S04.GEOS112.Minerals.ppt

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  Minerals, Plummer Chapter 2 Minerals, Plummer Chapter 2  What is a mineral? What is a mineral?  Silicate minerals Silicate minerals  Gemstones Gemstones March 1, 2004 March 1, 2004 Exams- so far so good! Exams will be returned and Exams- so far so good! Exams will be returned and discussed after all make-ups are completed. discussed after all make-ups are completed.  Test your diamond-buying skills Test your diamond-buying skills

Transcript of S04.GEOS112.Minerals.ppt

  • Minerals, Plummer Chapter 2 What is a mineral? Silicate minerals GemstonesMarch 1, 2004Exams- so far so good! Exams will be returned anddiscussed after all make-ups are completed. Test your diamond-buying skills

  • What is a mineral? The traditional definition Naturally occurring substance Solid InorganicNOTE: many minerals are produced by BOTH inorganic ANDbiological processes (biomineralization). Calcite - shells of marine organismsMagnetite- bacteriaApatite- bones and teeth Has a set of physical properties that are the same for any andall samples of a given mineral.

  • Mineral or Not a MineralHalite, NaCl ?

  • Mineral or Not a MineralLiquid H2O ?Ice, H2O ?

  • Mineral or Not a MineralAmber (C10H16O) ?

  • Mineral or Not a MineralPearls?

  • Crystal Structure is usually the sticking point for mineral/not a mineralCrystallinity- a regularly repeating patternLinear pattern (1-dimensional)

  • 2 dimensional patternMap ViewWhat do I get if I stack this 2-D pattern one on top of the otherfrom the floor up to the ceiling?What do I get if I put several chains side by side on the floor?

  • Plummer et al., Physical Geology 9th edition, McGraw Hill Inc, Fig 2.023-dimensional patternConnect the centers of the blue circles- cubic structure

  • Plummer et al., Physical Geology 9th edition, McGraw Hill Inc, Fig 2.02NaCl - table saltSodium (Na)Chlorine (Cl)NaCl held together by ionic bond, which is easy to break --> cleavageand hardness

  • A (paraphrased) question from Super MillionaireWhat is the most abundant element in the Earths crust?8 elements make up98.6 % of the Earths crust.ElementsymbolOxygenSiliconAluminumIronCalciumSodiumPotassiumMagnesiumOSiAlFeCaNaKMgThe building blocks of minerals

  • Main rock-forming mineral groups Silicates Oxides building block is SiO4 tetrahedron make up the majority of crustal rocks composed on metal + oxygenCarbonates important component of sedimentary rocks building block is CO3 ion

  • SiO44- complex ion A group of ions that is so tightly bound together that they act like a single unit. Building block of silicate minerals 1 silicon ion + 4 oxygen ions arranged in a triangular pyramid Electrical charge of -4

  • Plummer et al., Physical Geology 9th edition, McGraw Hill Inc, Fig 2.07

  • Silicate tetrahedronSiO44-

  • Tetrahedron ViewingView from the top,looking down.Top point oftetrahedronfacing youFlat base of tetrahedronfacing you. Top pointof tetrahedron pointingaway from you.

  • Nesosilicates (island silicates)SiO44- tetrahedron forms ionic bonds with cations such as Mg2+, Fe2+Fe2SiO4 - FayaliteMg2SiO4 - Fosterite(Mg, Fe)SiO4Solid solutionExample: Olivine

  • Olivine: nesosilicate structure (island silicate)Why Mg OR Fe? Same size Same electricalcharge

  • Corner Sharing Base to Baseside view3-D Side View

  • Inosilicicates: Single Chains (Pyroxene)SiO3 Chain forms ionic bonds with cations above the tipand below the base 2 Si6 OPlummer et al., Physical Geology 9th edition, McGraw Hill Inc, Fig 2.11

  • Corner Sharing Tip to TipExtra slide. Not shown in class. Not for exams. For your interest.Face sharing

  • Extra slide. Not shown in class. Not for exams. For your interest.Assembling a Single Chain Silicate (Pyroxene)

  • Extra slide. Not shown in class. Not for exams. For your interest.Pyroxene- Wheres the cleavage?90 cleavage

  • Extra slide. Not shown in class. Not for exams. For your interest.This wont work.No gold, silver, or uraniumfound with pyroxens.

  • Double Chain Silicates (Amphibole)PAIR of SiO4 chains that link by corner sharing in 2 directions Plummer et al., Physical Geology 9th edition, McGraw Hill Inc, Fig 2.11

  • Plummer et al., Physical Geology 9th edition, McGraw Hill Inc, Fig 2.11Amphibole formula is long: lots of space for smalland medium cationsCations include Na+, K+, Ca2+, Mn2+,Fe2+, Mg2+, Fe3+, Al3+, Ti4+ Extra slide. Not shown in class. Not for exams. For your interest.

  • Extra slide. Not shown in class. Not for exams. For your interest.60-120 Cleavage in Double Chain Silicates (Amphibole)- (actually 56 - 124)breaking at the molecular scaleWhat human eyes seeat the macro scale

  • What is Jade?Both pryoxeneAND amphiboleare Jade.Other JadesAfrican jade: Green garnetAmazon jade: Green K-feldsparIndian jade: Green quartzJadeite = NaAlSi2O6Nephrite = Ca2(Mg,Fe)5Si8O22(OH)2

  • Plummer et al., Physical Geology 9th edition, McGraw Hill Inc, Box 02.03.f1, photo by C.C. PlummerAsbestos- generic name for fibrous amphibole

  • Ring Silicates- BerylStack of SiO4 rings, builtup out of the plane of screen

  • Plummer et al., Physical Geology 9th edition, McGraw Hill Inc, Fig. 2.14Muscovite

  • Clay minerals: talc, kaolinite, illite, chlorite, montmorilloniteYou know them better as: baby powder, kaopectate/non-dairy creamer,facial mask, soapstone, and kitty litter.Main difference- ions that make up the middle of the sandwich

  • Quartz No cleavage. Covalent bondsare equally strong in all directions very roomy structure. Can accommodate large cations.

    Gold, silver always found with quartz Hardness of 7 on Mohs scale,also due to crystal structure. All oxygens are shared

  • Gemstones- beautiful, rare, durableWhat makes a mineral a gem?Fluorite- gem or not a gem?

  • GarnetRubyAmethystAquamarineDiamondEmeraldPearlPeridotSapphireOpalTopazTurquoiseBirthstones- Gem names

  • GarnetCorrundumQuartzBerylDiamondBerylPearlOlivineCorrundumAmorphousquartzAl-F silicateHydrouscopper phosphateBirthstones- The real names!

  • Ruby and Sapphire- forms of Corundum Al2O3Ruby- corundum with chromiumSapphire- corundum with iron and titanium

  • A quick guide to buying diamonds- Color Cut Clarity Carat

  • Gem- rare, beautiful, durableA typical diamond deposit yields ~ 5 grams of diamondper 1000 kg of rock mined.

  • 1. Color- Which one is the most valuable?ColorlessNearcolorlessFaint yellowVery LightyellowLightyellowFancyyellow

  • The Hope DiamondPossibly the re-cut (4 times) Tavernier Blue Diamond,which was reported at 112 carats in the year 1668. 45 carats

  • 2. CutTableCrownMain pavillion

  • Cutting DiamondsMarshak, S. Earth, Portrait of a Planet, W.W. Norton, Fig. 5.26

  • Why are diamonds cut this way?Facets control the pat of light traveling through the diamond.The more light that exits the top (crown), the more it sparkles.Pat of light in a round brilliant diamond

  • Imperfections in the cut

  • 3. ClarityAre there blemishes on the surface, or inclusions insidethe diamond?

  • 4. Carat weight1 carat (ct.) = 200 milligramsBig diamonds are more rare than little diamonds.

    A 2 ct diamond costs more than 2 times a 1 ct. diamond.Note: carat weight NOT THE SAME as gold karats. Gold is made of 24 parts.Karats indicates how many of those 24 parts are gold.14 karat gold = 14 parts gold + 10 parts alloying metal (copper, nickel, silver)18 karat gold = 18 parts gold + 6 parts alloying metal.

  • Is my diamond a fake?!Zirconium Oxide (ZrO2)Cubic ZirconiaSilicon Carbide (SiC)MoissaniteExtra credit for exam 2:How can you tell the difference betweena real diamond and one of these substitutesUsing physical properties?Note- you will not be allowed to leave the room during exam 2 to consult an appraiser.