Optical properties in cleavage flakes of rock-forming minerals. by E. D. Taylor

Cover of: Optical properties in cleavage flakes of rock-forming minerals. | E. D. Taylor

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  • Mineralogy.

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Book details

SeriesUniversité Laval. Faculté des sciences. Géologie et minéralogie. Contribution, no. 78
Classifications
LC ClassificationsQE1 .Q432 no. 78
The Physical Object
Pagination80 p.
Number of Pages80
ID Numbers
Open LibraryOL6073154M
LC Control Number50013089
OCLC/WorldCa1242169

Download Optical properties in cleavage flakes of rock-forming minerals.

Additional Physical Format: Online version: Taylor, E.D. Optical properties in cleavage flakes of rock-forming minerals.

Québec, (OCoLC) Optical and physical properties. The optical properties of micas cover a wide range but all have negative optic sign, low 2V, and have the α optic direction approximately perpendicular to their perfect cleavage.

Birefringence is generally very weak in the plane of cleavage flakes. In this edition of Introduction to the Rock-Forming Minerals, most of the commonly occurring minerals of igneous, metamorphic and sedimentary rocks are discussed in terms of structure, chemistry, optical and other physical properties, distinguishing features and paragenesis.

Introduction to Optical Mineralogy. Fourth Edition. William Nesse. Publication Date - March ISBN: pages Paperback /2 x /4 inches In Stock. Retail Price to Students: $ Comprehensive coverage of the optical properties of over rock-forming minerals and a selection of common ore minerals.

Glauconite, which most often occurs as pelletlike grains, has no apparent cleavage. The names of the rock-forming micas constitute a good example of the diverse bases used in naming minerals: Biotite was named for a person—Jean-Baptiste Biot, a 19th-century French physicist who studied the optical properties of micas; muscovite was named.

Covering theory and practice, this wide-ranging introductory textbook covers the main optical properties of rock-forming minerals that can be recognized under the polarizing microscope.

The authors elucidate the basic elements of microscopy, the theory of light transmission through translucent minerals, and the properties of light reflected from opaque minerals.5/5(1). The basic structural feature of mica is a composite layer in which a sheet of octahedrally coordinated M cations (mainly Al, Mg, Fe) is sandwiched between two identical and opposing sheets of linked (Si,Al)O 4 tetrahedra.

Two of these tetrahedral sheets, of composition (Si,Al) 4 O 10, are illustrated in Fig. On the left is a sheet in which all tetrahedra are pointing upwards, as may be. Several important optical properties are applicable to minerals and gemstones, and can be very useful for gem identification.

With proper equipment, jewelers can easily distinguish a Ruby from Garnet or red glass, even if their outward appearance may be identical. White Light, or visible light, is a form of electromagnetic radiation (energy waves produced by the motion of an electric charge).

Very old sediments are likely to have comparatively few mineral species. The methods of optical mineralogy serve to identify many of the minerals, herein described, quite readily, but there are other cases where optical tests must be supplemented by specific gravity determination, chemical-tests, dye-tests, flame-tests, fluoroscopy or, in cases.

Identification Tables for Common Minerals in Thin Section These tables provide a concise summary of the properties of a range of common minerals. Within the tables, minerals are arranged by colour so as to flakes with 1 perfect cleavage.

Habit and birefringence distinctive. In al u m in o sg rte+ y ph ck. Enjoy the videos and music you love, upload original content, and share it all with friends, family, and the world on YouTube.

Optical Properties of Common Rock-Forming Minerals J. Lyons, S. Morse, and R. Stoiber Distinguishing Characteristics Chemical XI. System and Indices Birefringence "Characteristically parallel, but Mineral Composition Best Cleavage Sign,2V and Relief and Color see Fig.

High Positive Relief Zircon ZrSiO. Tet. (+) = High. However, many of the rocks are primarily made up of minerals after the decomposition and consolidation along with other organic or inorganic substances. Some of the common rock forming minerals along with their physical and chemical properties are discussed below: 1.

Quartz. It is pure or nearly pure silica and is hard and glassy mineral. Of the many optical properties of minerals, their luster, their ability to transmit light, their Mineral Strength (CLEAVAGE) Some minerals have excellent cleavage in one, two, three, or more directions, Most common rock-forming minerals have a specific gravity of between 2 and 3.

Calcium carbonate forms as both Aragonite and Calcite, and these two minerals only differ in their e, the more common mineral, forms in trigonal crystals, whereas Aragonite forms orthorhombic crystals. On occasion, crystals of Aragonite and Calcite are too small to be individually determined, and it is only possible to distinguish these two minerals with optical or x-ray.

The name "biotite" is used in the field and in entry-level geology courses because these minerals generally cannot be distinguished without optical, chemical, or x-ray analysis. Biotite is a rock-forming mineral found in a wide range of crystalline igneous rocks such as granite.

This chapter deals with the optical properties of those minerals which make up the common rocks of the Earth’s crust, the so-called rock-forming minerals.

A study of these rock-forming minerals entails their examination under the microscope, either as tiny grains or as thin (~ mm) slices of rocks or minerals suitable for examination in. biotite mineralbiotite mineral; biotite mineral; Biotite is the most common mica mineral and also known as black mica, a silicate mineral in the common mica imate chemical formula K (Mg, Fe).

It can be found in massive crystal layers weighing several hundred pounds. Muscovite Mineral; schist_mica; Muscovite is the most common mineral of the mica own family. It is an essential rock-forming mineral present in igneous, metamorphic, and sedimentary rocks. Like other micas it with no trouble cleaves into skinny transparent sheets.

Muscovite sheets have a pearly to vitreous luster on their floor. Geologists identify minerals by their physical properties.

In the field, where geologists may have limited access to advanced technology and powerful machines, they can still identify minerals by testing several physical properties: luster and color, streak, hardness, crystal habit, cleavage and fracture, and some special properties.

Physical properties of minerals Fracture • Absence of cleavage when a mineral is broken Specific Gravity • Weight of a mineral / weight of an equal volume of water Department Environmental, Earth, & Atmospheric Sciences • Average value = Other properties Magnetism Reaction to hydrochloric acid Malleability Double refraction Taste.

Optical Properties of Olivine. We then crossed the polarizers and saw that the mineral was extinct when the cleavage planes were parallel with the cross-hairs: which looks to me to be about 20 degrees.

If we check in an optical mineralogy book, we can confirm our answer-- the book. Study of Optical Properties • In this method of study, the minerals are ground very fine and fixed over glass slides.

They are studied under petrological microscope. Different optical properties are studied under polar microscope. The properties of minerals like, color, relief, cleavage, shape and pleochroism are studied under polarized light. The points on the scale are determined by the hardness of these minerals.

Any mineral in the sequence will be scratched by a harder mineral. Cleavage Cleavage is the tendency in a mineral to break with smooth surfaces in directions which correspond to weakly bonded planes of atoms in. Rock Forming Minerals All the minerals constituting the rocks can be classified into two main types: Essential Minerals: These are the minerals which form more than 50% of the rocks.; Accessory Minerals: These minerals occur in limited quantities as small crystals.; The six minerals olivine, quartz, feldspar, mica, pyroxene and amphibole are the commonest rock-forming minerals and are used as.

Mineralogy is a subject of geology specializing in the scientific study of the chemistry, crystal structure, and physical (including optical) properties of minerals and mineralized ic studies within mineralogy include the processes of mineral origin and formation, classification of minerals, their geographical distribution, as well as their utilization.

General Magnesite Information: Chemical Formula: MgCO3: Composition: Molecular Weight = gm Magnesium % Mg % MgO: Carbon % C % CO 2: Oxygen % O: % % = TOTAL OXIDE. °c Mineral Data Publishing, version Crystal Data: Orthorhombic.

Point Group: 2=m 2=m 2=m: In euhedral or subhedral crystals, typically thick, with striations k elongation, with wedge-shaped terminations, to 17 cm.

Commonly granular or compact massive. Twinning: On fg, fg, fg. Physical Properties: Cleavage: fg, fg. The optical property of a mineral depends on how it interacts with light.

Several important optical properties are applicable to minerals and gemstones from a scientific standpoint. These properties are extremely useful for identifying a mineral. The most important of these properties are listed below Colour Transparency Lustre.

Color, luster, streak, hardness, cleavage, fracture, and crystal form are the most useful physical properties for identifying most minerals. Other properties-such as reaction with acid, magnetism, specific gravity, tenacity, taste, odor, feel, and presence of striations-are helpful in identifying certain minerals.

Positive / negative can only be determined by looking your mineral up (+n>, -nbook). CLEAVAGE (IN PLANE LIGHT)—Identify if the sample has cleavage (regularly spaced straight cracks--see enstatite) or fractures (irregular cracks--see olivine).

Is there a single cleavage or two. Mineralogists use a variety of physical and optical properties to help identify minerals without the help of special equipment. These properties include the mineral’s color, crystal shape, hardness, cleavage (the way a mineral breaks), streak, luster, magnetism, ability to transmit light, and specific gravity.

how to use optical properties to identify common rock-forming minerals in thin-section. It is meant to be straight-forward (e.g., the questions are simple, though the answers may not be!), but there are a lot of them.

Take your time looking them over and refer back to your notes for help. Showing alteration rim. To face page Rock-Forming Minerals 77 As there are many points of resemblance between the two groups, it is desirable to point out the char- acters by which we are enabled to distinguish between them; the most important are: (i) the form, and (2) the cleavage.

The fourth edition of Introduction to Optical Mineralogy has been thoroughly revised and updated to increase reading comprehension and improve the clarity of its illustrations. Author William D.

Nesse continues his detailed discussions of the petrographic microscope, the nature and properties of light, and the behavior of light in isotropic and anisotropic minerals, with detailed coverage of Price: $ Since minerals are the building blocks of rocks, it is important that you learn to identify the most common varieties.

Minerals can be distinguished using various physical and/or chemical characteristics, but, since chemistry cannot be determined readily in the field, geologists use the physical properties of minerals. Physical properties The color of a mineral when it is powdered is called the streak of the mineral 1 talc 2 gypsum 3 calcite 4 fluorite 5 apatite 6 feldspar 7 quartz 8 topaz 9 corundum 10 diamond.

Cleavage Cleavage is the way a mineral breaks. one direction mica two directions feldspar three directions calcite. Fracture Fracture is breakage. Phlogopite is a yellow, greenish, or reddish-brown member of the mica family of is also known as magnesium mica.

Phlogopite is the magnesium endmember of the biotite solid solution series, with the chemical formula KMg 3 AlSi 3 O 10 (F,OH) substitutes for magnesium in variable amounts leading to the more common biotite with higher iron content. Wonesite Crystallography: Axial Ratios: a:b:c = Cell Dimensions: a =b =c =Z = 2; beta = ° V = Den(Calc)= Mineral Property Sheets-- David Hirsch, Western Washington Univ.;This activity consists of a set of 69 mineral sheets to be used as part of a term-length set of labs.

Each sheet has spaces to write physical and optical properties for each mineral as well as a crystal form. Get Price []. Atlas of Minerals in Thin Section Elizabeth Johnson, Juhong Christie Liu, and Mark Peale.

Now that you are familiar with how to use a petrographic microscope and some of the optical characteristics that can be observed for minerals, it is possible to identify minerals under the polarizing light microscope (or at least to eliminate some possibilities).Taylor: Optical Properties in Cleavage Flakes of Rock-forming Minerals (Quebec Univ., Lava] Fac.

Sci., Geol. Mineral. Contr. 78, ); (5) colors in thin section; and (6) miscellaneous properties, such as anomalous colors, mag-netism, solubility. An Index gives the number assigned to each mineral .any of the largest group of mineral compounds, as quartz, beryl, garnet, feldspar, mica, and various kinds of clay, consisting of SiO 2 or SiO 4 groupings and one or more metallic ions, with some forms containing hydrogen.

Silicates constitute well over 90 percent of the rock-forming minerals .

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