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Geology and Mineral Resources of Paraguay A Reconnaissance

Geology and Mineral Resources of Paraguay A Reconnaissance

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24 GEOLOGY AND MINERAL RESOURCES OF PARAGUAYFIGURE 17. Black porphyry (specimen P-32) from dike parallel to the Del Puerto vein near Caapucu shows <strong>and</strong>esinic phenocrysts, /, in finely crystallinematrix, a rather coarsely crystalline cognate xenolitli, c-x, not discernible in the h<strong>and</strong> specimen, <strong>and</strong> quartz (q). X 20. Crossed nicols.In the norm symbols (Washington (1917)), thefollowing significance attaches to the four parts <strong>of</strong>the symbol.The initial Roman numerals termed the "class" indicatesthe relation <strong>of</strong> salic to femic minerals, that is,TABLE 2. Spectrographic analyses <strong>of</strong> Precambrian rocks <strong>of</strong><strong>Paraguay</strong>[Analyst: Paul R. Barnett, TJ. S. Geological Survey. Tr.=trace; concentrationuncertain. Looked for but not found, As, B, Bi, Cd, Ge, In, Pt, Sb, Ta, Th, Tl,U, <strong>and</strong> W]Ag_____Ba_ _Be..___Co._.__Cr_____Cu____.Ga_ _La...__Mo_.__Nb__._Ni._ -.Pb_.___Sc_-._Sn__Sr . ._V......Y.____.Yb____.Zn_____Zr ...P-310. 0001.1.0006.0002.0003.003.002.006.0002.0010 .009.00050.02.002.005.0004.2.02P-34 P-58b P-59 P-600 0 0 0 .05 .1 .07 .2.0007 .0004 .0003 0. 0002i Tr. Tr. .0008. 0004 . 0002 .0001 .0003.0007 .0003 .0002 .0007.002 .002 .001 .001.006 .006 .006 0.0002 .0001 .0003 .0003.001 .001 .001 .0020 . 0004 0 0 .002 .004 .003 .004.001 .0003 .0003 .0010 0 0 0.02 .009 .009 .05.0009 .002 .0004 .004.007 .006 .005 .007.0007 .0004 .0004 .00030 0 0 .03 .01 .040 .01P-62P-75 P-lOla P-lOlb0 0. 00004 0 .004 .02 .1.0007 .0006 .00050 .0005 .0005Tr. .002 .001.0002 .002 .001.003 .004 .00100 00 .002 .0002.003 .01 00 .001 .0008.005 .002 .0030 0 .00040 .0006 0 .0006 .002 .01Tr. .007 .005.007 .02 .004.0008 .002 .00040 0 0 0.01 .03 .08 .01P-740 0 .07 .0020 .0004.0003 0.0001 .0001.0003 .0002.001 .002.005 0.0002 .0003.001 .0020 0 .003 .003.0004 00 0.03 .002.002 Tr..004 .004.0002 .00040 .02NOTE. See following table for description <strong>of</strong> specimen <strong>and</strong> locality <strong>of</strong> collectionnumbers.Field No.P-31 .....P-34___P-58b..._-P-59 __ _P-60__P-62_____.P-74 _____P-75- -P-lOlb. _.RockPorphyry, dark phase ...Rhyolite agglomerate. _ _Rhyolite porphyry ......Porphyry (fine grained) _LocalityCountry rock <strong>of</strong> Del Puerto vein outcropnear Caapucu.Highway quarry near Ypacarai.Acahay caldera.North <strong>of</strong> Caapucu on Quiindy road.Near Caapucu.quartz-|-f el dspars+feldspathoids versus ferromagnesiansilicates-)-oxides + carbonates-]-phosphates, <strong>and</strong> others.There are five classes.The second numeral indicates the order, based ondifferences in the chief subgroup <strong>of</strong> the preponderantsalic or femic group, <strong>and</strong> serves to distinguish thosechemical characters that are dependent on the dominantacid-forming components <strong>of</strong> the magma, silicon, titanium,<strong>and</strong> ferric iron. For rocks not definitely femicin character, there are nine orders.The third numeral indicates the rang, based on theproportions <strong>of</strong> alkalies to lime in the preponderant salicage.age.

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