Itabirite of Minas Geraes, Brazil

1948 ◽  
Vol 18 (2) ◽  
pp. 86-87
Author(s):  
Stanley A. Tyler

Abstract "The mosaic texture and lack of clastic heavy accessory minerals indicate that the quartzose phase of the itabirite is recrystallized chert rather than clastic quartz." Thus this pre-Cambrian high-grade iron ore is more closely related to similar iron formations in other parts of the world.

1965 ◽  
Vol 21 (3) ◽  
pp. 274-294
Author(s):  
Harvey L. Johnson

All Americans know that much of our coffee comes from Brazil. Most have heard of marvelous Rio de Janeiro, one of the beauty k queens of the earth—a city compressed between ocean and granite hills with dazzling white beaches, mosaic sidewalks, scores of night clubs, merry-making sambas, and a lavish Carnival. Quite a number have read of its awesome new capital Brasília, a fabulous creation of glass and concrete built in the middle of nowhere. Some are aware that it is a vast country, our largest and most powerful Latin American neighbor, with huge natural resources and a mushrooming growth in population: its high-grade iron ore reserves are among the richest in the world; its population is estimated to be 80,000,000, the major portion distributed along the Atlantic seaboard. Brazil, the fourth largest country in the world, occupies approximately one-half of South America, with a surface of 3,287,195 square miles, much of it unexplored, and has borders with all the countries of that continent excepting Ecuador and Chile.


2011 ◽  
Vol 48 (2) ◽  
pp. 205-245 ◽  
Author(s):  
L. M. Heaman ◽  
Ch. O. Böhm ◽  
N. Machado ◽  
T. E. Krogh ◽  
W. Weber ◽  
...  

The Pikwitonei Granulite Domain located at the northwestern margin of the Superior Province is one of the largest Neoarchean high-grade terranes in the world, with well-preserved granulite metamorphic assemblages preserved in a variety of lithologies, including enderbite, opdalite, charnockite, and mafic granulite. U–Pb geochronology has been attempted to unravel the protolith ages and metamorphic history of numerous lithologies at three main localities; Natawahunan Lake, Sipiwesk Lake, and Cauchon Lake. The U–Pb age results indicate that some of the layered enderbite gneisses are Mesoarchean (3.4–3.0 Ga) and the more massive enderbites are Neoarchean. The high-grade metamorphic history of the Pikwitonei Granulite Domain is complex and multistage with at least four episodes of metamorphic zircon growth identified: (1) 2716.1 ± 3.8 Ma, (2) 2694.6 ± 0.6 Ma, (3) 2679.6 ± 0.9 Ma, and (4) 2642.5 ± 0.9 Ma. Metamorphic zircon growth during episodes 2 and 3 are interpreted to be regional in extent, corresponding to M1 amphibolite- and M2 granulite-facies events, respectively, consistent with previous field observations. The youngest metamorphic episode at 2642.5 Ma is only recognized at southern Cauchon Lake, where it coincides with granite melt production and possible development of a major northeast-trending deformation zone. The timing and multistage metamorphic history recorded in the Pikwitonei Granulite Domain is similar to most Superior Province high-grade terranes and marks a fundamental break in Archean crustal evolution worldwide at the termination of prolific global Neoarchean greenstone belt formation.


1982 ◽  
Vol 98 (1) ◽  
pp. 229-231 ◽  
Author(s):  
O. Alaku ◽  
J. Steinbachf

Various species of animals, ranging from ordinary laboratory rats to some high-grade beef and dairy cattle, have been imported from the temperate regions of the world to Nigeria in recent years. Most favoured are Large White pigs and this breed of livestock is proving to have very great potential in the livestock production industry in this part of the tropics. Temperate breeds of livestock when introduced to the tropics are said to decline in their general performance, owing partly to direct effects of high ambient temperatures(Yousef & Johnson, 1965). Some generalized statements have also been made on the adverse effects of tropical climate on growth though very little objective field experimental evidence exists (Williamson & Payne, 1978).


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