PPT-Mineral Systems

amp Gold Exploration Outline of talk Exploration Success 3 examples Relevance to exploration targeting at different scales Phoenix Gold probability analysis test case Current state of play for exploration industry. No 1 EN 27012011 StoMineral Fibre B oard Type 2 14 Insulation board made of mineral wool in accordance with EN 13162 Characteristics Areas of application Exterior As insulation board in EWIS Fixing bondeddowelled Not suitable in plinth area and in Naturally occurring. Inorganic. Solid. Crystalline structure. Specific physical and chemical properties. CRYSTALLINE. (molecular structure). Amethyst. HOW DO MINERALS AND ROCKS DIFFER?. clear Quartz mineral . Mineral Systems Workshop 1-3. rd. July . 2013. Martin . Fairclough. & Simon . van . der. . Wielen. www.dmitre.sa.gov.au. Outline. 2. Changing . Role of the Geological Survey. Mineral Systems and Mineral Potential Mapping Research in GSSA. Lesson 5: How are Minerals Identified?. Opening Activity. O. pen Science textbook to page 276.. Open Science workbook to page 90A to review home learning.. Open Science folder to review vocabulary words and outline for the chapter.. What is a mineral?. Solid. Not. liquid, gas, or plasma. What is a mineral?. Naturally-occurring. Not. man-made. What is a mineral?. Inorganic. Never. alive. What is a mineral?. Fixed chemical composition. Name of mineral. Must choose 1 of the following. Talc-Gypsum-Calcite-Fluorite-Apatite-Feldspar-Quartz-Topaz-Corundum-Diamond.. Your Name. Teacher . Name of Mineral. This Slide: . 2 -3 pictures of your mineral here.. Some examples from Latin America. Steven Webb. World Bank – September 2009. Drawing on case studies by Richard . Auty. (Trinidad), Simon . Cueva. (Ecuador), Alberto Diaz (Mexico), Patricio . Navia. Perth 2–3 July 2013. Declining (. greenfields. ) exploration success. Increasing costs. Australia 80% cover – great opportunity. Exploring under cover challenge. Costs. Know how and Technical risk. GLY 4200 . Fall, 2016. 2. Ionic Substitution - Size. Size: Fe. 2+. ↔ Mg. 2+. ↔ Ni. 2+. . (0.86Å) (0.80Å) (0.77Å) . 3. Ionic Substitution - Charge. GLY 4200 - Lecture 2 –Fall, 2016. 2. Hardness . Hardness may be measured in several ways. Moh’s scale – developed by Austrian mineralogist Friedrich Mohs in 1824. Absolute scales – Brinell, Knoop, Rockwell, Vicker’s. Bellwork. 9-13-16. Get out the video notes to check.. Objectives. Students will be able to identify how the earth is affected by long- term and short- term geological cycles and the influence of man.. A . mineral. is a substance with these characteristics:. Solid. Naturally. Occurring. Inorganic. (never lived, although graphite, diamond, and calcite may be byproducts of organisms). Definite . Chemical Composition. naturally occurring, . inorganic solid . with a specific chemical composition . a definite crystalline structure. Minerals can form from the cooling of magma which is the molten material found beneath Earth’s surface as magma rises closer to the surface the molten compounds no longer move freely and they begin to interact chemically to form minerals. All rocks are made up of 2 or more of these minerals. . Minerals are not rocks!. Silicon and oxygen are the most abundant elements in the crust and in minerals. Oxygen is the most abundant element in minerals.