Non-metallic Resources: Diamonds Rock cycle and plate boundaries • One or more minerals held together by a matrix Rock types: Igneous • Form from the solidification and crystallization of -magma (molten rock below ground) -lava (molten rock above ground) • Most common examples -Basalt -Granite http://csmres.jmu.edu/geollab/fichter/IgnRx/Introigrx.html 1 Rock types: Igneous • Four types of igneous rocks Mafic minerals Felsic minerals Contain iron and magnesium No iron and magnesium Bowen’s reaction series: arranged by temperature of formation http://csmres.jmu.edu/geollab/fichter/IgnRx/Introigrx.html Rock types: Igneous • Classified by texture and color/composition “slow” = thousands to millions of years “fast” = days to weeks Texture Cooling History Examples Glassy Very fast (hours) cooling; noncrystalline. Obisdian Vesicular Very fast cooling with rapid gas escape forming bubbles in the non-crystalline rock. Pumice, scoria Aphanitic (fine grained) Slow cooling; microscopic crystal growth. Rhyolite, andesite, basalt Phaneritic (coarse grained) Very slow cooling; crystals grow to visible size. Granite, diorite, gabbro Porphyritic (two grain sizes) Two stage cooling; one slow underground creating visible phenocrysts, the second fast at the earth's surface producing a fine grained groundmass. Any aphanitic rock with the word “porphyry” http://csmres.jmu.edu/geollab/fichter/IgnRx/Introigrx.html 2 3 Pegmatite 4 5 Rock types: Igneous rock distribution http://csmres.jmu.edu/geollab/fichter/IgnRx/Introigrx.html Rock types: Igneous rock distribution http://csmres.jmu.edu/geollab/fichter/IgnRx/Introigrx.html 6 Diamond Graphite Composition: Carbon Hardness: Hardest known, 10 Electrically: Insulator Luster: High, dispersion of light Uses: Gemstone, cutting Carbon 1.0 Conductor Dull, metallic Pencils, lubricant Carbon allotropes http://www.chem.ufl.edu/~itl/2041_u01/lectures/lec_h.html Diamond formation: Primary deposits Kimberlite rock - Volatile rich (CO2 & H2O) ultramafic rock - [Rarely] contains xenoliths (solid rocks incorporated into magma) of diamond http://www.diamond-all.com/Diamond.html 7 Diamond formation • Originate in Earth’s mantle, 150 km deep (~90 miles) http://dao.mit.edu/8.231/carbon_phase_diagram.jpg Diamond formation: Primary deposits Diatreme - Explosive volcanic pathway to Earth’s mantle - 50 m high tuff ring - Youngest event ~50 million years ago - 1 in 200 contain diamonds http://www.diamond-all.com/Diamond.html Diamond formation: Primary deposits Kimberlite pipe (Older than 2.5 Byr) Lamproite pipe (Youngest 50,000 years) http://www.brc-diamondcore.com/s/Technical.asp?ReportID=282496 8 Diamond formation: Primary deposits • Kimberley mine -Dug without any machinery, 1871-1908 -460 m diameter by 1100 m deep -3 tons of diamonds were extracted South Africa Diamond formation: Primary deposits • Open pit mine -Used when material is too loose for underground tunnels -Explosives break up layers of “overburden” -Rocks removed and inspected -Overburden replaced or made into a landfill Canada Diamond formation: Primary deposits • Open pit mine Siberia 9 Diamond formation: Primary deposits • Open pit mine South Africa Diamond formation: Primary deposits • Open pit mine Australia (Lamproite pipe, broader cone) Diamond formation: Primary deposits • Open pit mine Canada 10 Diamond formation: Primary deposits • Hydraulic mining -Jets of water loosen gem material -Sluices catch gravel slurry for inspection -Ended in 1960’s Diamond formation: Primary deposits • Strip mining -Similar to open pit mines but done in long strips -Strip one material is removed -Strip two material fills strip one . . . Bucket wheel excavator: moves material 100 m by 25 m deep per day http://apod.nasa.gov/apod/ap061122.html Diamond formation: Primary deposits • Underground mining Diavik open pit mine, Northwest Territories Canada 55 million year old pipe Planned 2012 transition to an underground mine Red: three kimberlite pipes Green/blue: planned mine network http://www.diavik.ca/ENG/ouroperations/1624_underground_mining_equipment.asp 11 Diamond formation: Primary deposits • Underground mining L: Block cave 250 m deep C: Underground entrance R: Haul trucks http://www.argylediamonds.com.au Diamond formation: Primary deposits • Diamond recovery -Millions of tons removed per year -Diamonds represent 1 part per million of host rock! 1,000,000 tons rock = 999,999 tons waste + 1 ton diamonds -Processing: 1. Gravity separation 2. X-ray detection -Waste 1. Piled 2. Covered and sealed “forever” http://www.diavik.ca/ENG/ouroperations/1624_underground_mining_equipment.asp Diamond formation: Secondary deposits • Alluvial (placer) deposits or “artisanal diamond mining” • Weathering of diamond-bearing pipes into water • Simple mining techniques Zimbabwe http://www.galdu.org/web/index.php?odas=5116&giella1=eng 12 Diamond formation: Secondary deposits • International concerns: -no regulatory framework -lack of safety measures -child labor -environmental degradation -prostitution in mining camps -spread of HIV/AIDS Conflict diamonds, or Blood diamonds -“...diamonds that originate from areas controlled by forces or factions opposed to legitimate and internationally recognized governments, and are used to fund military action in opposition to those governments, or in contravention of the decisions of the Security Council”. UN http://www.galdu.org/web/index.php?odas=5116&giella1=eng Diamond formation: Secondary deposits Conflict diamonds, or Blood diamonds • Regulations, 2003 -Kimberley Process Certification Scheme -US Clean Diamond Act • 1% of diamonds sold today are conflict diamonds according to the World Diamond Council http://en.wikipedia.org/wiki/File:Kimberly_Process_Map.svg • International concerns: -no regulatory framework -lack of safety measures -child labor -environmental degradation -prostitution in mining camps -spread of HIV/AIDS Diamond formation: Secondary deposits • Marine deposits http://www.amnh.org/exhibitions/diamonds/marine.html 13 US diamond mines • Murfreesboro, Arkansas discovery in 1906 -1 lamproite pipe -100,000 stones between 1907-1933 • Kelsey Lake, 1996-2002 -8 kimberlite pipes -2 open pit mines http://www.amnh.org/exhibitions/diamonds/marine.html Diamonds and the environment 14
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