calc in English
calcalkaline
Use "calc" in a sentence
1. Accumulations of Change AP Calc AB 1
2. Choose Format-Alignment-Left (%PRODUCTNAME Writer, %PRODUCTNAME Calc
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5. Press the [ HELP CALC ] key to access the quick- key help menu
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7. If calc exists, you can also use realpath() to retrieve an absolute path.
8. Building Site by Bargepole From the LP Sodbuster on Ediesta Records 1988 CALC LP 41
9. You can open the file in a spreadsheet program such as Microsoft Excel or OpenOffice Calc.
10. Pre- to Early Variscan metamorphic rocks and intrusive calc-alkaline rocks are constituting the Odenwald accretionary complex.
11. The dirname(__FILE__) call is necessary in order to convert the calc relative path into an absolute one.
12. These phases probably represent a differentiation sequence from an 'I-type' parent magma of calc-alkalic affinity.
13. The plutons are members of the calc-alcaline granite series, leucogranite type that are relatively alkali rich.
14. Définit les options de Bordures pour les objets sélectionnés dans Writer ou Calc
15. The calc-alkaline Ladakh Batholith (NW Himalayas) was dated to constrain the timing of continental collision and subsequent deformation
16. Borderliner provides a simple method to draw borders in tables and some text elements in OpenOffice.org Calc and Writer.
17. In addition, important functions and their parameters are described in the Help for the Shared Library %PRODUCTNAME Calc-Add-In-DLL
18. Acetamide Crystallography: Axial Ratios: a:c = 1:1.18006 : Cell Dimensions: a = 11.44, c = 13.5, Z = 18; V = 1,530.09 Den(Calc)= 1.15 : Crystal System:
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20. Austinite Crystallography: Axial Ratios: a:b:c =0.8303:1:0.6561 : Cell Dimensions: a = 7.5092, b = 9.0438, c = 5.9343, Z = 4; V = 403.01 Den(Calc)= 4.31
21. The Contract-Awarded Labor Category (CALC) tool helps federal contracting officers and others find Awarded prices to use in negotiations for labor contracts
22. Aragonite Crystallography: Axial Ratios: a:b:c =0.6223:1:0.7205 : Cell Dimensions: a = 4.959, b = 7.968, c = 5.741, Z = 4; V = 226.85 Den(Calc)= 2.93
23. The rocks in the Batholith belong to the calc-alkaline series and range in composition from granodiorite through quartz diorite (tonalite) to gneissic aplite
24. Mineralization at Zakanaka is characterized by a broad wall rock alteration halo of biotite–amphibole, and zoned quartz–calc silicate veins proximal to ore.
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26. Cummingtonite Crystallography: Axial Ratios: a:b:c =0.5229:1:0.292 : Cell Dimensions: a = 9.534, b = 18.231, c = 5.3235, Z = 2; beta = 101.97° V = 905.18 Den(Calc)= 2.86
27. Cryolite Crystallography: Axial Ratios: a:b:c =0.9642:1:1.3892 : Cell Dimensions: a = 5.4, b = 5.6, c = 7.78, Z = 2; beta = 90.183° V = 235.27 Den(Calc)= 2.96
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29. Augite Crystallography: Axial Ratios: a:b:c =1.0888:1:0.5833 : Cell Dimensions: a = 9.8, b = 9, c = 5.25, Z = 4; beta = 105° V = 447.27 Den(Calc)= 3.51
30. Major- and trace-element data suggest that least-altered volcanic rocks are of tholeiitic affinity and that there is no calc-alkaline unit in the HCF area.
31. Azurite Crystallography: Axial Ratios: a:b:c =0.8569:1:1.7686 : Cell Dimensions: a = 5.008, b = 5.844, c = 10.336, Z = 2; beta = 92.333° V = 302.25 Den(Calc)= 3.79
32. An offline version is available to Bc Connect ® or registered Bc Calc ® users with limited or no internet connectivity and can be downloaded once users have
33. Late-hercynian granodiorites in the eastern Serre are calc-alkaline and peraluminous in composition; actinolitic-hornblende typically occurs in the mafic types, whereas muscovite occurs in the felsic ones.
34. This, coupled with the occurrence of calc-alkalic volcanics at Glenrock and MORB and alkalic metabasites further southeast argues for variable loci of magma production and source region inhomogeneity along the fore-arc.
35. Chondrite-normalized REE plots show relatively flat patterns, with only slight LREE enrichment for tholeiitic compositions and greater LREE enrichment and lower heavy-rare-earth-element (HREE) abundance for calc-alkalic compositions.
36. Among these granitoids, the most important chemical difference is between calc-alkalic differentiated granitoids to the west and alkalicalcic more evolved granites to the east of an intraorogenic “suture” (the Mylonite Zone).
37. The Central Volcanic Complex which is host to the ores is a high-K calc-alkaline andesite-dacite-rhyolite suite which has erupted through thick continental crust along an ancient continental margin.
38. An effective discrimination between the calc-alkaline and tholeiitic affinities is obtained using the Zr/Y and Ti/Zr ratios, which are, respectively, less than 4 and greater than 70 in andesites of the tholeiitic units.
39. Bc Calc ® sizing software is a web-based application available at www.Bccalc.com It is compatible with Windows or Apple operating systems via Internet Explorer, Edge, Chrome and Safari browsers in addition to iOS and Android tablets
40. The principal copper deposits associated with Upper Creataceous — Laramian calc-alkaline volcano-plutonic complexes in the Bor district are classified as follows: Volcanogenic massive sulphide deposits are situated in andesitic volcanics, and are composed of pyrite and copper sulphides.
41. The accumulation of plagioclase phenocrysts suggests extensive crystal fractionation of the Knee Lake magmas. The gradual transition in affinity of the Knee Lake lavas from tholeiitic to calc-alkaline can be explained by near-surface fractionation under constant fO2 conditions.
42. (An aureole is the zone surrounding an intrusion, which is a mass of igneous rock that solidified between other rocks located within the Earth.) The contact Aureoles produced in siliceous limestones and dolomites, called skarns or calc-silicate rocks, characteristically…
43. Major and trace element chemistry shows that the older series of granitic rocks were formed by differentiation of a calc-alkali magma in situ. The younger dikes are all highly silicic, show limited major element variation, and have been affected by hydrothermal metasomatism.
44. The anorogenic chemistry of the North Bay orthogneiss and mixed calc-alkaline–alkaline chemistry of the Temiscaming gneisses suggest a connection between Paleoproterozoic anorogenic magmatism and synsedimentary quartzite deposition, which is a common association in 1.9–1.6 Ga accretionary orogens of southern Laurentia.
45. Hematite, magnetite, albite, quartz, Ca(Na) amphibole(s), CaNaFe clinopyroxene and andraditic garnet are major constituents of rare calc-silicate iron-formations in the Bimba and Calcsilicate Suites, whereas magnetite, quartz, almandine-spessartine, manganoan fayalite, manganoan grunerite and apatite form manganiferous iron-formations in the Pelite Suite.
46. The Pickle Crow assemblage consists of tholeiitic basalt with thin, but laterally extensive, oxide-facies iron formation overlain by alkalic basalts and minor calc-alkaline andesites to dacites with primitive Nd isotopic compositions (εNd2.89 Ga = +2.1 to +2.4) suggestive of deposition in a sediment-starved oceanic basin.
47. Bartsia alpina is a native herb of moist basic soils in upland meadows and pastures, on unstable flushed slopes resulting from stream erosion, in hummocky calcareous marshes grazed by cattle and sheep in northern England (Pigott 1956), and on ungrazed periodically inundated ledges of calc-schist crags in
48. Pre-accretionary volcanic and plutonic rocks of arc and ocean-floor tectonic affinities have crystallization ages of 1.906-1.901 and 1.888-1.881 Ga; the earlier period was dominated by juvenile tholeiitic arc basalts and related back-arc-basin basalts, and the younger period by juvenile calc-alkaline volcanic rocks and turbidites.
49. Averagely Perfect American Stout Project Recipe 2: WHOLE LEAF Hop version Targets: 5 Gallons into Fermenter (5.24 gallons including trub prior to xfer to fermenter) Target ABV: 6.5% Target OG: 1.068 Target FG: 1.018 Mash Efficiency: 70% Apparent Attenuation: 73% Mash Temp: 154F Ferment at 66F 54 IBUs (per Tinseth Calc) Grain Bill:
50. The Andalshatten Batholith (322 km 2, >700 km 3) is a predominantly granodioritic high-K, calc-alkaline igneous body that was assembled in the mid-crust across four lithologically distinct nappes within the Helgeland Nappe Complex, central Norway.Extensive vertical and horizontal exposures of metamorphic screens and xenoliths within the Batholith provide an unparalleled view of the nature of