The Effect of Cation Order on the Elasticity of Omphacite from Atomistic Calculations
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Orthopyroxene–Omphacite
Lithos 216–217 (2015) 1–16 Contents lists available at ScienceDirect Lithos journal homepage: www.elsevier.com/locate/lithos Orthopyroxene–omphacite- and garnet–omphacite-bearing magmatic assemblages, Breaksea Orthogneiss, New Zealand: Oxidation state controlled by high-P oxide fractionation☆ Timothy Chapman a,⁎, Geoffrey L. Clarke a, Nathan R. Daczko b,c, Sandra Piazolo b,c, Adrianna Rajkumar a a School of Geosciences, F09, University of Sydney, Sydney, NSW 2006, Australia b ARC Centre of Excellence for Core to Crust Fluid Systems, Department of Earth and Planetary Sciences, Macquarie University, NSW 2109, Australia c GEMOC, Department of Earth and Planetary Sciences, Macquarie University, NSW 2109, Australia article info abstract Article history: The Breaksea Orthogneiss comprises a monzodioritic host partially recrystallised to omphacite–garnet–plagioclase– Received 19 December 2013 rutile granulite at 850 °C and 1.8 GPa, with metre to decametre-scale, cognate inclusions ranging from ultramafic Accepted 21 November 2014 through gabbroic to monzodioritic composition. Coarsely layered garnetite and diopsidic clinopyroxenite cumulate Available online 3 December 2014 preserves igneous textures, whereas garnet–omphacite cumulate shows a partial metamorphic overprint to eclogite. Garnet and omphacite in undeformed to weakly deformed rocks have similar major and rare earth element Keywords: characteristics reflecting their common igneous origin, pointing to a lack of metamorphic recrystallisation. Inclusions Omphacite–garnet granulite – – – Orthopyroxene eclogite of omphacite orthopyroxene plagioclase ulvöspinel orthogneiss have whole-rock compositions almost identical Omphacite–orthopyroxene granulite to the host monzodiorite. Reaction zones developed along contacts between the orthopyroxene-bearing inclusions REE and host contain metamorphic garnet that is microstructurally and chemically distinct from igneous garnet. -
High-Pressure Single-Crystal Elasticity and Thermal Equation Of
Journal of Geophysical Research: Solid Earth 10.1029/2018JB016964 2001). For example, D. Zhang et al. (2016) performed single‐crystal X‐ray diffraction (XRD) experiments on omphacite up to 47 GPa at 300 K. Pandolfo et al. (2012b) measured the thermal expansion coefficients of omphacite up to 1073 K at 1 atm. The only available in situ high P‐T EOS study for omphacite is performed on polycrystalline samples using multianvil press up to 10 GPa and thus is unable to cover the entire P stability field of omphacite in the Earth's interior (Nishihara et al., 2003). On the other hand, although the sound velocities of the Mg,Ca end member diopside have been studied at various P‐T conditions (Isaak et al., 2006; Isaak & Ohno, 2003; Levien et al., 1979; Li & Neuville, 2010; Matsui & Busing, 1984; Sang et al., 2011; Sang & Bass, 2014; Walker, 2012), the single‐crystal elastic properties of omphacite have only been measured at ambient condition (Bhagat et al., 1992) or investigated computationally at high‐P 0‐K conditions (Skelton & Walker, 2015). The lack of experimentally determined thermoelastic properties of omphacite, which is the most abundant mineral phase in eclogite, restricts our understanding of the subduction process as well as the possible seismic identification of eclogitic materials in the Earth's interior. To fill in this knowledge gap, we performed high P‐T single‐crystal XRD measurements on natural P2/n omphacite crystals up to 18 GPa 700 K at GeoSoilEnviroCARS (GSECARS), Advanced Photon Source, Argonne National Laboratory, as well as single‐crystal Brillouin spectroscopy measurements of the same crystals up to 18 GPa at 300 K at the high‐P laser spectroscopy laboratory at University of New Mexico (UNM). -
Ultra-High Pressure Aluminous Titanites in Carbonate-Bearing Eclogites at Shuanghe in Dabieshan, Central China
Ultra-high pressure aluminous titanites in carbonate-bearing eclogites at Shuanghe in Dabieshan, central China D. A. CARSWELL Department of Earth Sciences, University of Sheffield, Sheffield $3 7HF, UK R. N. WILSON Department of Geology, University of Leicester, Leicester LE1 7RH, UK AND M. ZtIAI Institute of Geology, Academia Sinica, P.O. Box 634, Beijing 100029, China Abstract Petrographic features and compositions of titanites in eclogites within the ultra-high pressure metamorphic terrane in central Dabieshan are documented and phase equilibria and thermobarometric implications discussed. Carbonate-bearing eclogite pods in marble at Shuanghe contain primary metamorphic aluminous titanites, with up to 39 mol.% Ca(AI,Fe3+)FSiO4 component. These titanites formed as part of a coesite- bearing eclogite assemblage and thus provide the first direct petrographic evidence that AIFTi_IO_j substitution extends the stability of titanite, relative to futile plus carbonate, to pressures within the coesite stability field. However, it is emphasised that A1 and F contents of such titanites do not provide a simple thermobarometric index of P-T conditions but are constrained by the activity of fluorine, relative to CO2, in metamorphic fluids - as signalled by observations of zoning features in these titanites. These ultra-high pressure titanites show unusual breakdown features developed under more H20-rich amphibolite-facies conditions during exhumation of these rocks. In some samples aluminous titanites have been replaced by ilmenite plus amphibole symplectites, in others by symplectitic intergrowths of secondary, lower AI and F, titanite plus plagioclase. Most other coesite-bearing eclogite samples in the central Dabieshan terrane contain peak assemblage rutile often partly replaced by grain clusters of secondary titanites with customary low AI and F contents. -
Cold Subduction and the Formation of Lawsonite Eclogite – Constraints from Prograde Evolution of Eclogitized Pillow Lava from Corsica
J. metamorphic Geol., 2010, 28, 381–395 doi:10.1111/j.1525-1314.2010.00870.x Cold subduction and the formation of lawsonite eclogite – constraints from prograde evolution of eclogitized pillow lava from Corsica E. J. K. RAVNA,1 T. B. ANDERSEN,2 L. JOLIVET3 AND C. DE CAPITANI4 1Department of Geology, University of Tromsø, N-9037 Tromsø, Norway ([email protected]) 2Department of Geosciences and PGP, University of Oslo, PO Box 1047, Blindern, 0316 Oslo, Norway 3ISTO, UMR 6113, Universite´ dÕOrle´ans, 1A Rue de la Fe´rollerie, 45071 Orle´ans, Cedex 2, France 4Mineralogisch-Petrographisches Institut, Universita¨t Basel, Bernoullistrasse 30, 4056 Basel, Switzerland ABSTRACT A new discovery of lawsonite eclogite is presented from the Lancoˆne glaucophanites within the Schistes Lustre´ s nappe at De´ file´ du Lancoˆne in Alpine Corsica. The fine-grained eclogitized pillow lava and inter- pillow matrix are extremely fresh, showing very little evidence of retrograde alteration. Peak assemblages in both the massive pillows and weakly foliated inter-pillow matrix consist of zoned idiomorphic Mg-poor (<0.8 wt% MgO) garnet + omphacite + lawsonite + chlorite + titanite. A local overprint by the lower grade assemblage glaucophane + albite with partial resorption of omphacite and garnet is locally observed. Garnet porphyroblasts in the massive pillows are Mn rich, and show a regular prograde growth-type zoning with a Mn-rich core. In the inter-pillow matrix garnet is less manganiferous, and shows a mutual variation in Ca and Fe with Fe enrichment toward the rim. Some garnet from this rock type shows complex zoning patterns indicating a coalescence of several smaller crystallites. -
A Comparative Study of Jadeite, Omphacite and Kosmochlor Jades from Myanmar, and Suggestions for a Practical Nomenclature
Feature Article A Comparative Study of Jadeite, Omphacite and Kosmochlor Jades from Myanmar, and Suggestions for a Practical Nomenclature Leander Franz, Tay Thye Sun, Henry A. Hänni, Christian de Capitani, Theerapongs Thanasuthipitak and Wilawan Atichat Jadeitite boulders from north-central Myanmar show a wide variability in texture and mineral content. This study gives an overview of the petrography of these rocks, and classiies them into ive different types: (1) jadeitites with kosmochlor and clinoamphibole, (2) jadeitites with clinoamphibole, (3) albite-bearing jadeitites, (4) almost pure jadeitites and (5) omphacitites. Their textures indicate that some of the assemblages formed syn-tectonically while those samples with decussate textures show no indication of a tectonic overprint. Backscattered electron images and electron microprobe analyses highlight the variable mineral chemistry of the samples. Their extensive chemical and textural inhomogeneity renders a classiication by common gemmological methods rather dificult. Although a deinitive classiication of such rocks is only possible using thin-section analysis, we demonstrate that a fast and non-destructive identiication as jadeite jade, kosmochlor jade or omphacite jade is possible using Raman and infrared spectroscopy, which gave results that were in accord with the microprobe analyses. Furthermore, current classiication schemes for jadeitites are reviewed. The Journal of Gemmology, 34(3), 2014, pp. 210–229, http://dx.doi.org/10.15506/JoG.2014.34.3.210 © 2014 The Gemmological Association of Great Britain Introduction simple. Jadeite jade is usually a green massive The word jade is derived from the Spanish phrase rock consisting of jadeite (NaAlSi2O6; see Ou Yang, for piedra de ijada (Foshag, 1957) or ‘loin stone’ 1999; Ou Yang and Li, 1999; Ou Yang and Qi, from its reputed use in curing ailments of the loins 2001). -
Eclogite Resembling Metamorphic Disequilibrium Assemblage Formed Through Fuid‑Induced Metasomatic Reactions Sanghoon Kwon1, Vinod O
www.nature.com/scientificreports OPEN Eclogite resembling metamorphic disequilibrium assemblage formed through fuid‑induced metasomatic reactions Sanghoon Kwon1, Vinod O. Samuel1*, Yungoo Song1, Sung Won Kim2, Seung‑Ik Park3, Yirang Jang4 & M. Santosh5,6 Equilibrium omphacite‑garnet‑bearing mafc rocks have been classifed as eclogites, either pristine or retrogressed, that were formed at great depths in the lithosphere. Here we report a unique natural example of eclogite resembling assemblage in disequilibrium formed through fuid‑induced metasomatic reactions under the amphibolite to granulite facies. Primarily, the amphibolized protolith experienced a garnet‑amphibolite facies metamorphism at ~ 500–700 °C and ~ 0.8–1 GPa. Subsequently, CO2 fuid induced fracturing and dissolution‑reprecipitation reactions occurred at peak metamorphic conditions of ~ 700 °C and ~ 1 GPa. Occasional omphacite‑albite assemblage, which gradually replace diopside‑oligoclase symplectite adjacent to albite veins along fractures, indicates fuid‑induced coupled dissolution‑reprecipitation disequilibrium reactions. Here the albite‑omphacite assemblage is in local equilibrium at least on 1 mm length scale, during cooling, below ~ 600 ºC and ~ 1 GPa, within the amphibolite facies conditions. The results from this study clearly suggest that disequilibrium garnet‑omphacite assemblage in mafc rocks could be formed by crustal reworking processes below granulite facies conditions, and their textural equilibrium is an important criterion while defning eclogite facies. Eclogite facies metamorphic rocks formed through subduction and collision processes are common in global orogenic belts1–12 (e.g., Usagaran belt 1, Belomorian Belt2, Trans-Hudson orogen3, Grenvillian-Caledonian belt 4,5 Qinling–Dabie–Sulu belt6, Appalachian Orogenic Belt 7, Central Asian Orogenic Belt 8, Sambagawa belt 9, Alpine- Himalayan belt10,11, Franciscan complex12 etc.) created throughout Earth’s history. -
List of Abbreviations
List of Abbreviations Ab albite Cbz chabazite Fa fayalite Acm acmite Cc chalcocite Fac ferroactinolite Act actinolite Ccl chrysocolla Fcp ferrocarpholite Adr andradite Ccn cancrinite Fed ferroedenite Agt aegirine-augite Ccp chalcopyrite Flt fluorite Ak akermanite Cel celadonite Fo forsterite Alm almandine Cen clinoenstatite Fpa ferropargasite Aln allanite Cfs clinoferrosilite Fs ferrosilite ( ortho) Als aluminosilicate Chl chlorite Fst fassite Am amphibole Chn chondrodite Fts ferrotscher- An anorthite Chr chromite makite And andalusite Chu clinohumite Gbs gibbsite Anh anhydrite Cld chloritoid Ged gedrite Ank ankerite Cls celestite Gh gehlenite Anl analcite Cp carpholite Gln glaucophane Ann annite Cpx Ca clinopyroxene Glt glauconite Ant anatase Crd cordierite Gn galena Ap apatite ern carnegieite Gp gypsum Apo apophyllite Crn corundum Gr graphite Apy arsenopyrite Crs cristroballite Grs grossular Arf arfvedsonite Cs coesite Grt garnet Arg aragonite Cst cassiterite Gru grunerite Atg antigorite Ctl chrysotile Gt goethite Ath anthophyllite Cum cummingtonite Hbl hornblende Aug augite Cv covellite He hercynite Ax axinite Czo clinozoisite Hd hedenbergite Bhm boehmite Dg diginite Hem hematite Bn bornite Di diopside Hl halite Brc brucite Dia diamond Hs hastingsite Brk brookite Dol dolomite Hu humite Brl beryl Drv dravite Hul heulandite Brt barite Dsp diaspore Hyn haiiyne Bst bustamite Eck eckermannite Ill illite Bt biotite Ed edenite Ilm ilmenite Cal calcite Elb elbaite Jd jadeite Cam Ca clinoamphi- En enstatite ( ortho) Jh johannsenite bole Ep epidote -
Phase Composition and Genesis of Pyroxenic Jadeite from Guatemala: Insights from Cite This: RSC Adv., 2020, 10,15937 Cathodoluminescence
RSC Advances View Article Online PAPER View Journal | View Issue Phase composition and genesis of pyroxenic jadeite from Guatemala: insights from Cite this: RSC Adv., 2020, 10,15937 cathodoluminescence Chenlu Lin, a Xuemei He, *a Zhiyun Lu b and Yuwei Yaoa Guatemalan jadeite has a long history, and much Guatemalan jadeite can be found on the market today with a variety of colors and species diversity. Seven varieties of green pyroxenic jadeite from Guatemala with greyish green, yellow green, brilliant green, blue green, dark green, black green and mottled green colors were investigated by combining the methods of XRD, Raman spectroscopy, cathodoluminescence, EPMA and m-XRF mapping. The results showed that according to the composition, Guatemalan pyroxenic jadeite can be divided into three categories: jadeite jade, omphacite jade, and jadeite– omphacite jade. According to the characteristics of cathodoluminescence, it can be speculated that the formation of jadeite undergoes three stages, and the formation of jadeite jade is mainly due to the Creative Commons Attribution-NonCommercial 3.0 Unported Licence. crystallization (Jad I) of the early jadeite fluid, along with the second-stage fluid metasomatism/ Received 24th February 2020 crystallization (Jad II). In the later stage, the fluid that is rich in Ca–Mg–Fe components can replace early Accepted 1st April 2020 Jad I/Jad II, or it can coexist with Jad II, and metamorphism occurs to produce omphacite jade. The DOI: 10.1039/d0ra01772h jadeite–omphacite jade can be formed when the omphacite fluid with incomplete metasomatism, with rsc.li/rsc-advances uneven texture and reduced transparency. 1. Introduction relatively pure, mainly being of space group C2/c.8,9 The C2/c space group has the general formula, M2M1{T2O6}. -
LMHC Information Sheet # 11 Jade and Related Minerals
LMHC Standardised Gemmological Report Wording (version 4; December 2011) LMHC Information Sheet # 11 Jade and related minerals - Definitions - Report wording Members of the Laboratory Manual Harmonisation Committee (LMHC) have standardised the nomenclature that they use to describe nephrite jade, jadeite jade, omphacite, kosmochlor. Definitions Jade is a trade name that encompasses jadeite and nephrite only. Nephrite is a solid solution of the amphibole group minerals actinolite and tremolite composed of an interlocking mass of fibrous crystals. Its colour commonly ranges from white to deep green, but can also be brown or black. The ideal chemical formula is Ca2(Mg,Fe)5Si8O22(OH)2. Jadeite is a pyroxene mineral and forms solid solutions with other pyroxene members such as augite and diopside, aegirine, omphacite and kosmochlor. Gem quality called as ‘jadeite jade’ is not a single crystal but a rock consisting of aggregated fibrous or granular crystals of jadeite and considerable amount of various minerals. Its colour commonly ranges from white through pale green to deep green but can also be blue-green, dark green to black, and other rare colours of pink, lavender varieties. Mineralogically jadeite has the ideal chemical formula NaAlSi2O6. Omphacite is a member of the pyroxene group with a chemical formula of (Na, Ca) (Al, Mg, Fe) Si2O6. Gem quality omphacite displays pale green, deep green, black or nearly colourless varieties. Kosmochlor is a green chromium and sodium rich pyroxene with the chemical formula NaCrSi2O6. Pyroxenes have -
CHAPTER 4 - MINERAL CHEMISTRY and METAMORPHIC CONDITIONS A
- 217 - CHAPTER 4 - MINERAL CHEMISTRY AND METAMORPHIC CONDITIONS a - 218 - Mineral chemistry and metamorphic conditions The aims of this chapter are to present mineral chemical data, to describe the mineral chemistry in relation to parageneses in selected lithologies (with particular reference to high-pressure metamorphic types) and to evaluate the metamorphic conditions under which these parageneses formed in the light of published experimentally and theoretically derived phase equilibria. Finally, a synthesis of pressure-temperature-time (P-T-t) relationships will be presented. Analytical methods and mineral recalculation schemes are described in Appendices 1 and 2. Results of geothermometry calculations are sumarised in Tbj 4.20. SECTION 4.01 The Eclogites 4.01.1 Summary of petrography Detailed petrographic descriptions appear in Chapter 2, the salient features of which are summarised here. The most common parageneses in the eclogites are:- garnet + omphacite +1- amphibole +1- rutile garnet + omphacite + phengite +1- quartz +1- rutile garnet + omphacite + phengite + zoisite +/_ quartz +/_ rut i e. S - 219 - garnet + omphacite + phengite + zoisite + kyanite +1- quartz ^1- rutile Segregations of zoisite + kyanite + quartz occur in some more aluminous types. Occasionally, Na-poor rocks have pale green or blue-green amphibole in textural equilibrium with omphacite and garnet (figure 2.18) which may become an essential or dominant phase, to give:- garnet + amphibole + clinopyroxene +/_ rutile. The phases listed above will be referred to as 'matrix' phases. Solid inclusions are common in the matrix phases (figures 2.19, 2.45). They are not associated with fractures in the garnets and commonly occur in samples where no alteration of garnet rims or matrix grains has occurred. -
Omphacite (Ca; Na)(Mg; Fe; Al)Si2o6 C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Monoclinic
Omphacite (Ca; Na)(Mg; Fe; Al)Si2O6 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: Rarely in rough crystals, to 5 cm; anhedral, granular to massive. Twinning: Single and polysynthetic twinning on 100 , common. f g Physical Properties: Cleavage: Good on 110 , (110) (110) 87±; parting on 100 . Fracture: Uneven to conchoidal. Tenacity: Brfittleg. Hardn^ess = 5{»6 D(meas.) = 3f.16{3g.43 D(calc.) = [3.36] Optical Properties: Translucent. Color: Green to dark green; colorless to pale green in thin section. Luster: Vitreous to silky. Optical Class: Biaxial (+). Pleochroism: Weak; X = colorless; Y = very pale green; Z = very pale green, blue-green. Orientation: Y = b; Z c = 36 {48 . Dispersion: r > v; moderate. ^ ± ± ® = 1.662{1.701 ¯ = 1.670{1.712 ° = 1.685{1.723 2V(meas.) = 56±{84± Cell Data: Space Group: C 2=c or P 2=n: a = 9.45{9.68 b = 8.57{8.90 c = 5.23{5.28 ¯ = 105 108 Z = 4 ± ¡ ± X-ray Powder Pattern: Hareidland, Sunm¿re, Norway. 2.976 (100), 1.402 (80), 2.127 (70), 2.118 (70), 2.019 (70), 4.4 (50), 3.19 (50) Chemistry: (1) (2) (1) (2) SiO2 54.08 55.25 MnO trace 0.04 TiO2 0.14 0.23 MgO 11.51 7.23 Al2O3 9.20 16.17 CaO 17.50 12.34 Fe2O3 0.83 1.64 Na2O 4.20 6.19 Cr2O3 0.04 K2O 0.04 0.11 + FeO 2.18 1.36 H2O 0.46 Total 100.14 100.60 2+ (1) Kupplerbrunn, Austria; corresponds to (Ca0:58Na0:32)§=0:90(Mg0:61Al0:31Fe0:06 3+ Ti0:04Fe0:02)§=1:04(Si1:93Al0:07)§=2:00O6: (2) Yakutia, Russia; corresponds to 3+ 2+ (Ca0:46Na0:42K0:01)§=0:89(Al0:58Mg0:38Fe0:04Fe0:04Ti0:01)§=1:05(Si1:92Al0:08)§=2:00O6: Polymorphism & Series: A clinopyroxene solid solution of jadeite (25%{75%), augite (25%{75%), and aegirine (0%{25%). -
Nomenclature of Pyroxenes
Canadian Mineralogist Vol. 27, pp. 143-156 (1989) NOMENCLATURE OF PYROXENES SUBCOMMITTEE ON PYROXENES* COMMISSION ON NEW MINERALS AND MINERAL NAMES INTERNATIONAL MINERALOGICAL ASSOCIATION NOBUO MORIMOTO, Chairman Department of Geology and Mineralogy, University of Kyoto, Kyoto 606, Japan ABSTRACT ou de plusieurs elements. Cent-cinq noms utilises anterieu- rement sont abandonnes formellement. This is the final report on the nomenclature of pyrox- enes by the Subcommittee on Pyroxenes established by the (Traduit par la Redaction) Commission on New Minerals and Mineral Names of the International Mineralogical Association. The recommen- Mots-eMs: pyroxene, nomenclature, Association Interna- dations of the Subcommittee as put forward in this report tionale de Mineralogie, rapport final. have been formally accepted by the Commission. Accepted and widely used names have been chemically defined, by INTRODUCTION combining new and conventional methods, to agree as far as possible with the consensus of present use. Twenty names are formally accepted, among which thirteen are used to The subcommittee on pyroxenes has, after a represent the end members of definite chemical composi- thorough evaluation of the group of pyroxene miner- tions. In common binary solid-solution series, species names als, presented its recommendations for a new clas- are given to the two end members by the "50070 rule". sification and nomenclature to the Commission on Adjectival modifiers for pyroxene mineral names are New Minerals and Mineral Names (hereafter ab- defined to indicate unusual amounts of chemical consti- breviated as CNMMN). These recommendations tuents. This report includes a list of 105 previously used have been approved by the Commission by a for- pyroxene names that have been formally discarded by the Commission.