THE JOURNAL of GEMMOLOGY and PROCEEDINGS of the GEMMOLOGICAL ASSOCIATION of GREAT BRITJ\IN
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Phase Equilibria and Thermodynamic Properties of Minerals in the Beo
American Mineralogist, Volwne 71, pages 277-300, 1986 Phaseequilibria and thermodynamic properties of mineralsin the BeO-AlrO3-SiO2-H2O(BASH) system,with petrologicapplications Mlnx D. B.qnroN Department of Earth and SpaceSciences, University of California, Los Angeles,Los Angeles,California 90024 Ansrru,cr The phase relations and thermodynamic properties of behoite (Be(OH)r), bertrandite (BeoSirOr(OH)J, beryl (BerAlrSiuO,r),bromellite (BeO), chrysoberyl (BeAl,Oo), euclase (BeAlSiOo(OH)),and phenakite (BerSiOo)have been quantitatively evaluatedfrom a com- bination of new phase-equilibrium, solubility, calorimetric, and volumetric measurements and with data from the literature. The resulting thermodynamic model is consistentwith natural low-variance assemblagesand can be used to interpret many beryllium-mineral occurTences. Reversedhigh-pressure solid-media experimentslocated the positions of four reactions: BerAlrSiuO,,: BeAlrOo * BerSiOo+ 5SiO, (dry) 20BeAlSiOo(OH): 3BerAlrsi6or8+ TBeAlrOo+ 2BerSiOn+ l0HrO 4BeAlSiOo(OH)+ 2SiOr: BerAlrSiuO,,+ BeAlrOo+ 2H2O BerAlrSiuO,,+ 2AlrSiOs : 3BeAlrOa + 8SiO, (water saturated). Aqueous silica concentrationswere determined by reversedexperiments at I kbar for the following sevenreactions: 2BeO + H4SiO4: BerSiOo+ 2H2O 4BeO + 2HoSiOo: BeoSirO'(OH),+ 3HrO BeAlrOo* BerSiOo+ 5H4Sio4: Be3AlrSiuOr8+ loHro 3BeAlrOo+ 8H4SiO4: BerAlrSiuOrs+ 2AlrSiO5+ l6HrO 3BerSiOo+ 2AlrSiO5+ 7H4SiO4: 2BerAlrSiuOr8+ l4H2o aBeAlsioloH) + Bersio4 + 7H4sio4:2BerAlrsiuors + 14Hro 2BeAlrOo+ BerSiOo+ 3H4SiOo: 4BeAlSiOr(OH)+ 4HrO. -
TRENDS in MANDALAY Photo Credits
Local Governance Mapping THE STATE OF LOCAL GOVERNANCE: TRENDS IN MANDALAY Photo credits Paul van Hoof Mithulina Chatterjee Myanmar Survey Research The views expressed in this publication are those of the author, and do not necessarily represent the views of UNDP. Local Governance Mapping THE STATE OF LOCAL GOVERNANCE: TRENDS IN MANDALAY UNDP MYANMAR Table of Contents Acknowledgements II Acronyms III Executive Summary 1 1. Introduction 11 2. Methodology 14 2.1 Objectives 15 2.2 Research tools 15 3. Introduction to Mandalay region and participating townships 18 3.1 Socio-economic context 20 3.2 Demographics 22 3.3 Historical context 23 3.4 Governance institutions 26 3.5 Introduction to the three townships participating in the mapping 33 4. Governance at the frontline: Participation in planning, responsiveness for local service provision and accountability 38 4.1 Recent developments in Mandalay region from a citizen’s perspective 39 4.1.1 Citizens views on improvements in their village tract or ward 39 4.1.2 Citizens views on challenges in their village tract or ward 40 4.1.3 Perceptions on safety and security in Mandalay Region 43 4.2 Development planning and citizen participation 46 4.2.1 Planning, implementation and monitoring of development fund projects 48 4.2.2 Participation of citizens in decision-making regarding the utilisation of the development funds 52 4.3 Access to services 58 4.3.1 Basic healthcare service 62 4.3.2 Primary education 74 4.3.3 Drinking water 83 4.4 Information, transparency and accountability 94 4.4.1 Aspects of institutional and social accountability 95 4.4.2 Transparency and access to information 102 4.4.3 Civil society’s role in enhancing transparency and accountability 106 5. -
The Making of Modern Burma Thant Myint-U Index More Information
Cambridge University Press 0521780217 - The Making of Modern Burma Thant Myint-U Index More information Index Abhisha Husseini, 51 and local rebellions, 172, 173–4, 176 Afghanistan, 8, 22, 98, 102, 162 and modern Burma, 254 agriculture, 36, 37, 40, 44, 47, 119, 120, payment of, 121 122, 167, 224, 225, 236, 239; see also reforms, 111–12 cultivators Assam, 2, 13, 15–16, 18, 19, 20, 95, 98, 99, Ahom dynasty, 15–16 220 Aitchison, Sir Charles, 190–1 athi, 33, 35 Alaungpaya, King, 13, 17, 58, 59–60, 61, Ava (city), 17, 25, 46, 53, 54 70, 81, 83, 90, 91, 107 population, 26, 54, 55 Alaungpaya dynasty, 59, 63, 161 Ava kingdom, 2 allodial land, 40, 41 administration, 28–9, 35–8, 40, 53–4, Alon, 26, 39, 68, 155, 173, 175 56–7, 62, 65–8, 69, 75–8, 108–9, Amarapura, 14, 17, 18, 20, 21, 26, 51, 53, 115–18, 158–60, 165–6 54, 119, 127, 149 anti-British attitudes, 6–7, 99, 101–3 rice prices, 143 and Bengal, 94, 95, 96, 98, 99–100 royal library, 96 boundaries of, 9, 12, 24–5, 92, 101, Amarapura, Myowun of, 104–5 220 Amherst, Lord, 106 British attitudes to, 6, 8–9, 120, 217–18, Amyint, 36, 38, 175 242, 246, 252 An Tu (U), 242 and Buddhism, 73–4, 94, 95, 96, 97, 108, Anglo-Burmese wars, 2, 79 148–52, 170–1 First (1824–6), 18–20, 25, 99, 220 ceremonies, 97, 149, 150 Second (1852–3), 23, 104, 126 and China, 47–8, 137, 138, 141, 142, Third (1885), 172, 176, 189, 191–3 143, 144, 147–8 animal welfare, 149, 171 chronicles of, 79–83, 86, 240 appanages, 29, 53, 61–3, 68, 69, 72–3, 77, and colonial state, 219–20 107, 108, 231 commercial concessions, 136–7 reform of, -
Myanmar (Burma)
©Lonely Planet Publications Pty Ltd Myanmar (Burma) Northern Myanmar p271 Mandalay & Around p234 Western ^# Myanmar Bagan & Eastern p307 Central Myanmar Myanmar p196 p141 Southwestern Myanmar ^# Yangon p86 p34 Southeastern Myanmar p105 Simon Richmond, David Eimer, Adam Karlin, Nick Ray, Regis St Louis PLAN YOUR TRIP ON THE ROAD Welcome to Myanmar . 4 YANGON . 34 Myeik . 131 Myanmar Map . 6 Myeik (Mergui) Archipelago . 135 Myanmar’s Top 10 . .8 SOUTHWESTERN Kawthoung . 138 MYANMAR . 86 Need to Know . 14 Thanlyin & Kyauktan . 87 What’s New . 16 BAGAN & CENTRAL Bago . 88 MYANMAR . 141 If You Like… . 17 Pathein . .. 94 Yangon–Mandalay Month by Month . 19 Chaung Tha Beach . .. 99 Highway . 143 Ngwe Saung Beach . 102 Itineraries . 21 Taungoo (Toungoo) . 143 Nay Pyi Taw . 146 Before You Go . 23 SOUTHEASTERN Meiktila . 149 Regions at a Glance . 30 MYANMAR . 105 Yangon–Bagan Mon State . 107 Highway . 151 2P2PLAY / SHUTTERSTOCK © SHUTTERSTOCK / 2P2PLAY Mt Kyaiktiyo Pyay . 151 (Golden Rock) . 107 Thayekhittaya Mawlamyine . 109 (Sri Ksetra) . 154 Around Mawlamyine . 116 Magwe . 155 Ye . 119 Bagan . 156 Kayin State . 121 Nyaung U . 158 Hpa-an . 121 Old Bagan . 164 Around Hpa-an . 124 Myinkaba . 167 Myawaddy . 126 New Bagan (Bagan Myothit) . 167 Tanintharyi Region . 127 Around Bagan . 172 STREET FOOD AT BOGYOKE AUNG Dawei . 127 SAN MARKET P54, YANGON CHANTAL DE BRUIJNE / SHUTTERSTOCK © SHUTTERSTOCK / BRUIJNE DE CHANTAL SHWE YAUNGHWE KYAUNG P197, NYAUNGSHWE Contents UNDERSTAND Mt Popa . 172 Mingun . 269 Myanmar Salay . 173 Paleik . 270 Today . 336 Pakokku . 175 History . 338 Monywa . 176 NORTHERN People & Religious Around Monywa . 178 MYANMAR . 271 Beliefs of Myanmar . 352 Mandalay to Lashio . 273 Aung San Suu Kyi . -
Mandalay Region Census Report Volume 3 – L
THE REPUBLIC OF THE UNION OF MYANMAR The 2014 Myanmar Population and Housing Census Mandalay Region Census Report Volume 3 – l Department of Population Ministry of Immigration and Population May 2015 The 2014 Myanmar Population and Housing Census Mandalay Region Report Census Report Volume 3 – I For more information contact: Department of Population Ministry of Immigration and Population Office No. 48 Nay Pyi Taw Tel: +95 67 431 062 www.dop.gov.mm May, 2015 Figure 2: Map of Mandalay Region, Districts and Townships ii Census Report Volume 3–I (Mandalay) Foreword The 2014 Myanmar Population and Housing Census (2014 MPHC) was conducted from 29th March to 10th April 2014 on a de facto basis. The successful planning and implementation of the census activities, followed by the timely release of the provisional results in August 2014 and now the main results in May 2015, is a clear testimony of the Government’s resolve to publish all information collected from respondents in accordance with the Population and Housing Census Law No. 19 of 2013. It is now my hope that the main results both Union and each of the State and Region reports will be interpreted correctly and will effectively inform the planning and decision-making processes in our quest for national and sub-national development. The census structures put in place, including the Central Census Commission, Census Committees and officers at the State/Region, District and Township levels and the International Technical Advisory Board (ITAB), a group of 15 experts from different countries and institutions involved in censuses and statistics internationally, provided the requisite administrative and technical inputs for the implementation of the census. -
Heat Capacities and Thermodynamic Functions for Beryl, Beralrsiuotr
American Mineralogist, Volume 7I, pages 557-568, 1986 Heat capacitiesand thermodynamicfunctions for beryl, BerAlrSiuOtr, phenakite, BerSiOn,euclase, BeAlSiOo(OH)' bertranditeo BeoSirOt(OH)r,and chrysoberyl' BeAl2Oa B. S. HnluNcw.q,Y U.S. GeologicalSurvey, Reston, Y irgrnia22092 M. D. B.nnroN Departmentof Earthand SpaceSciences, University of California,Los Angeles,Los Angeles,California 90024 R. A. Ronrn, H. T. HLsnr.roN, Jn. U.S. GeologicalSurvey, Reston, Y irginia22092 Ansrru,cr The heat capacities of beryl, phenakite, euclase,and bertrandite have been measured betweenabout 5 and 800 K by combined quasi-adiabaticcryogenic calorimetry and dif- ferential scanningcalorimetry. The heat capacitiesof chrysoberylhave beenmeasured from 340 to 800 K. The resulting data have been combined with solution and phase-equilibrium experimentaldata and simultaneouslyfit using the program pHAS2oto provide an internally consistent set of thermodynamic properties for several important beryllium phases.The experimentalheat capacitiesand tablesof derived thermodynamic propertiesare presented in this report. The derived thermodynamic properties at I bar and 298.15 K for the stoichiometric beryllium phasesberyl, phenakite, euclase,and bertrandite are entropies of 346.7 + 4.7, 63.37+0.27,89.09+0.40, andl72.l+0.77 J/(mol'K),respectively,andGibbsfree energiesof formation(elements) of -8500.36 + 6.39, -2028.39 + 3.78, -2370.17 + 3.04, and -4300.62 + 5.45 kJlmol, respectively,and, -2176.16 + 3.18kJ/mol for chrysoberyl. The coefficientscr to c, of the heat-capacityfunctions are as follows: valid phase ct c2 c, x 105 c4 c, x 10-6 range beryl 1625.842 -0.425206 12.0318 -20 180.94 6.82544 200-1800K phenakite 428.492 -0.099 582 1.9886 -5 670.47 2.0826 200-1800K euclase 532.920 -0.150729 4.1223 -6726.30 2.1976 200-1800K bertrandite 825.336 -0.099 651 -10 570.31 3.662r7200-1400 K chrysoberyl 362.701 -0.083 527 2.2482 -4033.69 -6.7976 200-1800K whereC!: cr * ctT + crT2 * coT-os* crT-2and Zisinkelvins. -
Geochemical Journal, Vol. 55 (No. 4), Pp. 209-222, 2021
Geochemical Journal, Vol. 55, pp. 209 to 222, 2021 doi:10.2343/geochemj.2.0630 10Be/9Be ratios of phenakite and beryl measured via direct Cs sputtering: Implications for selecting suitable Be carrier minerals for the measurement of low-level 10Be ATSUNORI NAKAMURA,1* ATSUYUKI OHTA,1 HIROYUKI MATSUZAKI2 and TAKASHI OKAI1 1Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba Central 7, 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan 2Micro Analysis Laboratory, Tandem Accelerator (MALT), The University Museum, The University of Tokyo, 2-11-16, Yayoi, Bunkyo-ku, Tokyo 113-0032, Japan (Received December 23, 2020; Accepted April 29, 2021) Preparing Be carrier solutions with low 10Be/9Be ratios is essential for the applications of in-situ-produced cosmogenic 10Be in geochronology. This is because commercially available Be carriers are non-negligibly contaminated by 10Be. Recently, in-house Be carriers have been successfully applied to samples that contain small amounts of in-situ-produced 10Be. The first step in preparing in-house Be carriers is selecting suitable Be-bearing minerals that contain less 10Be. Here, we present a simple method for selecting appropriate raw minerals for in-house Be carriers. That is, measuring the 10Be/ 9 10 9 Be ratios of Be-bearing minerals by direct Cs sputtering. Analyses of the Be/ Be ratios of phenakite (Be2SiO4) and beryl (Be3Al2Si6O18) obtained from a mineral collection at the Geological Survey of Japan indicate that phenakite gener- ally contains more 10B, interfering isobar of 10Be, than beryl. In addition to the necessity of finding raw materials that contain low 10Be, our results indicate that it is preferable to select a starting material with a low B concentration. -
Myanmar Arrow Brothers Lot #RH.Indd
Myanmar Mogok MYANMAR ARROW BROTHERS LOT #RH Profi le Country Myanmar Division Mandalay District Pyin Oo Lwin Township Mogok Village Bhamon Farm Ruby Hills Producer Thi Ha Ram Gyawalie Altitude 1311 masl Varietal Caturra, Catimor Harvest January - March Process Washed Myanmar Arrow Brothers Lot #RH Myanmar Thi Ha Gyawalie is currently the youngest coffee producer in Myanmar at 24 years old. His family has been growing coffee for the past 14 years. Three Arrow Brothers years ago Thi Ha became director of Arrow Brothers, where he changed some handling of processing and applied for an organic certifi cation that Lot #RH has been awarded. He has started playing with processing methods such as carbonic maceration and fermentation as well as producing naturals and honeys, and is known for staying up until the early hours cupping in order to get the best from his crop. His farm is situated in an area which remains closed for foreigners, known as ‘The Valley of the Rubies’. Mogok sits four miles long and two miles wide surrounded by the many mountains of the Shan Plateau. It was destined to be entered in competition, but there was not enough left over to enter after being sold! Once the cherries are picked, they are pulped and fermented for 48 hours in equally sized tanks to ensure consistency within batches. Once this has been done, they are moved to raised beds and dried for 2-3 weeks before being dry milled and bagged for shipping. Drying the washed coffee. -
MYANMAR A? Flood Kachin, Shan (North) State and Sagaing, Mandalay, Magway Region Imagery Analysis: 25 July 2020 | Published 5 August 2020 | Version 1.0 FL20200730MMR
MYANMAR A? Flood Kachin, Shan (North) State and Sagaing, Mandalay, Magway Region Imagery analysis: 25 July 2020 | Published 5 August 2020 | Version 1.0 FL20200730MMR 94?40'0"E 95?20'0"E 96?0'0"E 96?40'0"E 97?20'0"E M O H N Y I N M Y I T K Y I N A H K A M T I Map location T A M U K A T H A K A C H I N B H A M O M Y A N M A R N " 0 ' 0 ? N 4 " 2 0 ' 0 ? 4 2 M AW L A I K K A W L I N M U S E M O N G M I T N " 0 ' 0 2 N ? " 3 0 ' 2 0 2 ? K A N B A L U Satellite detected water extent as 3 2 S A G A I N G of 25 July 2020 in central part of P A L A U N G S E L F - A D M I N I S T E R E D Z O N E Myanmar This map illustrates satellite-detected surface K A L E L A S H I O S H A N ( N O R T H ) waters over Kachin, Shan (North) State and MOGOK Sagaing, Mandalay, Magway Region of Myanmar as observed from a Terra(MODIS) L A S H I O N " 0 image acquired on 25 July 2020 due to the ' S H W E B O 0 4 N ? " 2 0 ' 2 current monsoon rains. -
The Seven Crystal Systems
Learning Series: Basic Rockhound Knowledge The Seven Crystal Systems The seven crystal systems are a method of classifying crystals according to their atomic lattice or structure. The atomic lattice is a three dimensional network of atoms that are arranged in a symmetrical pattern. The shape of the lattice determines not only which crystal system the stone belongs to, but all of its physical properties and appearance. In some crystal healing practices the axial symmetry of a crystal is believed to directly influence its metaphysical properties. For example crystals in the Cubic System are believed to be grounding, because the cube is a symbol of the element Earth. There are seven crystal systems or groups, each of which has a distinct atomic lattice. Here we have outlined the basic atomic structure of the seven systems, along with some common examples of each system. Cubic System Also known as the isometric system. All three axes are of equal length and intersect at right angles. Based on a square inner structure. Crystal shapes include: Cube (diamond, fluorite, pyrite) Octahedron (diamond, fluorite, magnetite) Rhombic dodecahedron (garnet, lapis lazuli rarely crystallises) Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Cubic Crystals: Diamond Fluorite Garnet Spinel Gold Pyrite Silver Tetragonal System Two axes are of equal length and are in the same plane, the main axis is either longer or shorter, and all three intersect at right angles. Based on a rectangular inner structure. Crystal shapes include: Four-sided prisms and pyramids Trapezohedrons Eight-sided and double pyramids Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Tetragonal Crystals: Anatase Apophyllite Chalcopyrite Rutile Scapolite Scheelite Wulfenite Zircon Hexagonal System Three out of the four axes are in one plane, of the same length, and intersect each other at angles of 60 degrees. -
THE BIRON HYDROTHERMAL SYNTHETIC EMERALD by Robert E
THE BIRON HYDROTHERMAL SYNTHETIC EMERALD By Robert E. Kane and Richard T. Liddicoat, ]r. A new synthetic emerald grown in Western merald was first synthesized by Ebelman in 1848 by Australia is now commercially available E adding natural emerald powder to a molten boric acid as faceted stones. Infrared spectra revealed flux, which produced very small prismatic emerald crys- the presence of water, thereby confirming tals as the mixture cooled. In the ensuing years, the flux that these synthetic emeralds are synthe- growth of synthetic emerald was achieved by many re- sized by a hydrothermal process. Chemical searchers (Nassau, 1980; Sinkankas, 198 1). In 1957, the analysis showed that they contain vana- dium as well as lesser amounts of chro- growth of minute beryl crystals by a hydrothermal process mium. This new synthetic exhibits some was first reported [Wyart and ¤6avnic~r1957). Although characteristics that are distinctly different many processes for growing synthetic emerald hydro- from other synthetic emeralds and there- thermally have been described since then (summarized in fore must now be considered when identi- Sinkankas, 1981),until recently only three major produc- fying emeralds. In addition to distinctive tions of hydrothermal synthetic emerald have been com- inclusions such as gold, the Biron synthetic mercially available to the jewelry trade: Linde (patented is inert to ultraviolet radiation, has a spe- process now owned by Regency), Lechleitner (full syn- cific gravity of 2.68 -2.71, and refractive thetic in addition to overgrowth), and, most recently, those indices of = 1,569 and (D = 1.573. This ar- grown in the Soviet Union (see Talzubo, 1979). -
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American Mineralogist, Volume 63, pages 664_676, l97g Multisyste_msanalysis of beryiliumminerar stabilities: the systemBeO-A[rOa_SiO2_H2O DoNer.n M. Bunr Department of Geology, Arizona State (Jniuersitv Tempe,Arizona8528I Abstract seven commonly associatedminerals in the systemBeo-Alror-Sior-Hro includechry- soberyl,phenakite, euclase,bertrandite, beryl, kaolinite,and qiuit . The phaserule implies that not more than six of theseminerals can coexistat an invariantpoint, and, with the addition of an aqueousphase, the associationconstitutes an (n * 4; ptrase(negative two d-egreesof freedom)multisystem. The apparentincompatibility of taotinite with phenakite allowsthe splitting of this unwieldymultisystem into two smaller(n + 3) phasemultisystems, which may belabeled (Kao) and (phe).Moiar volumedata, compuier program RrlcrroN, and naturalassemblages can then be usedto derivethe presumablystabie cJnfiguration of these multisystemson p"-minus an isothermal pHro diagram. n, p-r diagramprojected through theaqueous phase shouldhave the sametopology, and cansimilarlf be drawn. on the resultingdiagrams, three . invariant-butpoinis rabeled tchrl, tBr;;, and [etz] arestable in the.multisystem (Kao), and threedistinct identically-fuU"i.Opoint, u.. stablein rhe multisystem(Phe). An implicationof this topologyvia ihe "r.tu.tubl"-rtable correspon- dence,"is that the assemblagephenakite + euclase* beryl(* aqueousphase) has a finite i'I;ix, ii,l'J.?lT"t' ::ff,,,j :r;: :":.T' ? ts why" euclase is muchrarer than bertrandite. and its stabilityfield, especially