GEOLOGY AND MINERAL RESOURCES OF PARAGUAY A RECONNAISSANCEBy EDWIN B. ECKELABSTRACTAlthough this report includes the results <strong>of</strong> a 6-month reconnaissanceinvestigation <strong>of</strong> the geology <strong>and</strong> mineral resources <strong>of</strong><strong>Paraguay</strong>, it is essentially a compilation <strong>and</strong> interpretation <strong>of</strong>existing published <strong>and</strong> unpublished information on the subject.The rocks can be divided into five major classes, depending onage <strong>and</strong> mode <strong>of</strong> origin. The oldest are <strong>of</strong> Precambrian age,here subdivided into an older group <strong>of</strong> metamorphic rocks <strong>and</strong>a younger group <strong>of</strong> granitic rocks. They are a part <strong>of</strong> the Brazilianshield <strong>and</strong> underlie the entire country but are exposed atthe surface in only a few places. The second group consists <strong>of</strong>marine sedimentary rocks <strong>and</strong> ranges in age from Cambrian orOrdovician through Early Devonian. It comprises three mappableunits, here called the Itapucumi series, the Caacup6 series<strong>and</strong> the Itacurubi series. The third group, which ranges fromPennsylvanian through Triassic in age, constitutes the Gondwanaor Santa Catarina continental clastic sedimentary rocksknown in a large part <strong>of</strong> South America. This group is divisibleinto three map units the Tubarao series <strong>of</strong> glacial deposits, theIndependencia series, <strong>and</strong> the Misiones s<strong>and</strong>stone, <strong>and</strong>, like themarine beds <strong>of</strong> Paleozoic age, is much thinner in eastern <strong>Paraguay</strong>than it is in parts <strong>of</strong> the Gran Chaco in the western half <strong>of</strong> thecountry. The fourth group is Tertiary to Recent in age <strong>and</strong>consists in large part <strong>of</strong> un consolidated clay <strong>and</strong> s<strong>and</strong> <strong>of</strong> continental origin. These materials are very thin in most <strong>of</strong> eastern<strong>Paraguay</strong>, but they cover nearly all <strong>of</strong> the Gran Chaco to depthsas great as 2,000 feet.The fifth large group <strong>of</strong> rocks consists <strong>of</strong> igneous extrusive <strong>and</strong>intrusive rocks, mostly <strong>of</strong> basic composition. The most importantsingle member is the Serra Geral basaltic lava, <strong>of</strong> LateTriassic or Jurassic age, which covers the eastern edge <strong>of</strong> thecountry <strong>and</strong> extends far into Brazil. Associated with the SerraGeral lavas are many smaller bodies <strong>of</strong> intrusive diabase, extrusivebasalt, <strong>and</strong> possibly other rocks. There are also manyintrusive <strong>and</strong> extrusive igneous rocks whose age is unknown.Some are strongly alkalic <strong>and</strong> <strong>of</strong> considerable interest petrographically;some may be related in age <strong>and</strong> origin to the SerraGeral lavas, but for others there is strong evidence that they areno older than late Tertiary. Chemical <strong>and</strong> spectrographicanalyses <strong>of</strong> a number <strong>of</strong> samples <strong>of</strong> the igneous rocks are includedin the report.The geologic structure <strong>of</strong> <strong>Paraguay</strong> appears to be relativelysimple in its grosser aspects, but little is known <strong>of</strong> even the largerfeatures. In the eastern half <strong>of</strong> the country the beds dip gentlyeastward toward the great Parana1 basin <strong>of</strong> southeastern Brazil.This easterly dip appears to reverse along the axis <strong>of</strong> a low anticlinethat trends north-south only a few kilometers east <strong>of</strong> theRio <strong>Paraguay</strong> <strong>and</strong> exposes the older sediments <strong>and</strong> the Precambrianbasement rocks at the surface in many places. West <strong>of</strong>this axis the beds either dip steeply westward, or are downfaultedto the west, into the depths <strong>of</strong> the Gran Chaco basin. The rocksin this basin are, in places, at least 10,000 feet deeper than theyare in eastern <strong>Paraguay</strong>; west <strong>of</strong> the basin, in eastern Bolivia,they rise to the surface in a series <strong>of</strong> anticlines <strong>and</strong> synclines thatform the foothills <strong>of</strong> the Andes.<strong>Paraguay</strong> possesses large quantities <strong>of</strong> certain nonmetallicmineral resources, notably clays for brick, tile, <strong>and</strong> pottery,limestone <strong>and</strong> other raw materials for portl<strong>and</strong> cement <strong>and</strong> forlime; common <strong>and</strong> ornamental building stones; glass s<strong>and</strong>; talc;<strong>and</strong> mineral pigments. Except for iron ore, <strong>of</strong> which there aremany small but rich deposits, <strong>Paraguay</strong> appears to be poorlyendowed in most other mineral resources. It has a little manganese,copper, mica, <strong>and</strong> beryl <strong>and</strong> there are good geologicreasons for hoping that worthwhile deposits <strong>of</strong> salt, gypsum, <strong>and</strong>bauxite may yet be discovered.Aside from wood, <strong>and</strong> water power that is both remote <strong>and</strong>undeveloped, the only known source <strong>of</strong> fuel or energy lies insome little-known peat deposits near Pilar. Petroleum mayexist in the Gran Chaco basin, but pro<strong>of</strong> <strong>of</strong> its presence mustawait a willingness on the part <strong>of</strong> <strong>Paraguay</strong>an or other investorsto risk much more money than has already been spent in oneexploratory campaign.Besides the available facts on all <strong>of</strong> the country's known <strong>and</strong>reported mineral resources, a number <strong>of</strong> suggestions are givenfor establishing local industries that could provide mineralproducts for local use <strong>and</strong> conserve some <strong>of</strong> <strong>Paraguay</strong>'s foreignexchange. By all odds the most valuable <strong>and</strong> promising <strong>of</strong><strong>Paraguay</strong>'s mineral resources are the water resources, bothsurface <strong>and</strong> underground, <strong>and</strong> the soils.INTRODUCTIONPRESENT INVESTIGATIONThe investigation recorded here was a part <strong>of</strong> theUnited States' Point Four program <strong>of</strong> giving technicalaid to underdeveloped countries. The author wasassigned by the U. S. Geological Survey to act asgeologic technical advisor to the Government <strong>of</strong> <strong>Paraguay</strong>under the auspices <strong>of</strong> the Institute <strong>of</strong> Inter-American Affairs. He was in <strong>Paraguay</strong> from February25 through August 6, 1952. In addition to the workwhose results are recorded here, his duties includedadvice on the establishment <strong>and</strong> maintenance <strong>of</strong> aDepartment <strong>of</strong> <strong>Geology</strong> arid Mines, as well as therelated problems <strong>of</strong> staffing <strong>and</strong> training geologists <strong>and</strong>engineers for such a Department. These latter dutieswere discharged by means <strong>of</strong> <strong>of</strong>ficial written <strong>and</strong> oralcommunications to the Government <strong>of</strong> <strong>Paraguay</strong>.This report contains a base map <strong>and</strong> a geologic mapthat are as complete as can be expected from the factsnow available. The chief contributions <strong>of</strong> this report
GEOLOGY AND MINERAL RESOURCES OF PARAGUAYare that it assembles in one place most <strong>of</strong> the hithertowidely scattered published information on the geology<strong>of</strong> <strong>Paraguay</strong>; it contains a considerable amount <strong>of</strong>hitherto unpublished information collected from varioussources; it presents new facts, based on modernpetrographic <strong>and</strong> chemical methods, on a few <strong>of</strong> theigneous rocks; <strong>and</strong> it contains an objective summary<strong>of</strong> the country's mineral resources <strong>and</strong> its potentialitiesas a mineral producer. This summary is not as optimisticas many would hope, but it does point out afew real possibilities <strong>and</strong> narrows the areas that mostdeserve further study.The report is, then, a compilation <strong>and</strong> interpretation<strong>of</strong> existing information on the geology <strong>and</strong> mineralresources <strong>of</strong> <strong>Paraguay</strong> based on a 6-month reconnaissancestudy, but if it were confined to recording personalobservations during that period it would be a"thin" report indeed. Travel conditions in <strong>Paraguay</strong>are difficult at best, <strong>and</strong> were made somewhat more soby greater than average rainfall during the winter <strong>of</strong>1952. These <strong>and</strong> other tangible <strong>and</strong> intangible factorspermitted field work for considerably less than halfthe total time available for the project. The author'spersonal observations were limited to a comparativelysmall part <strong>of</strong> central <strong>Paraguay</strong>, plus spot studies atthe termini <strong>of</strong> a few airplane trips; these flights permittedexcellent aerial views <strong>of</strong> representative crosssections <strong>of</strong> the country. These personal observationswere greatly supplemented by the use <strong>of</strong> aerial photographs,by the study <strong>of</strong> specimens in various museums<strong>and</strong> private collections, <strong>and</strong> by data supplied by severalgeologists <strong>and</strong> others who had observed <strong>and</strong> recordedthe geology at particular spots.The facts gathered would, by themselves, have beenbeen utterly insufficient as a basis for a report <strong>of</strong> thescope attempted here. Personal observations, supportedby studies <strong>of</strong> the small collections <strong>of</strong> rocks <strong>and</strong>fossils have, however, given a clearer underst<strong>and</strong>ing<strong>of</strong> the existing literature en the subject. They havealso given a modicum <strong>of</strong> confidence in this attempt togather published information on the geology <strong>of</strong> <strong>Paraguay</strong><strong>and</strong> to integrate it with facts observed by workersin neighboring countries, where geologic knowledge ismore advanced than in <strong>Paraguay</strong>.Throughout this report an effort has been made todistinguish between fact <strong>and</strong> fancy as well as betweenthe author's own contributions <strong>and</strong> those <strong>of</strong> others.Since facts that are absorbed by the mind, regardless<strong>of</strong> their source, have a tendency to emerge as newdiscoveries, these efforts have doubtless been onlypartially successful. The reader would, therefore, dowell to remember that the present author is a compiler<strong>of</strong> scattered information, rather than a recorder <strong>of</strong>his own observations. Naturally, he must bear responsibilityfor all the interpretations, good or bad, thathave been drawn from the basic data.PREVIOUS GEOLOGIC INVESTIGATIONSA considerable body <strong>of</strong> knowledge on the geology <strong>and</strong>mineral resources <strong>of</strong> <strong>Paraguay</strong> has been accumulatedthrough the years. Most <strong>of</strong> this information, however,is widely scattered through the world literature <strong>of</strong>geology, where it appears in several languages, orexists only in unpublished files or in the memories <strong>of</strong>individuals who have made observations <strong>of</strong> particularspots or restricted areas. It should be remembered,too, that until 1938 more than half <strong>of</strong> the Gran Chacobelonged to Bolivia, hence descriptions <strong>of</strong> this areain the older literature are referenced under the name<strong>of</strong> that country. The pertinent literature that hasbeen found is listed in the annotated bibliography,which contains a number <strong>of</strong> items that are not referredto specifically in the text. Such items haveserved a purpose by providing needed background forother facts <strong>and</strong> all will be <strong>of</strong> interest to future seriousstudents <strong>of</strong> the subject.The most complete descriptions <strong>of</strong> the geology <strong>of</strong><strong>Paraguay</strong> that have appeared in print are the recentpapers by Harrington (1950, 1956). Unfortunately,his work is limited to the eastern part <strong>of</strong> the country<strong>and</strong> is based on only a few weeks fieldwork. Even withthese limitations, he was able to present a clear <strong>and</strong>accurate picture <strong>of</strong> the stratigraphy <strong>and</strong> geologic history,one on which the present author has leaned veryheavily in preparing this compilation. The only othercomprehensive study <strong>of</strong> the geology known to theauthor is that made by the Union Oil Company duringits exploration for petroleum in 1944-49. In additionto the drilling <strong>of</strong> five deep wells, this company is understoodto have done reconnaissance geologic mapping <strong>of</strong>the entire country, plus a very large amount <strong>of</strong> geophysicalexplorations in the Gran Chaco. Of theinformation accumulated, only the records <strong>of</strong> the deepwells <strong>and</strong> fossil identifications made by Dr. Horacio J.Harrington are available for publication.Among the older descriptions <strong>of</strong> the geology <strong>of</strong> eastern<strong>Paraguay</strong>, those <strong>of</strong> Carnier (1911, 1913), supplementedby Goldschlag's (1913) chemical <strong>and</strong> petrographicdescriptions <strong>of</strong> Carnier's rocks, are by far the mostuseful; much dependence has been placed on themhere <strong>and</strong> in the compilation <strong>of</strong> plate 1. Kanter (1936)gives the most complete description extant <strong>of</strong> the geology<strong>of</strong> the Gran Chaco region. DeMersay (1860) <strong>and</strong>DuGraty (1865) give far more complete accounts <strong>of</strong>the country's mineral resources than any more modernworkers <strong>and</strong> both give, in addition, many notes on thegeology. M. S. Bertoni (1921), A. deW. Bertoni (1939),G. T. Bertoni (1940), Conradi (1935), <strong>and</strong> Boettne