Introduction to Metamorphic Textures and Microstructures Introduction to Metamorphic Textures and Microstructures Second Edition A.J
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Microstructure of Selected Metamorphic Rock Types – Application of Petrographic Image Analysis
Acta Geodyn. Geomater., Vol. 7, No. 4 (160), 431–443, 2010 MICROSTRUCTURE OF SELECTED METAMORPHIC ROCK TYPES – APPLICATION OF PETROGRAPHIC IMAGE ANALYSIS Šárka ŠACHLOVÁ 1,2)*, Vladimír SCHENK 2) and Zdeňka SCHENKOVÁ 2) 1) Institute of Geochemistry, Mineralogy and Mineral Resources, Faculty of Science, Charles University in Prague, Albertov 6, 128 43 Prague 2, Czech Republic 2) Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, v.v.i., V Holešovičkách 41, 182 09 Prague, Czech Republic *Corresponding author‘s e-mail: [email protected] (Received August 2010, accepted November 2010) ABSTRACT Microscopic techniques, such as polarising microscopy and scanning electron microscopy with energy dispersive spectrometer (SEM/EDS), were used in combination with petrographic image analysis with the aim of a quantitative determination of the mineral composition, rock microstructure, and degree of metamorphism of selected quartz-rich metamorphic rock types. Sampled orthogneiss rock types are mainly composed of feldspar, quartz, biotite, and amphibole. The grains are less isometric, elongated, having smooth boundaries, and showing a weak preferential orientation. The deformation and recrystallization characteristics of quartz indicate high-temperature recrystallization (the grain boundary migration recrystallization mechanism). Schist and phyllite rock types are preferentially very-fine to fine-grained, showing a strong shape preferred orientation. Their sedimentary origin was indicated by the presence of graphite. -
Igneous Garnet and Amphibole Fractionation in the Roots of Island Arcs: Experimental Constraints on Andesitic Liquids
CORE Metadata, citation and similar papers at core.ac.uk Provided by Serveur académique lausannois Contrib Mineral Petrol (2009) 157:541–558 DOI 10.1007/s00410-008-0351-8 ORIGINAL PAPER Igneous garnet and amphibole fractionation in the roots of island arcs: experimental constraints on andesitic liquids Raquel Alonso-Perez Æ Othmar Mu¨ntener Æ Peter Ulmer Received: 23 January 2008 / Accepted: 6 October 2008 / Published online: 30 October 2008 Ó Springer-Verlag 2008 Abstract To evaluate the role of garnet and amphibole for ‘slab melting’, or dehydration melting in the deep arc. fractionation at conditions relevant for the crystallization of Garnet fractionation, either in the deep crust via formation magmas in the roots of island arcs, a series of experiments of garnet gabbros, or in the upper mantle via formation of were performed on a synthetic andesite at conditions garnet pyroxenites remains an important alternative, ranging from 0.8 to 1.2 GPa, 800–1,000°C and variable despite the rare occurrence of magmatic garnet in volcanic H2O contents. At water undersaturated conditions and fO2 rocks. established around QFM, garnet has a wide stability field. At 1.2 GPa garnet ? amphibole are the high-temperature Keywords Experimental petrology Á Hydrous andesite liquidus phases followed by plagioclase at lower tempera- liquids Á High-pressure crystallization Á Amphibole Á ture. Clinopyroxene reaches its maximal stability at H2O- Garnet fractionation contents B9 wt% at 950°C and is replaced by amphibole at lower temperature. The slopes of the plagioclase-in boundaries are moderately negative in T-XH2O space. At Introduction 0.8 GPa, garnet is stable at magmatic H2O contents exceeding 8 wt% and is replaced by spinel at decreasing Major and trace element similarities between estimates of dissolved H2O. -
II Eshelby Tensor of Concave Superspherical Inclusions
AVERTISSEMENT Ce document est le fruit d'un long travail approuvé par le jury de soutenance et mis à disposition de l'ensemble de la communauté universitaire élargie. Il est soumis à la propriété intellectuelle de l'auteur. Ceci implique une obligation de citation et de référencement lors de l’utilisation de ce document. D'autre part, toute contrefaçon, plagiat, reproduction illicite encourt une poursuite pénale. Contact : [email protected] LIENS Code de la Propriété Intellectuelle. articles L 122. 4 Code de la Propriété Intellectuelle. articles L 335.2- L 335.10 http://www.cfcopies.com/V2/leg/leg_droi.php http://www.culture.gouv.fr/culture/infos-pratiques/droits/protection.htm Thèse de DOCTORAT Préparée à L’Université de Lorraine - Laboratoire Georessources –UMR7359 Présentée par Fengjuan CHEN Pour obtenir le grade de Docteur en SCIENCES DE L’UNIVERSITE DE LORRAINE Spécialité Mécanique - Génie Civil Modélisation Micromécanique de Milieux Poreux Hétérogènes et Applications aux Roches Oolithiques Ph-D Thesis Micromechanical Modelling of Heterogeneous Porous Materials with Application to Oolitic Rocks Soutenance publiquement le 24 Octobre 2016 Jury composé de M.KACHANOV Professeur Tufts University, USA Rapporteur V.KUSHCH Professeur Ukraine National Academy of Science, UA Rapporteur Y.GUEGUEN Professeur Ecole Nationale Supérieure, Paris, France Examinateur I.SEVOSTIANOV Professeur New Mexico State University, USA Examinateur A.GIRAUD Professeur ENSG, Nancy, France Directeur D.GRGIC Maître de conférences ENSG, Nancy, France Co-directeur II For my father, for my mother, "It's not that I'm so smart, it's just that I stay with problems longer " Albert Einstein III IV Acknowledgement Considering the challenge, I would not accomplish my Ph.D. -
Reworked Restite Enclave
Reworked restite enclave: Petrographic and mineralogical constraints from the Tongshanling intrusion, Nanling Range, South China Xu-Dong Huang, Jian-Jun Lu, Stanislas Sizaret, Ru-Cheng Wang, Jin-Wei Wu, Dong-Sheng Ma To cite this version: Xu-Dong Huang, Jian-Jun Lu, Stanislas Sizaret, Ru-Cheng Wang, Jin-Wei Wu, et al.. Re- worked restite enclave: Petrographic and mineralogical constraints from the Tongshanling intru- sion, Nanling Range, South China. Journal of Asian Earth Sciences, Elsevier, 2018, 166, pp.1-18. 10.1016/j.jseaes.2018.07.001. insu-01856863 HAL Id: insu-01856863 https://hal-insu.archives-ouvertes.fr/insu-01856863 Submitted on 10 Dec 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Reworked restite enclave: Petrographic and mineralogical constraints from the Tongshanling intrusion, Nanling Range, South China Xu-DongHuangab Jian-JunLua StanislasSizaretb Ru-ChengWanga Jin-WeiWua Dong-ShengMaa A : State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China B : Institut des Sciences de la Terre d’Orléans, UMR 7327-CNRS/Université d’Orléans/BRGM, Orléans 45071, France Abstract Microgranular enclaves, which can provide important petrogenetic indications for the host granitoids, are commonly observed in the Middle-Late Jurassic Cu-Pb-Zn-bearing granodiorites in the Nanling Range of South China. -
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Open Geosci. 2015; 7:53–64 Research Article Open Access László Molnár*, Balázs Vásárhelyi, Tivadar M. Tóth, and Félix Schubert Integrated petrographic – rock mechanic borecore study from the metamorphic basement of the Pannonian Basin, Hungary Abstract: The integrated evaluation of borecores from the 1 Introduction Mezősas-Furta fractured metamorphic hydrocarbon reser- voir suggests significantly distinct microstructural and Brittle fault zones of crystalline rock masses can serve as rock mechanical features within the analysed fault rock migration pathways or also as sealing surfaces for fluid samples. The statistical evaluation of the clast geometries flow in the Earth’s crust, so the understanding of their in- revealed the dominantly cataclastic nature of the sam- ternal structure is crucial for interpreting hydraulic sys- ples. Damage zone of the fault can be characterised by tems. Earlier studies [1, 2] on the architecture of fault an extremely brittle nature and low uniaxial compressive zones defined two main structural elements: first, a weakly strength, coupled with a predominately coarse fault brec- disaggregated, densely fractured “damage zone” and a cia composition. In contrast, the microstructural manner strongly deformed and fragmented “fault core”, where of the increasing deformation coupled with higher uni- the pre-existing rock fabrics were erased by fault devel- axial compressive strength, strain-hardening nature and opment. These elements can be characterised by the for- low brittleness indicate a transitional interval between mation of diverse tectonite types (fault breccias, catacla- the weakly fragmented damage zone and strongly grinded sites, fault gouges), which often also possess quite hetero- fault core. Moreover, these attributes suggest this unit is geneous rheological features. -
Petrogenesis of Slab-Derived Trondhjemite-Tonalite-Dacite/ Adakite Magmas M
Transactions of the Royal Society of Edinburgh: Earth Sciences, 87, 205-215, 1996 Petrogenesis of slab-derived trondhjemite-tonalite-dacite/ adakite magmas M. S. Drummond, M. J. Defant and P. K. Kepezhinskas ABSTRACT: The prospect of partial melting of the subducted oceanic crust to produce arc magmatism has been debated for over 30 years. Debate has centred on the physical conditions of slab melting and the lack of a definitive, unambiguous geochemical signature and petrogenetic process. Experimental partial melting data for basalt over a wide range of pressures (1-32 kbar) and temperatures (700-1150=C) have shown that melt compositions are primarily trondhjemite- tonalite-dacite (TTD). High-Al (> 15% A12O3 at the 70% SiO2 level) TTD melts are produced by high-pressure 015 kbar) partial melting of basalt, leaving a restite assemblage of garnet + clinopyroxe'ne ± hornblende. A specific Cenozoic high-Al TTD (adakite) contains lower Y, Yb and Sc and higher Sr, Sr/Y, La'/Yb and.Zr/Sm relative to other TTD types and is interpreted to represent a slab melt under garnet amphibolite to eclogite conditions. High-Al TTD with an adakite-like geochemical character is prevalent in the Archean as the result of a higher geotherm that facilitated slab melting. Cenozoic adakite localities are commonly associated with the subduction of young (<25Ma), hot oceanic crust, which may provide a slab geotherm (*9-10=C km"1) conducive for slab dehydration melting. Viable alternative or supporting tectonic effects that may enhance slab melting include highly oblique convergence and resultant high shear stresses and incipient subduction into a pristine hot mantle wedge. -
Metamorphic Rocks.Pdf
Metamorphism & Metamorphic Rocks (((adapted from Brunkel, 2012) Metamorphic Rocks . Changed rocks- with heat and pressure . But not melted . Change in the solid state . Textural changes (always) . Mineralogy changes (usually) Metamorphism . The mineral changes that transform a parent rock to into a new metamorphic rock by exposure to heat, stress, and fluids unlike those in which the parent rock formed. granite gneiss Geothermal gradient Types of Metamorphism . Contact metamorphism – – Happens in wall rock next to intrusions – HEAT is main metamorphic agent . Contact metamorphism Contact Metamorphism . Local- Usually a zone only a few meters wide . Heat from plutons intruded into “cooler” country rock . Usually forms nonfoliated rocks Types of Metamorphism . Hydrothermal metamorphism – – Happens along fracture conduits – HOT FLUIDS are main metamorphic agent Types of Metamorphism . Regional metamorphism – – Happens during mountain building – Most significant type – STRESS associated with plate convergence & – HEAT associated with burial (geothermal gradient) are main metamorphic agents . Contact metamorphism . Hydrothermal metamorphism . Regional metamorphism . Wide range of pressure and temperature conditions across a large area regional hot springs hydrothermal contact . Regional metamorphism Other types of Metamorphism . Burial . Fault zones . Impact metamorphism Tektites Metamorphism and Plate Tectonics . Fault zone metamorphism . Mélange- chaotic mixture of materials that have been crumpled together Stress (pressure) . From burial -
Finding of Prehnite-Pumpellyite Facies Metabasites from the Kurosegawa Belt in Yatsushiro Area, Kyushu, Japan
Journal ofPrehnite Mineralogical-pumpellyite and Petrological facies metabasites Sciences, in Yatsushiro Volume 107, area, page Kyushu 99─ 104, 2012 99 LETTER Finding of prehnite-pumpellyite facies metabasites from the Kurosegawa belt in Yatsushiro area, Kyushu, Japan * * ** Kenichiro KAMIMURA , Takao HIRAJIMA and Yoshiyuki FUJIMOTO *Department of Geology and Mineralogy, Graduate School of Science, Kyoto University, Kitashirakawa Oiwakecho, Kyoto 606-8502, Japan ** Nittetsu-Kogyo Co., Ltd, 2-3-2 Marunouchi, Chiyoda, Tokyo 100-8377, Japan. Common occurrence of prehnite and pumpellyite is newly identified from metabasites of Tobiishi sub-unit in the Kurosegawa belt, Yatsushiro area, Kyushu, where Ueta (1961) had mapped as a greenschist facies area. Prehnite and pumpellyite are closely associated with chlorite, calcite and quartz, and they mainly occur in white colored veins or in amygdules in metabasites of the relevant area, but actinolite and epidote are rare in them. Pumpellyite is characterized by iron-rich composition (7.2-20.0 wt% as total iron as FeO) and its range almost overlaps with those in prehnite-pumpellyite facies metabasites of Ishizuka (1991). These facts suggest that the metabasites of the Tobiishi sub-unit suffered the prehnite-pumpellyite facies metamorphism, instead of the greenschist facies. Keywords: Prehnite-pumpellyite facies, Lawsonite-blueschist facies, Kurosegawa belt INTRODUCTION 1961; Kato et al., 1984; Maruyama et al., 1984; Tsujimori and Itaya, 1999; Tomiyoshi and Takasu, 2009). Until now, The subduction zone has an essential role for the global there is neither clear geological nor petrological evidence circulation of solid, fluid and volatile materials between suggesting what type of metamorphic rocks occupied the the surface and inside of the Earth at present. -
The Initiation and Development of Metamorphic Foliation in the Otago Schist, Part 2: Evidence from Quartz Grain-Shape Data
The initiation and development of metamorphic foliation in the Otago Schist, Part 2: Evidence from quartz grain-shape data AARON STALLARD,1 DAVID SHELLEY1 AND STEVE REDDY2 1Department of Geological Sciences, University of Canterbury, Private Bag 4800, Christchurch, New Zealand ([email protected]) 2Tectonics Special Research Centre, Dept. of Applied Geology, Curtin University of Technology, Perth, WA 6845, Australia ABSTRACT Shape, size and orientation measurements of quartz grains sampled along two transects that cross zones of increasing metamorphic grade in the Otago Schist, New Zealand, reveal the role of quartz in the progressive development of metamorphic foliation. Sedimentary compaction and diagenesis contributed little to forming a shape preferred orientation (SPO) within the analysed samples. Metamorphic foliation was initiated at sub-greenschist facies conditions as part of a composite S1- bedding structure parallel to the axial planes of tight to isoclinal F1 folds. An important component of this foliation is a pronounced quartz SPO that formed dominantly by the effect of dissolution- precipitation creep on detrital grains in association with F1 strain. With increasing grade, the following trends are evident from the SPO data: (i) a progressive increase in the aspect ratio of grains in sections parallel to lineation, and the development of blade-shaped grains; (ii) the early development of a strong shape preferred orientation so that blade lengths define the linear aspect of the foliation (lineation) and the intermediate axes of the blades define a partial girdle about the lineation; (iii) a slight thinning and reduction in volume of grains in the one transect; (iv) an actual increase in thickness and volume in the survivor grains of the second transect. -
Metamorphic Fabrics
11/30/2015 Geol341 J. Toro Topics • Fabrics • Foliation, cleavage, lineation Metamorphic Rocks and – Cleavage and Folds –Geometry Cleavage Development – Strain significance • Origin of Cleavage – Pressure solution – Passive rotation – Recrystallization • Shear zones Many diagrams are from Earth Structure, van der Pluijm and Marshak, 2004 2013 Geothermal Gradient and Metamorphism Naming of Metamorphic Rocks Slatey cleavage Gneiss Segregation of mafic and felsic components Where does it come from? 1 11/30/2015 Looks like bedding, but is it? Metamorphic layering Brooks Range, AK Quartz-mica schist Isoclinal Fold Transposition of Layering Fabric “Arrangement of component features in a rock” van der Pluijm & Marshak •Includes: •Texture •Composition •Microstructure •Preferred Orientation Horizontal fabric => Vertical fabric 2 11/30/2015 Quartz-mica schist Fabric Elements •Bedding (S0) •Compositional layering •Crystallographic orientation •Fold Hinges •Cleavage planes (S1) •Mineral elongation lineation Passchier and Trouw (1996) Metamorphic Fabrics Metamorphic Fabrics • Foliation : Cleavage, Schistosity • Foliation • Lineation: Mineral Lineation, Intersection Lineation – Cleavage – Schistosity • Lineation Random fabric S-tectonite L-tectonite L/S-tectonite Foliation Lineation S-Tectonites L-Tectonites Schists Columbia Pluton, VA Lineated Gneiss USGS photo U. Western Ontario photo 3 11/30/2015 L-S Tectonites 3D Strain - Flinn diagram No strain along 3rd dimension Cigars S =S >S S1/S2 1 2 3 S1>S2=S3 Lineated and foliated gneiss, Himalayas Prolate -
Fabric Foliation
2/14/15 Fabric • The characteristics of the geometry and spacing of the elements that make up a rock. – Linear – Planar – Random Foliation • Any fabric-forming planar or curvi-planar structure. • May be primary or tectonic • Many rocks have more than one foliation • Approximate as planes and/or surfaces 1 2/14/15 Cleavage • Describes the tendency of a rock to split along foliation planes • Not the same as cleavage of a single crystal/mineral ! Where well-developed, synonym for foliation. Lineation • Linear elements in a rock • One axis >> other two • Penetrative, surface or geometric Image from your friend Wikipedia 2 2/14/15 Keep thinking about strain ellipse • Foliations form perpendicular to shortening (e3 axis is pole to foliation plane) • Lineations – Elongation – mineral stretching = e1 – Shear lineations – oblique to strain ellipse axes, gives asymmetry/rotation 3 2/14/15 Tectonites • Fabrics in deformed metamorphic rocks are referred to as tectonites L-tectonite 4 2/14/15 S-tectonite Gneissic banding • Gneiss – Early layering is folded – Flattened limbs are parallel • Transposed foliation 5 2/14/15 Mylonites • Contain a “mylonitic foliation” formed by crystal plastic deformation in a shear zone (pure or simple) • Transposed layering • Shear zone fault rocks Describing cleavage 6 2/14/15 Metamorphosis of a pelite • Slaty cleavage – Preferential dissolution of some minerals – Perpendicular to shortening • Minerals line up • Becomes more continuous as it 1mm develops Crenulation = 2nd foliation folds first 7 2/14/15 Crenulation Cleavage -
Persson Mines 0052N 11296.Pdf
THE GEOCHEMICAL AND MINERALOGICAL EVOLUTION OF THE MOUNT ROSA COMPLEX, EL PASO COUNTY, COLORADO, USA by Philip Persson A thesis submitted to the Faculty and Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date ________________ Signed: ________________________ Philip Persson Signed: ________________________ Dr. Katharina Pfaff Thesis Advisor Golden, Colorado Date ________________ Signed: ________________________ Dr. M. Stephen Enders Professor and Interim Head Department of Geology and Geological Engineering ii ABSTRACT The ~1.08 Ga Pikes Peak Batholith is a type example of an anorogenic (A)-type granite and hosts numerous late-stage sodic and potassic plutons, including the peraluminous to peralkaline Mount Rosa Complex (MRC), located ~15 km west of the City of Colorado Springs in Central Colorado. The MRC is composed of Pikes Peak biotite granite, fayalite-bearing quartz syenite, granitic dikes, Mount Rosa Na-Fe amphibole granite, mafic dikes ranging from diabase to diorite, and numerous rare earth (REE) and other high field strength element (HFSE; e.g. Th, Zr, Nb) rich Niobium-Yttrrium-Fluorine (NYF)-type pegmatites. The aim of this study is to trace the magmatic evolution of the Mount Rosa Complex in order to understand the relationship between peraluminous and peralkaline rock units and concomitant HFSE enrichment and mineralization processes. Field work, petrography, SEM-based methods, whole rock geochemistry, and electron probe micro-analysis (EPMA) of micas was performed on all rock units to determine their textural, mineralogical and geochemical characteristics. Early peraluminous units such as the Pikes Peak biotite granite and fayalite-bearing quartz syenite contain annite-siderophyllite micas with high Fe/(Fe + Mg) ratios, and show relatively minor enrichments in REE and other HFSE compared to primitive mantle.