EMERALD GREEN PDF

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Emerald Green Pdf

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ABSTRACT! The Crabtree pegmatite in the Spruce Pine district of North Carolina is a beryl (emerald, green beryl, aquamarine Beryl (Aquamarine, Emerald. The Emerald Green Clubhouse is open for resident use from 9 AM to 9 PM daily. It is located Download this file (Emerald Green 2 and 3 pdf). TVS Emerald Green Acres Kolapakkam, Chennai. Auric Acres Real Estate offers complete details on TVS Emerald Green Acres at Kolapakkam, Chennai.

Provided t h a t the s u l f a t e and i r o n contents o f the batch are well adjusted, the redox o f the batch and the furnace atmosphere during melting have l i t t l e e f f e c t on the o x i d a t i o n state of the chromium atoms in the f i n a l glass.

This use is continued in the production of glass containers f o r s o f t drinks. A good understanding of the chromium e q u i l i b r i a in glass w i l l in f u l f i l l i n g the requirements of the market. The more stable t r i v a l e n t chromium has two absorption bands at and nm. The o v e r a l l e f f e c t o f these absorption bands is that i t gives the glass a deep emerald green c o l o r.

Hexavalent chromium on the other hand has a very strong absorption band centered a t nm. Much work has been done to determine the factors a f f e c t i n q the chromium e q u i l i b r i u m in glasses. He has concluded t h a t , upto 0. CuO and Co added in glass decreased the dominant wavelength, brightness and p u r i t y.

Istanbul TURKEY A study is made to determine the redox e q u i l i b r i a of chromium ions and the factors a f f e c t i n g these e q u i l i b r i a in a sodalime-silica-glass. The concentrations of i n d i v i d u a l o x i d a t i o n states of chromium are determined by both physical and chemical methods. The results of the two methods are found to be in good agreement.

Provided t h a t the s u l f a t e and i r o n contents o f the batch are well adjusted, the redox o f the batch and the furnace atmosphere during melting have l i t t l e e f f e c t on the o x i d a t i o n state of the chromium atoms in the f i n a l glass. This use is continued in the production of glass containers f o r s o f t drinks.

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A good understanding of the chromium e q u i l i b r i a in glass w i l l in f u l f i l l i n g the requirements of the market. The more stable t r i v a l e n t chromium has two absorption bands at and nm. The o v e r a l l e f f e c t o f these absorption bands is that i t gives the glass a deep emerald green c o l o r. Hexavalent chromium on the other hand has a very strong absorption band centered a t nm. However, it was not all encompassing as large areas of relatively unaltered AMS interfinger with the granofels.

The granofels is in contact with the Crabtree pegmatite along its west side Figure 3.

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Both the granofels and the Figure 7. Schematic diagram of the Crabtree granitic pegmatite in map view. After mining pegmatite were cut by a fault or shear zone.

The evidence for this is indirect and consists of the presence of a excavation, the surface exposure is 5. This rock displays brittlely deformed K-feldspar and quartz no The contact of the pegmatite with the granofels at the western boundary is sharp and cordierite, no chlorite of type found in granofels, little plagioclase, and contains a foliated matrix of aphanitic sericite, chlorite, and epidote.

At this contact, there are two magma-induced, metasomatic alteration assemblages known as exocontacts or selvages.

The chlorite granofels alteration hydothermal alteration that may have also have generated the epidote and converted the cordierite to pinite. The shear zone grades into a biotite selvage inward toward the pegmatite. In addition, three has apparently juxtaposed a portion of the unaltered AMS adjacent to the pegmatite at the mine site giving the impression that the pegmatite body lies in contact with typical AMS rock, specifically biotite-white mica quartz schist mineralogically and texturally distinct biotite-white mica xenoliths are found within the pegmatite Figure 3.

Modified from Tappan and Smith ! Table 3. Microprobe data of representative yellow beryl, Figure 9. Slabbed sample of emerald-bearing Microprobe data in Table 3 illustrates that the beryl associated with green beryl, and emerald in the Crabtree pegmatite.!

Beryl in the Crabtree pegmatite includes emerald, green beryl, the Crabtree pegmatite is sodic according to Cerny Crabtree aquamarine, and yellow beryl Table 1. Emerald and green beryl beryl typically has 0. K2O, CaO and MnO, TiO2 generally occur in the biotite and chlorite selvage and the pegmatite contents are very low and vary between 0 and 0. Total FeO margin, whereas aquamarine and yellow beryl occurs in the pegmatite varies from 0.

The FeO concentrations generally core.

The emerald occurs in various shades from dark to vibrant grass overlap between the emerald, green and yellow beryl but appear to green colors and is generally 0. Na2O concentration is anhedral habits Figure 9. Light green beryl occurs as subhedral to markedly higher in the green beryl over the yellow beryl or the euhedral pale green hexagonal prisms and generally occurs in a matrix emerald and is typically 1.

MgO concentration ranges of quartz and plagioclase. In hand sample, green beryl grading into from 0. Beryl crystals with values of 1.

Euhedral yellow beryl is found in direct Pale, light green beryl contains 0. Emerald to 3 cm in diameter and 10 cm in length. Rare aquamarine occurs as contains the highest Cr2O3 concentration ranging from 0. Throughout a traverse of a single emerald crystal, Cr2O3 is not homogeneous. The chemical compositions of Crabtree emerald are consistent Table 1.

Distribution of tourmaline, beryl, Figure Emerald with those of natural emeralds from other deposits Figure The plagioclase, quartz, and phyllosilicates in the E with quartz Q chemical composition of emeralds appears to be highly dependent Crabtree pegmatite. Q and plagioclase P on host rock compositions, and emeralds from the same occurrence P inclusions.

Note show a wide chemical variation.

The Crabtree emerald shows a inclusions within the well-defined chemical trend with increasing FeO and Cr2O3! Thinner, smaller prisms, up to 0. Throughout the pegmatite body, rounded quartz and plagioclase inclusions Figure Electron tourmaline occurs in local aggregates of thicker prisms up to 5 cm in length, which are brown or black and may be bent or microprobe analysis of one plagioclase inclusion was An9. The quartz fractured. Sunburst tourmaline occurs locally in the pegmatite as well.

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In thin section, margin tourmaline displays highly variable and plagioclase inclusions vary in size from 0. The tourmaline commonly has blue cores with yellow rims, but may exhibit a patchy, occasionally host biotite-phlogopite microlites. Quartz and plagioclase irregular blue zonation.

The larger tourmaline prisms are commonly 5 mm in basal section and 7 mm in length. They are usually inclusions also rarely host tourmaline that may contain biotite inclusions. Both quartz and plagioclase inclusions Green beryl occurs as subhedral to euhedral crystals with biotite and host biotite and white mica, as does emerald. Elongate, irregularly shaped quartz and plagioclase inclusions occur in some white mica inclusions alone and having fewer quartz and plagioclase tourmaline prisms.

Poikiloblastic tourmaline commonly embays the emerald crystals. Smaller tourmalines are 1 to 2 mm basal inclusions than the emerald. Aquamarine is subhedral with minor section and 4 mm in length and contain few to no inclusions.He has concluded t h a t , upto 0.

Location map View in Figure 4 is for the Big Crabtree apparently to the north. Smaller tourmalines are 1 to 2 mm basal inclusions than the emerald. Electron tourmaline occurs in local aggregates of thicker prisms up to 5 cm in length, which are brown or black and may be bent or microprobe analysis of one plagioclase inclusion was An9.

Crabtree emerald mine in The granofels is in contact with the Crabtree pegmatite along its west side Figure 3. After mining pegmatite were cut by a fault or shear zone.

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