
Differentiation of calcite veins and surrounding rocks
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The origin of fluid in calcite veins and its implications for
2020年12月1日 Some calcite veins share carbon isotopic characteristics and REEs distribution pattern with the surrounding rocks, revealing that the dissolution/buffering of the surrounding rocks and the pore fluid in the carbonate diagenesis are involved2017年6月15日 Planar calcite veins appear to postdate compaction and have sparser and thinner twins than those of their folded counterparts (Figure 4c) Therefore, development of calcite veins persisted throughout the burial and Regional‐scale development of opening‐mode calcite 2023年8月1日 Powdered calcite samples from 13 calcite veins and 20 wall rocks were used for stable oxygen and carbon isotopes analyses In this paper, four geochemical methods were used to analyze the properties, compositions, and isotopic ratios of the minerals in the fracturesGeochemistry of syntaxial calcite veins in ultradeep sandstone 2020年12月7日 The Somerset veins show abundant microstructural evidence for syntaxial veinfilling mechanisms, including crystal terminations towards the vein interior, cathodoluminescence banding patterns that are interpreted as growth zoning from the vein walls towards the centre, Formation of wideblocky calcite veins by extreme growth

Kinematics of Crystal Growth in Single‐Seal Syntaxial
2021年9月4日 Syntectonic syntaxial calcite or quartz veins are ubiquitous in rocks at low metamorphic grades in the upper and middle crust (Passchier Trouw, 2005; Ramsay Huber, 1983 )2024年3月11日 Calcite veins in limestone significantly influence its mechanical behavior and fracture extension: (a) Laterally distributed calcite veins often induce stress concentration in the rock massInvestigations on the effect of natural veined calcite on the 2021年2月5日 Here we combined phasefield modeling with microtextural analysis of previously unexplained wideblocky calcite veins in natural limestone and of the fresh fracture surface in this limestone Results show that the wideblocky vein textures can only be reproduced if Wideblocky veins explained by dependency of crystal growth rate 2021年7月28日 We show that (a) calcite veins in mylonite and nonmylonitic schist experienced differential stresses of ∼28–135 MPa at temperatures ∼200–400°C, and (b) calcite veins in foliated cataclasites and ultracataclasites Using Syntectonic Calcite Veins to Reconstruct the
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The origin of fluid in calcite veins and its implications for
2020年12月1日 The highangle, structural genetic calcite veins of the Ordovician in the ShunnanGucheng area in the Tarim Basin provide a convenient study of fluid properties, hydrocarbon migration, and2024年6月1日 The carbon and oxygen isotopes of calcite veins and the surrounding rocks were also analyzed The testing process involved first extracting in situ calcite samples using a small microdrill The calcite was then separated and purified to achieve a purity of more than 99%Further study on the genesis of lamellar calcite veins in lacustrine Even though all magmas originate from similar mantle rocks, and start out as similar magma, other things, like partial melting and crystallization processes like magmatic differentiation, can change the chemistry of the magma This 44: Partial Melting and Crystallization Geosciences 2017年6月1日 Overall, the mechanical behaviour is largely influenced by the orientation and thickness of calcite veins in basaltic rocksKeywordCalcite veinsMechanical behaviourFailure modeBasaltOrientation of Quantifying the effects of vein mineralogy, thickness, and orientation
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Bleached mudstone, iron concretions and calcite veins: A natural
2016年10月1日 Request PDF Bleached mudstone, iron concretions and calcite veins: A natural analogue for the effects of reducing CO 2 bearing fluids on iron migration and mineralization, sealing properties 2014年6月1日 Images showing the distribution of subsample locations in calcite veins and calcite crystals (inserted scanning electron microscope images) Growth directions (arrows) and breaks of vein growth or Source and character of syntaxial hydrothermal calcite veins in 2021年5月12日 Carbonate minerals are ubiquitous in most sedimenthosted mineral deposits These deposits can contain a variety of carbonate types with complex paragenetic relationships When normalized to chondritic values (CN), rareearth elements and yttrium (REE+YCN) can be used to constrain fluid chemistry and fluidrock interaction processes in both low and high Rareearth elements and yttrium (REE+Y) SpringerFurther study on the genesis of lamellar calcite veins in lacustrine black shaledA case study of Paleogene in Dongying Depression, China GuanMin Wang*, YunJiao Zhang, ZiYuan wards the two boundaries of the surrounding rocks This growth pattern resembles the muscle fiber of an animal, earning it the nickname ‘Beef’ (Lang et al,1923 Further study on the genesis of lamellar calcite veins in lacustrine
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(PDF) Geochemistry of Calcite Veins: Records of Fluid
2013年12月31日 Detailed geochemical investigations of calcite veins, genetically related to intrusions and veinhosting bedrock, have been used to indicate fluid evolution during intrusionrelated hydrothermal 2023年7月4日 Distribution pattern of rare earth elements between veins of Triassic Qinglong Formation and surrounding rocks in Huangqiao area, Subei Basin 42 方解石脉体 C 、 O 同位素特征Formation time and fluid source of calcite veins and geological Determination of mass changes in altered rocks surrounding selected epithermal deposits suggest Si, K, and Al gains and Na and Ca losses increasing in intensity toward ore veins, consistent with Photomicrographs of calcite paragenesis in altered rocks A Calcite 2021年11月8日 Many authors recognized the association of fibrous calcite (±quartz) veins with hydrocarbon generation during thermal maturation of organic matter (Bredehoeft et al 1976;Osborne Swarbrick Age, material source, and formation mechanism of beddingparallel
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The genesis of calcite and dolomite carbonatiteforming magma
2023年9月15日 Note that we refer in the title of this polemic to ‘carbonatiteforming magmas’ rather than the commonly used ‘carbonatite magma’ or ‘carbonatite melt’, as the actual composition of any calcite or dolomite carbonatiteforming magma is not known Typically, many carbonatites appear to be rocks formed by crystal fractionation from a variety of 2019年12月17日 The similar ⁸⁷Sr/⁸⁶Sr and δ¹³C values of the calcite veins and surrounding host rocks, combined with the relatively uniform fluid δ¹⁸OVSMOW values, indicate that the calcite SmNd isochron dating and geochemical (rare earth2021年11月1日 Carbonatites are a rare variety of igneous rocks enriched in niobium (Nb), rare earth elements (REE), uranium (U), thorium (Th), phosphorous (P), strontium (Sr), barium (Ba), and other incompatible elements (Gittins, 1988)Some of carbonatites are characterized by Nb–REE mineralization, rendering them to be of special economic importance, and hence Genesis of carbonatite and associated U–Nb–REE mineralization at 2021年2月1日 UPb dating of calcite veins allows direct dating of brittle deformation events Here, we apply this method to hydrothermal calcite veins in a foldandthrust belt and a large scale strikeslip (PDF) Insitu calcite UPb geochronology of hydrothermal veins

(PDF) Widespread beddingparallel veins of fibrous calcite (“beef
2009年6月17日 Veins mineralization consists mainly of calcite, but some have accessory constituents intercalated with fibers such as the surrounding rock fragments (Liu et al, 2017b;Ukar et al, 2017a 2024年6月6日 The Middle Atlas hosts calcite veins of considerable economic value, being found in the Mahdi and Bou Naceur ridges in the eastern part of the Moroccan Middle Atlas In this study, we aim to identify the fundamental factors controlling mineralization, which could be essential for the exploration of calcite minerals Jurassic dolomites and limestones host calcite Identification, Characterization, and Deposit Model of Calcite 2018年10月1日 Beddingparallel, fibrous calcite veins (commonly referred to as “beefs”) are widely developed within Eocene, lacustrine, laminated organicrich source rocks in the Dongying Depression of Formation of beddingparallel, fibrous calcite veins in laminated –Field views of the main outcrop of metamorphic rocks dilated by pervasive calcite veins: A) Panoramic view of SP251 km9 outcrop; B) Outcrop view of the red veins consisting of micropeloidal facies filling the fractures; C) Detail of the metamorphic rocks cut by two generations of neptunian dykes with different compositions, ie Pliensbachian shallowwater carbonates Pervasive calcite veins and cleavage dilation in lowgrade
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The Occurrence of BeddingParallel Fibrous Calcite
1 Introduction Beddingparallel fibrous calcite veins are found in sedimentary rocks from Cambrian to Palaeogene strata in many locations worldwide (Cobbold and Rodrigues, 2007; Cobbold et al, 2013; Heindel et al, 2015; Kershaw and 2021年3月11日 The orecontrolling surrounding rocks are primarily Linglong granite and Guojialing granodiorite; in which the ore is composed of quartz and calcite veins and contains a small amount of pyrite the P in the oreforming fluid is less likely to originate from the crust or wall rock differentiation fluidMicroGeochemistry of Pyrite and Gold Mineral in Jiaodong2024年9月1日 We report herein for the first time the occurrence of lowgrade metamorphic rocks dilated by the growth of calcite veins induced by microbial communities inhabiting the cleavage planesPervasive calcite veins and cleavage dilation in lowgrade 2014年2月1日 Field observation shows that multiple phases of calcite veins occur along fractures in the Ordovician, Permian and Triassic of overthrust belts and foldthrust belts in Jingshan region, MidYangtze(PDF) Genesis of calcite vein and its implication to petroleum

The Role of Reductive Carbonaceous Surrounding Rocks in the
2023年7月17日 CH4 is commonly present in fluid inclusions in the main mineralization stage, and the δ13CVPDB values of calcite and fluid inclusions from the altered surrounding rocks and ore minerals are generally low and significantly different from those of marine sedimentary carbonate rocks, indicating that the involvement of reductive components from carbonaceous 2002年1月12日 For example, calcite veins cutting calciumabsent pelitic rocks may indicate calcium mobility over scales at least as broad as the nearest carbonate layer; potassiumdepleted selvages around quartz veins in granite may reflect potassium transfer over distances as large as the host granite (assuming that potassium enrichment zones are absent)Mechanisms of fluid flow and fluid–rock interaction in fossil Veins Veins are dilated fractures filled with oriented crystal fibers or nonoriented mineral deposits (typically quartz, calcite or carbonates) Veins occur in rocks of all types and metamorphic grades with thickness from less than a millimeter to several metersALEX STREKEISENVeins2012年10月1日 Powdered calcite samples from 13 calcite veins and 20 wall rocks (Bons et al, 2012) (b) Basic scheme depicting growth of synand postkinematic crystals during fracture opening (after Ukar and A review of the formation of tectonic veins and their microstructures

The ubiquitous nature of accessory calcite in granitoid rocks
2005年3月1日 Request PDF The ubiquitous nature of accessory calcite in granitoid rocks: Implications for weathering, solute evolution, and petrogenesis Calcite is frequently cited as a source of excess Ca In addition, average mineralogical composition of this rock was determined using powdered XRay Diffraction analysis The orientation and thickness of calcite veins in the selected basaltic rocks (Fig 1) were also measured and discussed in the relevant sections to delineate the influence of calcite veins on mechanical behaviourInfluence of Calcite Veins on the Failure Mode and SpringerThe similarity between 87Sr/86Sr values of the calcite and those of their respective surrounding host rocks (072670−072875 of the Longmaxi shales; 072030−072648 of the Wufeng shales Fluid inclusion microthermometric data of calcite veins413 Igneous Rock Bodies Igneous rocks are common in the geologic record, but surprisingly, it is the intrusive rocks that are more common Extrusive rocks, because of their small crystals and glass, are less durable Plus, they are, by 4 Igneous Processes and Volcanoes – An

Characteristics of a LowSulfidation Epithermal
2017年7月19日 the contact between veins and their surrounding rocks (Figure 7 a) Chlorite and chlorite/smectite appear to replace biotite and hornblende, respectively (Figure 7 b)2018年10月9日 The Phapon gold deposit is located in the northern Laos and the northern segments of the Luang Prabang–Loei metallogenic belt The lodegold orebodies consist of auriferous calcite veins in the middle, and the surrounding siderite alteration and hematite alteration zones in red color This deposit is hosted in Lower Permian limestone and controlled Rare Earth Elements Geochemistry and C–O Isotope MDPI1532 TX Diagrams are (Almost) the Same as PT Diagrams 159 Example of a TX diagram with four reactions and an invariant point; this chapter contains many phase diagrams – these and other diagrams in this chapter were generated using the winTWQ program (Berman 1991) Reactions and reaction lines intersect and behave the same in TX diagrams as they do in PT 15 Metamorphism of Calcareous Rocks – Open Petrology2023年8月25日 In hydrothermal systems, where hot fluids interact with rocks, calcite can precipitate as veins and deposits Pressure: Pressure affects the solubility of minerals, including calcite In deep sedimentary basins, increased pressure can lead to the precipitation of calcite from fluids, contributing to the formation of calciterich rocksCalcite : Properties, Formation, Occurrence and Uses Areas

Rare Earth Elements Geochemistry and C–O Isotope
the Luang Prabang–Loei metallogenic belt The lodegold orebodies consist of auriferous calcite veins in the middle, and the surrounding siderite alteration and hematite alteration zones in red color This deposit is hosted in Lower Permian limestone and controlled by a NEtrending2023年8月1日 Powdered calcite samples from 13 calcite veins and 20 wall rocks were used for stable oxygen and carbon isotopes analyses In this paper, four geochemical methods were used to analyze the properties, compositions, The blocky and elongate blocky veins both incorporate wallrock fragments or whole grains from surrounding rocks Geochemistry of syntaxial calcite veins in ultradeep sandstone (a) An ~150‐mm‐thick calcite vein sandwiched by the Horton Formation (siltstone), England, (b) distortion of the calcite veins due to tectonic activities, and (c) fracturing along a soft vein (a) An ~150‐mm‐thick calcite vein sandwiched by the Horton In general, the sequence here dips gently to the E However, it also contains asymmetric folds and thrust faults, verging to the W, which appear to detach within it At this locality we found several veins of fibrous calcite (beef), as well as a few veins of bitumen, all parallel or nearly parallel to bedding (Fig 9B)Beef veins and thrust detachments in Early Cretaceous source rocks