Minerals that are found in the ejected line blocks of Monte Somma 2 II Pneumatolytic minerals LIMONITE occurs as an alteration product of iron minerals CALCITE c PEROVSKITE small black crystals in geodes with spinel calcite and apatite vr APATITE CHALCANTHITE a secondary product r

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  • CHAPTER 5 – SECONDARY MINERALS IN THE LHZBG AND PCR

    hornblende and tremolite occur in association with dolomite and talc commonly occur as an alteration product in rocks rich in olivine Deer et al 1997 pelites basic and ultrabasic rocks siliceous line and dolomite Deer et al

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  • a review of the dolomite and line industry in south africa DMR

    Year on year change Lime line and dolomite products are 1 Expanded set of secondary applications for line dolomite and lime products see

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  • Terminology of Line and Related Rocks An CiteSeerX

    line calcitic dolomite or dolostone marl marlstone oi lite o6id coquina coquinite and coquinoid ferred carbonate rocks also if the alter sible examples of products of the second position in the rock fabric secondary

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  • The Evolution of Line and Dolomite I JStor

    Origin of dolomite by secondary replacement of line C Evolution versus Resume of calcium and magnesium in the products of metamorphism 323 This content Daly 39 has suggested that it is due to a change in the nature of the life

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  • Techniques for Determining Line Composition and Reactivity

    Jan 10 2009 Mineralogically line may be regarded as calcite magnesian calcite sizing product quality wastewater treatment line consumption rate in pH will change the reaction rate rendering results inconclusive The NIST SRM 88b sample data uses the secondary axis time scale located on top

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  • Determination of elemental concentrations of dolomite dolerite and

    Serpentines are a class of secondary minerals derived by alterations in magnesium bedding planes separated by wrpentinised dolomitic line They are also found in the rock serpentinite an alteration product of olivine bearing rocks

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  • Dolomite A sedimentary rock known as dolostone or dolomite rock

    Dolomite is found in sedimentary basins worldwide It is thought to form by the postdepositional alteration of lime mud and line by magnesium rich

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  • PDF 3 3

    almost invariably a secondary rather than a primary sedimentary mineral meaning that carbonate sediments don 39 t start their lives as dolomite Much dolomite is contrast to usually gray weathering line 2 7 The other D are called the products whereas if the reaction goes to the left A and B are the products and C

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  • Dolomitization Mechanism Based on Petrography and Geochemistry

    Geochemical studies have revealed that the dolomites of Shotori Formation have The variety of dolomites accounts for their Formation time source and early line dolomites and hence is interpreted as the final product of dolomitization secondary diagenetic dolomites which is due to the change in their fabric

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  • line Missouri Department of Natural Resources MO

    of living Products derived from line are abundant line products require rock with specific particular line or dolomite deposit will dictate applications LIME Lime plays a agricultural field to change the physical and chemical properties of finely crushed line with secondary raw materials such as

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  • Techniques for Determining Line Composition and Reactivity

    Oct 1 2009 Mineralogically line may be regarded as calcite magnesian calcite sizing product quality wastewater treatment line consumption rate in pH will change the reaction rate rendering results inconclusive The NIST SRM 88b sample data uses the secondary axis time scale located on top

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  • Dolomitic Lime Amendment Affects Pine Bark Substrate pH Nutrient

    The two primary line products used in agriculture include calcitic lime 2 discuss the primary and secondary effects of DL on nutrient availability and 3 of this empirical relationship is that dolomite will cause a pH change up to ≈6 5

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  • Formation of Forsterite by Silicification of Dolomite during Contact

    Jul 27 2011 Some rocks with reactants and products of reaction 1 and 2 contain Forsterite in the four samples is partially altered to an intergrowth of serpentine and brucite because dolomite and dolomitic line at the lowest grade in the Beinn Secondary Ion Mass Spectrometry in the Earth Sciences

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  • Dolomites Encyclopedia

    Dolomite rocks are originally deposited as calcite aragonite rich line but The symbol means that the vitamin and mineral manufacturer 39 s product has cleavage perfect rhombohedral 1011 usually secondary having formed by the calcium magnesium carbonate CaMg CO 3 2 found in altered lines

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  • Hydrothermal Alteration of Line and Mineral Exploration of Zn

    ment of Fe and Mn was more conspicuous in calcite and chlorite in skarn deposits The occurrence and minerals expected to be present in altered line and so either of the minerals to secondary minerals Nakano et al 1991 In order to widespread product of the alteration in Zn type skarn deposits that

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