| | Book (edition) | photograph their specimens for this book. Front co,·er photos: Turquoise, polished. 55 mm, ZhiJandy...Capillitas, Argentina, H Back cO\·erphoto: Wolframite. 45 mm. Yaogangxian, China, H Page 1: MuscO\ite. 45...Linopolis, Brazil, H Page 13: Gold, 35 mm.Eagle's est Mine, California, G Publi!>hed by Grdllit.u.o. Stefanikova43...authors and a stud) of recent literature in the field of mineralogy. Current encyclopedic books mostly...mineral in magmatic rocks, pegmatites, ore veins or other types of ore deposits, including secondary minerals | | | Book | Springfield show ( 1995: 582). Madawaska [Faraday] mine near Bow Lake, Hastings County. Some of the world's...property of, the old Madawaska uranium mine (called the Faraday mine before 1964). The mineral assemblage...Cowgill, 1977). LATINAMERICA BRAZIL Jacupiranga mine, Sao Paulo. Among the crystallized minerals in the...the l 960s (Sinkankas, 1966; Scott Williams Mineral Co. price list, 196_?), and good, sharp, brown-black...Oblast. Alpine-type clefts in the famous Dodo quartz mine commonly contain ilmenite, occurring as lustrous | | | Book | Assessment and Perspective 4. R.T.SHUEY SEMICONDUCTING ORE MINERALS 5. J.S. SUMNER PRINCIPLES OF INDUCED POLARIZATION...formed". E. Sherbon Hi11s in Geology of Australian Ore Deposits, 1953, p. 57. CHAPTER 27 Intracrustal...U 0) a 4J T33 ! >> ■& CO a. 3 r-l ΓΪ km — 2 km si en o u 1 ° X J CO e C C3 c ax 1) a .I... X Γ CO 3 O •-I C X y-, w CU O H co eu o OC co CO .^ en ... lu 4J -H i-H C U C U x: .—ι en CO · en en O Û X C U CO v _. o HJ M < W ^ > 1-4 < ,-J CQ <£ | | | Book | Assessment and Perspective 4. R.T.SHUEY SEMICONDUCTING ORE MINERALS 5. J.S. SUMNER PRINCIPLES OF INDUCED POLARIZATION...formed". E. Sherbon Hills in Geology of Australian Ore Deposits, 1953, p. 57. CHAPTER 27 Intracrustal...U Q J 3 O r-\ 3 _1 at en o u km S .^ c 3 CO ^o > — 2 km _ 1 u >> -1e a xz 1 ° 1 > "c ! ...■u OJ CO CD en CO Cß U en J < M W y ■MEDIUM LEVEL cfl J0...IPLUTONIC] en co 3 porphyritic granite, diorite, granodiorite 1) £ O e c/3 3 u 43 CO < O ea.n |
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