Minerals under the microscope

Slides:



Advertisements
Similar presentations
Petrological Microscope
Advertisements

ROCKS under the microscope
Minerals under the microscope
Rock Test 1 Write down details on each rock as seen under PPL and XPL on the worksheets provided for you ; then identify the rock type (igneous/ sedimentary/metamorphic)
Mineral Test 2 Write down details on each mineral as seen under PPL and XPL on the worksheets provided for you; then name the mineral under PPL colour.
Mineral Test 1 Write down details on each mineral as seen under PPL and XPL on the worksheets provided for you; then name the mineral under PPL colour.
Appearance of crystals in microscope Crystal shape – how well defined the crystal shape is –Euhedral – sharp edges, well- defined crystal shape –Anhedral.
OPTICAL PROPERTIES OF ROCK FORMING MINERAL
Practical 1 – Acid Igneous Rocks. Light Minerals: Quartz and Feldspars Most acid igneous rocks are dominated by quartz and feldspar as the main minerals.
Compaction and cementation Melting and solidification Heat and/or pressure metamorphic igneous sedimentary Melting Weathering and erosion Heat and pressure.
Minerals of the Earth’s Crust
Minerals.
Practical Igneous Petrology (for Dummies)
Silicon Tetrahedra by Charina Cameron 4 oxygen atoms 1 silicon atom in the center Forms a 4-sided geometry Each side is like an equilateral triangle Creates.
GEOS 254: INTRODUCTION  Petrological microscopes are used to: (a) identify the minerals present (a) identify the minerals present (b) determine the microstructure.
Content Composition of Earth Crust Minerals Groups Silicates Structures Silicates Minerals Nonsilicate Minerals.
Optical Mineralogy WS 2008/2009. Examinations 1) Mid-term - December normal time (13:30) THEORY TEST 2) Finals - February 10 (probably) PRACTICAL.
Use of the petrographic microscope
Optical Mineralogy WS 2012/2013. The week before last…. l BIAXIAL INDICATRIX l EXTINCTION ANGLES.
WJEC AS Mineral Guide I.G.Kenyon.
Use of the petrographic microscope
Study of Rocks 1) Field outcrop observe relationship between rocks
Clues for the Identification of Those Pesky Rock Forming Minerals (Follow along on p. 62) Colby Geology.
Isotropic vs Anisotropic
Descriptions of Rock Forming Minerals: All the following minerals are made of silica tetrahedrons, either alone or combined with other elements.
Classifications of Igneous Rocks Chapter 2. Classification of Igneous Rocks Method #1 for plotting a point with the components: 70% X, 20% Y, and 10%
Minerals. Minerals: Building blocks of rocks To be considered a mineral, a substance must: be a naturally occurring solid be formed by inorganic processes.
Source of course material Dr. Olaf Medenbach, Ruhr-Universit ä t Bochum Optical microscopy of rock-forming minerals, G. W ö rner, USTC Hefei Compact Course.
Optical Properties of Minerals
EARTH MATERIALS III Rock-forming minerals: silicates Professor Peter Doyle
Rocks are aggregates of minerals. Many are silicate minerals. This granite, an igneous rock, has Quartz, an amphibole called Hornblende, a pink potassium.
Metamorphic Textures.
Ge 101. Introduction to Geology and Geochemistry Lecture 2 Crystal Structure of Minerals.
Ionic radius is related to the valence of the ion - ions that have lost electrons (cations) are smaller than their neutral state, ions that have gained.
Difference Between a Rock and a Mineral
Sheet Silicates Micas Chlorite.
After 7.5 mins, 1 st P wave arrived at New York. EAS 220 Lab 4: Igneous Rocks.
Chapter 10 - B Identification of minerals with the petrographic microscope.
Hosted by Miss Bernal Minerals Key Words/ Types of Rocks Pages 6 and 7 of the ESRT Short Answers
Chapter 9 Minerals Section 1 What is a Mineral? Notes 9-1.
4:55 AM October 24, 2011Sanders Unit 2: Rocks and Minerals 2-5 Igneous Rock Identification.
Isotropic Minerals. fluorite A B CD Fluorite is a fairly common mineral in hydrothermal veins and occurs as an accessory mineral in some granitic rocks.
Optical Properties of Minerals
Optical Mineralogy in a Nutshell Use of the petrographic microscope in three easy lessons Part III © Jane Selverstone, University of New Mexico, 2003 Used.
Optical Mineralogy WS 2008/2009. Theory Exam…. Thursday 18th 13:30 90 minutes Answer 3 questions from 5 Total of 30% of the course.
Sedimentology Grain Mineralogy Reading Assignment: Boggs, Chapter 5
Mineral - A naturally occurring, inorganic, homogeneous solid with a definite chemical composition and an ordered atomic arrangement. naturally occurring.
The Polarizing Light Microscope
Mineral Groups Silicates Carbonates Oxides and Sulfides
Optical Mineralogy in a Nutshell
Quartz (crystal form, concoidal fracture, harder than glass)
AS-A level Geology Mineral Guide
GCSE Geology Mineral Guide Click anywhere on the screen to move on.
Minerals on the AS/A level Data Sheet
Optical properties of uniaxial minerals
Appearance of crystals in microscope
Rocks.
Optical Mineralogy in a Nutshell
It’s Lego Time link.
Feldspars.
Other Biaxial Minerals
Minerals under the microscope
Igneous Rock edition Geology
Pyroxene Amphibole Plagioclase Feldspar Olivine Garnet Quartz Fluorite
(2) Talc, Pyrite, & Muscovite
Thursday, January 5 How would you describe what a mineral is to someone? Why or why not do you think minerals are important?
Ge 11a/101. Introduction to Geology and Geochemistry
Metamorphic Textures.
It’s Lego Time link.
Metamorphic Textures.
Presentation transcript:

Minerals under the microscope

The MINERALS you need to know quartz microcline plagioclase muscovite biotite amphibole pyroxene olivine garnet calcite

Quartz grains in sandstone PPL XPL Quartz grains in sandstone

Plagioclase with repeated twinning PPL XPL Plagioclase with repeated twinning

microcline microcline PPL XPL Microcline grain in centre showing its distinctive cross-hatched twinning

muscovite muscovite PPL XPL PPL XPL Muscovite clear under PPL but with perfect cleavage and bright interference colours

feldspar feldspar biotite biotite PPL : lower view rotated to show pleochroism Biotite pleochroic with one perfect cleavage; strong natural colour masks polarisation colours making look greenish under XPL XPL biotite

amphibole amphibole PPL : lower view showing pleochroism Amphibole pleochroic with 2 cleavages at 60o or 120o distinguishing it from biotite or pyroxene XPL

pyroxene pyroxene enlarged PPL XPL Pyroxene well-formed crystal seen here with 2 cleavages at 90o: brightly coloured under XPL

olivine olivine plagioclase plagioclase PPL Olivine looks like a stained-glass window; bright interference colours and thick black fractures XPL

garnet garnet Garnet rounded crystal, transparent under PPL but goes extinct under XPL PPL XPL

calcite calcite Calcite may show both high and low relief, transparent under PPL with 2 perfect cleavages at 120o. Under XPL it shows pearly shades PPL XPL