地质专业词汇英语翻译 2-368 关于建筑的英语词汇 369-370
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Geobotanical Prospecting Around the Navan Zn-Pb Deposit, Ireland: Developing Geochemical Vectors for Mineral Exploration
Goldschmidt2017 Abstract Geobotanical Prospecting around the Navan Zn-Pb Deposit, Ireland: Developing geochemical vectors for mineral exploration DANIJELA MAVRIC1,2*, JOHN H. ASHTON1, SEÁN H. MCCLENAGHAN2 & BALZ S. KAMBER2 1Boliden Tara Mines Limited, Navan, Co Meath, Ireland (*correspondence: [email protected]) 2Department of Geology, ScHool of Natural Sciences, Trinity College Dublin, Dublin, Ireland Recent studies Have shown great potential for Using plants in mineral exploration, for example grass root geocHemistry, wHich led to a discovery of a new AUstralian metallogenic province [1]. In this researcH, the trace-element geocHemistry of native and common plant species in Ireland sucH as ash, beecH, blackberry, Hawthorn, oak, poplar and sycamore was systematically determined above the Navan Zn-Pb deposit (Ireland), cUrrently mined by Boliden Tara Mines Limited. THe study area represents a sub-oUtcropping carbonate-Hosted base˗metal ore body characterised by a large shallow soil Zn- Pb anomaly. The new results show that Zn contents in leaf materials across all species vary from 18 ppm to 700 ppm (dry weigHt). THe HigHest concentrations of Zn are observed in poplar trees growing above subcropping mineralization. Levels of Pb and Cd are anomaloUsly HigH in all investigated tree species grown in soil witH metal anomalies, compared to the backgroUnd values from control sites. In this study, focUs was also placed on Hawthorn and oak as a representative plant species Used for spatial and temporal vectoring. Using trace- element analysis, anomalies can be detected, bUt Uncertainties remain concerning their soUrces. In order to better Understand anomaly soUrce several models of Cu and Zn isotope data will illustrate the typical ranges of metal stable isotopes one migHt expect in diverse geological, and botanical setting. -
Hydrogeology and Simulation of Ground-Water Flow in the Thick Regolith-Fractured Crystalline Rock Aquifer System of Indian Creek
Hydrogeology and Simulation of Ground-Water Flow in the Thick Regolith-Fractured Crystalline Rock Aquifer System of Indian Creek Basin, North Carolina AVAILABILITY OF BOOKS AND MAPS OF THE US. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current- year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publica tions released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may be no longer available. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books and Maps Professional Papers, Bulletins, Water-Supply Papers, Tech Books and maps of the U.S. Geological Survey are available niques of Water-Resources Investigations, Circulars, publications over the counter at the following U.S. Geological Survey Earth Sci of general interest (such as leaflets, pamphlets, booklets), single ence Information Centers (ESIC's), all of which are authorized copies of Preliminary Determination of Epicenters, and some mis agents of the Superintendent of Documents: cellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtain ANCHORAGE, Alaska Rm. 101, 4230 University Dr. able by mail from LAKEWOOD, Colorado Federal Center, Bldg. -
Glide and Screw
Space Groups •The 32 crystallographic point groups, whose operation have at least one point unchanged, are sufficient for the description of finite, macroscopic objects. •However since ideal crystals extend indefinitely in all directions, we must also include translations (the Bravais lattices) in our description of symmetry. Space groups: formed when combining a point symmetry group with a set of lattice translation vectors (the Bravais lattices), i.e. self-consistent set of symmetry operations acting on a Bravais lattice. (Space group lattice types and translations have no meaning in point group symmetry.) Space group numbers for all the crystal structures we have discussed this semester, and then some, are listed in DeGraef and Rohrer books and pdf. document on structures and AFLOW website, e.g. ZnS (zincblende) belongs to SG # 216: F43m) Class21/1 Screw Axes •The combination of point group symmetries and translations also leads to two additional operators known as glide and screw. •The screw operation is a combination of a rotation and a translation parallel to the rotation axis. •As for simple rotations, only diad, triad, tetrad and hexad axes, that are consistent with Bravais lattice translation vectors can be used for a screw operator. •In addition, the translation on each rotation must be a rational fraction of the entire translation. •There is no combination of rotations or translations that can transform the pattern produced by 31 to the pattern of 32 , and 41 to the pattern of 43, etc. •Thus, the screw operation results in handedness Class21/2 or chirality (can’t superimpose image on another, e.g., mirror image) to the pattern. -
Linn E and Taxonomy in Japan: on the 300Th Anniversary of His Birth
No. 3] Proc. Jpn. Acad., Ser. B 86 (2010) 143 Linne and taxonomy in Japan: On the 300th anniversary of his birth By Akihito (His Majesty The Emperor of Japan) (Communicated by Koichiro TSUNEWAKI, M.J.A.) President, dear friends bers of stamens belonged to dierent classes, even when their other characteristics were very similar, I am very grateful to the Linnean Society of while species with the same number of stamens be- London for the kind invitation it extended to me to longed to the same class, even when their other participate in the celebration of the 300th anniver- characteristics were very dierent. This led to the sary of the birth of Carl von Linne. When, in 1980, I idea that the classication of organisms should be was elected as a foreign member of the Society, I felt based on a more comprehensive evaluation of all I did not really deserve the honour, but it has given their characteristics. This idea gained increasing me great encouragement as I have tried to continue support, and Linne’s classication system was even- my research, nding time between my ofcial duties. tually replaced by systems based on phylogeny. Today, I would like to speak in memory of Carl The binomial nomenclature proposed by Linne, von Linne, and address the question of how Euro- however, became the basis of the scientic names of pean scholarship has developed in Japan, touching animals and plants, which are commonly used in the upon the work of people like Carl Peter Thunberg, world today, not only by people in academia but also Linne’s disciple who stayed in Japan for a year as by the general public. -
The Håkåneset Rockslide, Tinnsjø
The Håkåneset rockslide, Tinnsjø Stability analysis of a potentially rock slope instability. Inger Lise Sollie Geotechnology Submission date: June 2014 Supervisor: Bjørn Nilsen, IGB Norwegian University of Science and Technology Department of Geology and Mineral Resources Engineering I II ABSTRACT The Håkåneset rockslide is located on the west shore of Lake Tinnsjø (191 m.a.s.l), a fjordlake stretching 32 km with a SSE-NNW orientation in Telemark, southern Norway. The instability extends from 550 m.a.s.l. and down to approximately 300 m depth in the lake, making up a surface area of 0.54 km2 under water and 0.50 km2 on land. The rockslide comprises an anisotropic metavolcanic rock that is strongly fractured. Five discontinuity sets are identified with systematic field mapping supported by structural analysis of terrestrial laser scan (TLS) data. These are interpreted as gravitationally reactivated inherited tectonic structures. At the northern end the instability is limited by a steep south-east dipping joint (JF3 (~133/77)) that is one direction of a conjugate strike slip fault set (JF3, JF2 (~358/65)). Towards the south the limit to the stable bedrock is transitional. A back scarp is defined by a north-east dipping J1 (~074/59) surface that is mapped out at 550 m.a.s.l. Kinematic analysis indicates that planar sliding, wedge sliding and toppling are feasible. However, because the joint sets are steeply dipping these failure mechanisms can only occur for small rock volumes and are limited to steep slope sections only. Large scale rock slope deformation can only be justified by assuming deformation along a combination of several anisotropies. -
Botanical Nomenclature: Concept, History of Botanical Nomenclature
Module – 15; Content writer: AvishekBhattacharjee Module 15: Botanical Nomenclature: Concept, history of botanical nomenclature (local and scientific) and its advantages, formation of code. Content writer: Dr.AvishekBhattacharjee, Central National Herbarium, Botanical Survey of India, P.O. – B. Garden, Howrah – 711 103. Module – 15; Content writer: AvishekBhattacharjee Botanical Nomenclature:Concept – A name is a handle by which a mental image is passed. Names are just labels we use to ensure we are understood when we communicate. Nomenclature is a mechanism for unambiguous communication about the elements of taxonomy. Botanical Nomenclature, i.e. naming of plants is that part of plant systematics dealing with application of scientific names to plants according to some set rules. It is related to, but distinct from taxonomy. A botanical name is a unique identifier to which information of a taxon can be attached, thus enabling the movement of data across languages, scientific disciplines, and electronic retrieval systems. A plant’s name permits ready summarization of information content of the taxon in a nested framework. A systemofnamingplantsforscientificcommunicationmustbe international inscope,andmustprovideconsistencyintheapplicationof names.Itmustalsobeacceptedbymost,ifnotall,membersofthe scientific community. These criteria led, almost inevitably, to International Botanical Congresses (IBCs) being the venue at which agreement on a system of scientific nomenclature for plants was sought. The IBCs led to publication of different ‘Codes’ which embodied the rules and regulations of botanical nomenclature and the decisions taken during these Congresses. Advantages ofBotanical Nomenclature: Though a common name may be much easier to remember, there are several good reasons to use botanical names for plant identification. Common names are not unique to a specific plant. -
M.Sc. Plant Science (Applicable to Students Admitted in 2009 Onwards)
M.Sc. Plant Science (Applicable to students admitted in 2009 onwards) (w.e.f. examination of 2009 onwards) M.Sc. I (Previous) Semester I Paper I - Microbiology (Bacteriology, Virology) and Microbial 100 Marks Biotechnology. Paper II - Mycology & Plant Pathology (Fungal Diseases) 100 Marks Paper III - Algology & Lichenology 100 Marks Paper IV - Bryology 100 Marks Practical - Based on Papers I to IV including 200 Marks Class and Field Work (Local excursion) 600 Marks Semester II Paper V - Pteridophytes 100 Marks Paper VI - Gymnosperms and Palaeobotany 100 Marks Paper VII - Angiosperms: Taxonomy and Economic Botany 100 Marks Paper VIII - Angiosperms: Histology, Anatomy, Embryology 100 Marks Practical - Based on Papers V to VIII 200 Marks - Class and Field Work (Local excursion) 600 Marks Students have to take all the eight papers. M.Sc. II (Final) Semester III Paper I - Cytology, Genetics and Cytogenetics 100 Marks Paper II - Plant Breeding and Biostatistics 100 Marks Paper III - Ecology, Environment and Soil Science 100 Marks Paper IV - Modern experimental techniques and computer application 100 Marks Practical - Based on Papers I to IV including 200 Marks - Class and field work/Laboratory visit 600 Marks Semester IV Paper V - Plant Physiology 100 Marks Paper VI - Cell Biology & Plant Biochemistry 100 Marks Paper VII - Biotechnology and Human welfare 100 Marks Paper VIII Elective - Project work (Review based on all Papers from 100 Marks Semester I to IV) Practical - Based on Papers V and VII 200 Marks (Incl. Biotech Lab visits & class work) 600 Marks Students have to take all the seven papers (a) The theory papers would have internal evaluation by the teaching/guest faculty as decided by the Coordinator in accordance with the nature and requirement of the subject and shall be notified to the students in the beginning of the semester. -
Iidentilica2tion and Occurrence of Uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals from the Colorado Plateaus
IIdentilica2tion and occurrence of uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals From the Colorado Plateaus c By A. D. WEEKS and M. E. THOMPSON A CONTRIBUTION TO THE GEOLOGY OF URANIUM GEOLOGICAL S U R V E Y BULL E TIN 1009-B For jeld geologists and others having few laboratory facilities.- This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE- INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan. Director Reprint, 1957 For sale by the Superintendent of Documents, U. S. Government Printing Ofice Washington 25, D. C. - Price 25 cents (paper cover) CONTENTS Page 13 13 13 14 14 14 15 15 15 15 16 16 17 17 17 18 18 19 20 21 21 22 23 24 25 25 26 27 28 29 29 30 30 31 32 33 33 34 35 36 37 38 39 , 40 41 42 42 1v CONTENTS Page 46 47 48 49 50 50 51 52 53 54 54 55 56 56 57 58 58 59 62 TABLES TABLE1. Optical properties of uranium minerals ______________________ 44 2. List of mine and mining district names showing county and State________________________________________---------- 60 IDENTIFICATION AND OCCURRENCE OF URANIUM AND VANADIUM MINERALS FROM THE COLORADO PLATEAUS By A. D. WEEKSand M. E. THOMPSON ABSTRACT This report, designed to make available to field geologists and others informa- tion obtained in recent investigations by the Geological Survey on identification and occurrence of uranium minerals of the Colorado Plateaus, contains descrip- tions of the physical properties, X-ray data, and in some instances results of chem- ical and spectrographic analysis of 48 uranium arid vanadium minerals. -
1 NANO 704-Crystallography & Structure of Nanomaterials 3
1 NANO 704-Crystallography & Structure of Nanomaterials 3. Space Groups Space lattices Lattice points are all equivalent by translational symmetry. We start with a primitive lattice, having points at rabcuvw uvw, where uvw,, ¢ . So lattice points exist at (0,0,0) and all equivalent positions. If we have a lattice point at xyz,, , then we also have a lattice point at xuyvzw,, . Suppose two lattice points exist at xyz111,, and xyz222,, . If xyz,, is a lattice point, then xyz,, x212121 x , y y , z z is also a lattice point. But this does not imply that for all xyz,, representing lattice points, the values of xyz,, are integers. In particular, it is often useful to represent some of them by half integers. A primitive cell has lattice points at 0,0,0 . Centered cells have additional lattice points. 11 An A-centered cell also has points at 0,22 , . (Center of the A face.) 11 A B-centered cell also has points at 22,0, . (Center of the B face.) 11 A C-centered cell also has points at 22,,0. (Center of the C face.) 11 11 11 An F (face)-centered cell also has points at 0,22 , , 22,0, , 22,,0. (Centers of all three faces.) 111 An I (body)-centered cell also has points at 222,, . (Center point of the unit cell.) Observations I. Suppose a cell is both A- and B-centered. The lattice points exist at 11 11 P1 : 0,0,0 , P2 : 0,22 , , and P3 : 22,0, and equivalent positions. P1 and P2 form a lattice row. -
Tigers Eye Free
FREE TIGERS EYE PDF Karen Robards | 400 pages | 11 May 2010 | HarperCollins Publishers Inc | 9780380755554 | English | New York, United States Tigers Eye Stone Meaning & Uses: Aids Harmonious Balanced Action Tiger's eye also called tiger eye is a Tigers Eye gemstone that is usually a metamorphic rock with a golden to red-brown colour and a silky lustre. As members of the quartz group, tiger's eye and the related blue-coloured mineral hawk's eye gain their silky, lustrous appearance from the parallel intergrowth of quartz crystals and altered amphibole fibres that have mostly turned into limonite. Tiger iron is an altered rock composed chiefly of tiger's eye, red jasper and black hematite. The undulating, contrasting bands of colour and lustre make for an attractive motif and it is Tigers Eye used for Tigers Eye and ornamentation. Tiger iron is a popular ornamental material Tigers Eye in a variety of applications, from beads to knife hilts. Tiger iron is mined primarily in South Africa and Western Australia. Tiger's eye is composed chiefly of silicon dioxide SiO 2 and is coloured mainly by Tigers Eye oxide. The specific gravity ranges from 2. Serpentine deposits in which are occasionally found chatoyant bands of chrysotile fibres have been found in the US states of Arizona and California. These have been cut and sold as "Arizona tiger-eye" and "California tiger's eye" gemstones. In some parts of the world, the stone is believed to ward off the evil eye. Gems are usually given a cabochon cut to best display their chatoyance. -
The Picking Table Volume 50, No. 2 – Fall 2009
2009FallPT:Layout 1 8/27/2009 10:21 AM Page 1 JOURNAL OF THE FRANKLIN-OGDENSBURG MINERALOGICAL SOCIETY Volume 50, No. 2 – Fall 2009 $20.00 U.S. SPECIAL EDITION TH 50 ANNIVERSARY The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. 2009FallPT:Layout 1 8/27/2009 10:21 AM Page 2 The Franklin-Ogdensburg Mineralogical Society, Inc. OFFICERS and STAFF 2009 PRESIDENT SLIDE COLLECTION CUSTODIAN Bill Truran Edward H. Wilk 2 Little Tarn Court, Hamburg, NJ 07419 202 Boiling Springs Avenue (973) 827-7804 E. Rutherford, NJ 07073 [email protected] (201) 438-8471 VICE-PRESIDENT TRUSTEES Richard Keller C. Richard Bieling (2009-2010) 13 Green Street, Franklin, NJ 07416 Richard C. Bostwick (2009-2010) (973) 209-4178 George Elling (2008-2009) [email protected] Steven M. Kuitems (2009-2010) Chester S. Lemanski, Jr. (2008-2009) SECOND VICE-PRESIDENT Lee Lowell (2008-2009) Joe Kaiser Earl Verbeek (2008-2009) 40 Castlewood Trail, Sparta, NJ 07871 Edward H. Wilk (2008-2009) (973) 729-0215 Fred Young (2008-2009) [email protected] LIAISON WITH THE EASTERN FEDERATION SECRETARY OF MINERALOGICAL AND LAPIDARY Tema J. Hecht SOCIETIES (EFMLS) 600 West 111TH Street, Apt. 11B Delegate Joe Kaiser New York, NY 10025 Alternate Richard C. Bostwick (212) 749-5817 (Home) (917) 903-4687 (Cell) COMMITTEE CHAIRPERSONS [email protected] Auditing William J. Trost Field Trip Warren Cummings TREASURER Historical John L. Baum Denise Kroth Mineral Exchange Richard C. Bostwick 240 Union Avenue Nominating William Kroth Wood-Ridge, NJ 07075 Program Fred Young (201) 933-3029 Swap & Sell Chester S. -
1469 Vol 43#5 Art 03.Indd
1469 The Canadian Mineralogist Vol. 43, pp. 1469-1487 (2005) BORATE MINERALS OF THE PENOBSQUIS AND MILLSTREAM DEPOSITS, SOUTHERN NEW BRUNSWICK, CANADA JOEL D. GRICE§, ROBERT A. GAULT AND JERRY VAN VELTHUIZEN† Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ABSTRACT The borate minerals found in two potash deposits, at Penobsquis and Millstream, Kings County, New Brunswick, are described in detail. These deposits are located in the Moncton Subbasin, which forms the eastern portion of the extensive Maritimes Basin. These marine evaporites consist of an early carbonate unit, followed by a sulfate, and fi nally, a salt unit. The borate assemblages occur in specifi c beds of halite and sylvite that were the last units to form in the evaporite sequence. Species identifi ed from drill-core sections include: boracite, brianroulstonite, chambersite, colemanite, congolite, danburite, hilgardite, howlite, hydroboracite, kurgantaite, penobsquisite, pringleite, ruitenbergite, strontioginorite, szaibélyite, trembathite, veatchite, volkovskite and walkerite. In addition, 41 non-borate species have been identifi ed, including magnesite, monohydrocalcite, sellaite, kieserite and fl uorite. The borate assemblages in the two deposits differ, and in each deposit, they vary stratigraphically. At Millstream, boracite is the most common borate in the sylvite + carnallite beds, with hilgardite in the lower halite strata. At Penobsquis, there is an upper unit of hilgardite + volkovskite + trembathite in halite and a lower unit of hydroboracite + volkov- skite + trembathite–congolite in halite–sylvite. At both deposits, values of the ratio of B isotopes [␦11B] range from 21.5 to 37.8‰ [21 analyses] and are consistent with a seawater source, without any need for a more exotic interpretation.