31:
1169:
828:
Bahlburg, Heinrich; Vervoort, Jeffrey D.; DeFrane, S. Andrew; Carlotto, Victor; Reimann, Cornelia; Cárdenas, José (2011). "The U-Pb and Hf isotope evidence of detrital zircons of the
Ordovician Ollantaytambo Formation, southern Peru, and the Ordovician provenance and paleogeography of southern Peru
261:
a "Famatinian" orogeny exists which is coeval with the classical
Famatinian orogeny found further south. In the time-span from 480 Ma to 435 Ma (Late Cambrian to Silurian) rocks of Cordillera Oriental were deformed and a magmatic arc developed.
910:
680:
Pinotti, L.P.; Coniglio, J.E.; Esparza, A.M.; D'Eramo, F.J.; Llambías, E.J. (2002). "Nearly circular plutons emplaced by stoping at shallow crustal levels, Cerro Aspero batholith, Sierras
Pampeanas de Córdoba, Argentina".
415:
block of
Laurentian origin that was left in Gondwana after the continents went apart. But such views are not unchallenged since Cuyania is alternatively suggested to have drifted across Iapetus Ocean as a
242:
is thought to have been subject to metamorphism that was "time-equivalent" to the
Famatinian orogeny in the early Paleozoic. It can this be considered part of the orogen in a broad sense. To the south in
754:
Chernicoff, Carlos J.; Zappettini, Eduardo O.; Santos, João O.S.; Allchurch, Shelley; McNaughton, Neal J. (2010). "The southern segment of the
Famatinian magmatic arc, La Pampa Province, Argentina".
1031:
Dalla Salda, Luis H.; López de Luchi, Mónica.; Cingolani, Carlos A.; Varela, Ricardo (1998). "Laurentia-Gondwana collision: the origin of the
Famatinian-Appalachian Orogenic Belt (a review)". In
911:"Age Constraints on the Tectonic Evolution and Provenance of the Pie de Palo Complex, Cuyania Composite Terrane, and the Famatinian Orogeny in the Sierra de Pie de Palo, San Juan, Argentina"
1095:
953:
726:; Faundez, Victor; Calderón, Mauricio; Massonne, Hans-Joachim; Willner, Arne P. (2006). "2. Metamorphic and plutonic basement complexes". In Moreno, Teresa; Gibbons, Wes (eds.).
531:
1724:
193:
280:. This basin went from Peru, through Bolivia to northwestern Argentina. The basin collected sediments from the Famatinian orogen and arc and while it did not contain
560:"The geodynamic evolution of the Famatinian orogen from the paleomagnetic record of El Hongo trondhjemite (Early Paleozoic, Sierras Pampeanas de Córdoba, Argentina)"
473:
In other words: what is at present the northern end of the
Famatinian orogen would have been connected with what is currently the southern end of the Taconic orogen.
1088:
1525:
1451:
1055:"Trilobites laurénticos de la Formación La Laja (Cámbrico), Precordillera de San Juan, Argentina: un aporte biogeográfico al modelo alóctono de Precordillera"
1485:
1054:
1671:
1081:
1596:
386:. Supporting this hypothesis is the suggestion that the orogens have "truncated ends" that can be matched and that both share the commonality of having
1644:
1579:
1059:
511:
234:. Only the western part of Sierras Pampeanas bears evidence of the Famatinian orogeny; the eastern parts appear to have been largely unaffected. In
1572:
1473:
873:"Geoquímica de las rocas plutónicas del batolito cambro-ordovícico del Cordón de Lila y de la Sierra de Almeida, Región de Antofagasta, Chile"
1372:
558:
Geuna, Silvana E.; Escostegoy, Leonardo D.; Díaz
Appella, Belena; Pinotti, Lucio; D'Eramo, Fernando; Hollanda, Maria Helena B.M. (2021).
400:, something that is not expected to be unless both orogens had some sort of contact. This is because trilobites are unable to cross deep
42:
about 70 million years before the
Famatinian orogeny. The Famatinian orogeny took place near the right border of the area marked as "
831:
683:
665:
Lira, Raúl; Kirschbaum, Alicia M. (1990). "Geochemical evolution of granites". In Mahlburg Kay, Suzanne; Rapela, Carlos W. (eds.).
564:
432:
movements starting not from Laurentia but from another region of Gondwana. The fact that Precordillera terrane has many trilobite
1941:
302:
in Chile formed in the Cambrian and Ordovician in association with the orogeny. The compositions of the plutonic rocks are
1871:
791:
Chew, David M.; Pedemonte, Giovanni; Corbett, Eoghan (2016). "Proto-Andean evolution of the Eastern Cordillera of Peru".
1785:
1926:
735:
247:, outcrops associated with the orogeny are scarce since most of that region has become blanketed by much more recent
504:"Comparative seismic and petrographic crustal study between the Western and Eastern Sierras Pampeanas region (31ºS)"
1916:
1780:
1515:
1458:
1936:
1931:
1921:
1773:
214:
of central Argentina is not fully understood. These Devonian batholiths are possibly of post-orogenic character.
1010:
610:
Galliski, Miguel Ángel; Márquez-Zavalía, María Florencia; Roda-Robles, Encarnación; von Quadt, Albrecht (2022).
366:
is the "northward" continuation of the Famatinian orogeny. This has been explained by adding that the continent
1409:
872:
1901:
1876:
1317:
1367:
1347:
1327:
1790:
440:
on what paleogeographic and tectonic history conditions are plausible explanations for this biogeography.
239:
1911:
1906:
1896:
1881:
1337:
925:
30:
612:"The Li-Bearing Pegmatites from the Pampean Pegmatite Province, Argentina: Metallogenesis and Resources"
530:
González, Pablo Diego; Sato, Ana María; Basei, Miguel A.S.; Vlach, Silvio R.F.; Llambías, Jorge (2002).
1946:
258:
159:
17:
559:
1886:
1537:
1429:
1414:
533:
Structure, metamorphism and age of the Pampean-Famatinian orogenies in the western Sierra de San Luis
1823:
1384:
1236:
1226:
43:
1891:
396:
at what is today their western side. Further, in the mentioned sediments both orogens host similar
1547:
127:
1270:
1231:
1666:
1520:
437:
208:
1362:
1828:
1763:
1552:
1394:
1322:
1032:
371:
360:
318:. These rocks are remnants of the magmatism along the western rim of the Famatinian orogeny.
1379:
1753:
1399:
1158:
1073:
998:
929:
840:
802:
765:
692:
627:
573:
425:
390:
1818:
8:
1768:
1758:
421:
231:
1002:
933:
844:
806:
769:
696:
631:
577:
1704:
1656:
1639:
1624:
1619:
1216:
1196:
983:
Dalla Salda, Luis H.; Dalziel, Ian W.D.; Cingolani, Carlos A.; Varela, Ricardo (1992).
589:
503:
1404:
941:
723:
704:
1800:
1743:
1694:
1689:
1502:
1148:
989:
984:
945:
793:
756:
731:
593:
429:
311:
295:
269:
244:
227:
119:
1661:
1039:. Vol. 142. Geological Society, London, Special Publications. pp. 219–234.
291:
1833:
1808:
1719:
1557:
1389:
1221:
1206:
1191:
1183:
1168:
1006:
937:
886:
848:
810:
773:
700:
645:
635:
581:
341:
beneath Gondwana. As subduction went on, the peak of the orogeny resulted from the
299:
204:
75:
1567:
1480:
1463:
1332:
1813:
1714:
1651:
1629:
1510:
1295:
1255:
1201:
1123:
1118:
1110:
852:
585:
363:
342:
131:
1586:
1312:
1699:
1614:
1562:
1424:
1260:
877:
417:
387:
273:
197:
189:
87:
51:
1855:
1865:
1357:
1342:
1307:
1275:
1211:
1138:
949:
891:
814:
777:
669:. Geological Society of America Special Paper. Vol. 241. pp. 67–76.
456:
All coordinates in this article are in relation to present-day geography and
401:
383:
378:(at what is today western South America) in early Paleozoic times due to the
335:
287:
281:
115:
91:
1419:
1352:
1153:
609:
379:
315:
307:
303:
235:
175:
171:
155:
147:
123:
1591:
1532:
1492:
1285:
1280:
1143:
1133:
1128:
397:
338:
266:
1709:
1030:
640:
611:
1542:
1468:
1299:
1265:
1247:
650:
436:
in common with Laurentia but many species are endemic have led to some
412:
331:
277:
248:
196:
formed during the orogeny. These dykes are thought to be derived from
1734:
367:
327:
211:
186:
139:
95:
39:
985:"Did the Taconic Appalachians continue into southern South America?"
502:
Alvarado, Patricia; Castro de Machuca, Brígida; Beck, Susan (2005).
753:
393:
375:
251:
223:
167:
135:
111:
107:
63:
35:
909:
Vujovich, Graciela I.; van Staal, Cees R.; Davis, William (2004).
557:
982:
679:
461:
408:
405:
349:
346:
179:
151:
83:
55:
47:
1443:
1179:
827:
433:
353:
163:
59:
265:
Towards what is now the east of the Famatinian magmatic arc a
501:
143:
1103:
722:
1439:
1011:
10.1130/0091-7613(1992)020<1059:DTTACI>2.3.CO;2
623:
424:
then to Gondwana. Further a third model claims Cuyania is
908:
529:
1858:, note Cuyania's (red) trajectory from 0:20 onwards.
790:
749:
747:
866:
864:
862:
497:
495:
493:
491:
489:
118:, with orogenic activity peaking about 490 to 460
744:
1863:
1048:
1046:
870:
859:
924:(4). Facultad de Ciencias Exactas y Naturales,
730:. Geological Society of London. pp. 5–19.
718:
716:
714:
486:
664:
1089:
1043:
1060:Revista de la Asociación Geológica Argentina
978:
976:
974:
711:
512:Revista de la Asociación Geológica Argentina
178:. The youngest igneous rocks of the arc are
673:
658:
90:and that took place in what is now western
27:Paleozoic geological event in South America
1096:
1082:
605:
603:
1052:
971:
890:
649:
639:
321:
217:
203:The relationship of the orogeny with the
106:. The Famatinian orogeny lasted from the
1104:Major South American geological features
832:Journal of South American Earth Sciences
684:Journal of South American Earth Sciences
565:Journal of South American Earth Sciences
29:
904:
902:
600:
539:. Actas XV Congreso Geológico Argentino
460:to the past disposition of continents,
14:
1864:
467:
359:It has been suggested that the coeval
158:of the Famatinian magmatic arc are of
1077:
450:
899:
428:and arrived at its current place by
1037:The Proto-Andean Margin of Gondwana
667:Plutonism from Antarctica to Alaska
24:
1856:Animation of world plate tectonics
1167:
98:, leading to the formation of the
34:Paleogeographic reconstruction of
25:
1958:
1849:
1024:
871:Niemeyer Rubilar, Hans (2020).
821:
784:
551:
523:
13:
1:
942:10.1016/s1342-937x(05)71083-2
705:10.1016/S0895-9811(02)00033-0
480:
404:. According to this view the
222:The Famatinian orogen's main
853:10.1016/j.jsames.2011.07.002
586:10.1016/j.jsames.2020.103059
7:
1942:Carboniferous South America
1053:Bordonaro, Osvaldo (2016).
926:Universidad de Buenos Aires
10:
1963:
1872:Orogenies of South America
1725:Pampean Pegmatite Province
420:starting in Laurentia and
398:Olenellid trilobite faunas
194:Pampean Pegmatite Province
1799:
1742:
1733:
1682:
1607:
1501:
1438:
1294:
1245:
1197:Arequipa-Antofalla Craton
1178:
1165:
1109:
438:differing interpretations
240:Belén Metamorphic Complex
1927:Ordovician South America
1683:Metallogenetic provinces
1207:Central Brazilian Shield
892:10.5027/andgeoV47n3-3305
815:10.1016/j.gr.2016.03.016
778:10.1016/j.gr.2009.10.008
443:
1917:Carboniferous orogenies
1318:Bucaramanga-Santa Marta
1035:; Rapela, C.W. (eds.).
829:and northern Bolivia".
284:it was a marine basin.
150:that formed a chain of
122:. The orogeny involved
1937:Devonian South America
1932:Silurian South America
1922:Cambrian South America
1246:Structures undergoing
1227:Río de la Plata Craton
1172:
322:Plate tectonic setting
232:northwestern Argentina
218:Outcrops and sediments
162:character and include
79:
67:
1171:
198:S-type granitic melts
33:
1902:Ordovician orogenies
1877:Geology of Argentina
1271:Juan Fernández Ridge
1232:São Francisco Craton
959:on 26 September 2015
80:Orogenia de Famatina
1791:Paraná and Etendeka
1003:1992Geo....20.1059D
934:2004GondR...7.1041V
845:2011JSAES..32..196B
807:2016GondR..35...59C
770:2010GondR..17..662C
697:2002JSAES..15..251P
641:10.3390/min12070841
632:2022Mine...12..841G
578:2021JSAES.10603059G
356:in the Ordovician.
259:Cordillera Oriental
146:along a Famatinian
116:Early Carboniferous
1912:Devonian orogenies
1907:Silurian orogenies
1897:Cambrian orogenies
1882:Geology of Bolivia
1745:Volcanic provinces
1705:El Indio Gold Belt
1503:Sedimentary basins
1368:Magallanes-Fagnano
1217:Paranapanema Block
1173:
426:para-autochthonous
330:was caused by the
102:also known as the
86:that predates the
72:Famatinian orogeny
68:
1947:Sierras Pampeanas
1846:
1845:
1842:
1841:
1695:Chilean Iron Belt
1690:Bolivian Tin Belt
1548:Eastern Venezuela
1338:Dolores-Guayaquil
1328:Cordillera Blanca
997:(12): 1059–1062.
918:Gondwana Research
794:Gondwana Research
757:Gondwana Research
430:strike-slip fault
296:Sierra de Almeida
272:developed into a
270:sedimentary basin
245:La Pampa Province
228:Sierras Pampeanas
120:million years ago
114:and possibly the
100:Famatinian orogen
88:rise of the Andes
16:(Redirected from
1954:
1887:Geology of Chile
1786:Central Atlantic
1746:
1740:
1739:
1720:Lithium Triangle
1674:
1647:
1599:
1582:
1575:
1528:
1488:
1476:
1454:
1375:
1237:Uruguayan Shield
1192:Amazonian Craton
1098:
1091:
1084:
1075:
1074:
1069:
1068:
1050:
1041:
1040:
1028:
1022:
1021:
1019:
1017:
980:
969:
968:
966:
964:
958:
952:. Archived from
915:
906:
897:
896:
894:
868:
857:
856:
825:
819:
818:
788:
782:
781:
751:
742:
741:
728:Geology of Chile
724:Hervé, Francisco
720:
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607:
598:
597:
555:
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520:
508:
499:
474:
471:
465:
454:
310:that are either
300:Salar de Atacama
290:cropping out in
110:to at least the
21:
1962:
1961:
1957:
1956:
1955:
1953:
1952:
1951:
1892:Geology of Peru
1862:
1861:
1852:
1847:
1838:
1814:Noronha hotspot
1795:
1744:
1729:
1715:Iron Quadrangle
1678:
1672:
1667:Terra Australis
1645:
1603:
1597:
1580:
1573:
1553:Golfo San Jorge
1526:
1521:Andean foreland
1497:
1486:
1474:
1452:
1434:
1430:Trans-Brazilian
1373:
1348:Eastern Frontal
1290:
1256:Antarctic Plate
1241:
1202:Atlantic Shield
1174:
1163:
1111:Tectonic plates
1105:
1102:
1072:
1051:
1044:
1033:Pankhurst, R.J.
1029:
1025:
1015:
1013:
981:
972:
962:
960:
956:
913:
907:
900:
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860:
826:
822:
789:
785:
752:
745:
738:
721:
712:
678:
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663:
659:
608:
601:
556:
552:
542:
540:
536:
528:
524:
506:
500:
487:
483:
478:
477:
472:
468:
455:
451:
446:
364:Taconic orogeny
326:Famatinian arc
324:
220:
104:Famatinian belt
52:microcontinents
28:
23:
22:
15:
12:
11:
5:
1960:
1950:
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1939:
1934:
1929:
1924:
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1850:External links
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1824:Juan Fernández
1821:
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1415:Sierra Ballena
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1410:Sarandí del Yí
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1261:Carnegie Ridge
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1234:
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1222:Río Apa Craton
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1159:South American
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1071:
1070:
1063:(in Spanish).
1042:
1023:
970:
898:
885:(3): 628–640.
881:(in Spanish).
878:Andean Geology
858:
839:(3): 196–209.
820:
783:
764:(4): 662–675.
743:
736:
710:
691:(2): 251–265.
672:
657:
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466:
448:
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418:microcontinent
323:
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292:Cordón de Lila
288:Plutonic rocks
274:back-arc basin
236:northern Chile
219:
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26:
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1625:Cariri Velhos
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1600:
1595:
1593:
1590:
1588:
1585:
1583:
1578:
1576:
1571:
1569:
1566:
1564:
1561:
1559:
1556:
1554:
1551:
1549:
1546:
1544:
1541:
1539:
1536:
1534:
1531:
1529:
1524:
1522:
1519:
1517:
1514:
1512:
1509:
1508:
1506:
1504:
1500:
1494:
1491:
1489:
1484:
1482:
1481:Neuquén Rifts
1479:
1477:
1472:
1470:
1467:
1465:
1464:Asunción Rift
1462:
1460:
1457:
1455:
1450:
1449:
1447:
1445:
1441:
1437:
1431:
1428:
1426:
1423:
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1413:
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1408:
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1398:
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1391:
1388:
1386:
1383:
1381:
1378:
1376:
1371:
1369:
1366:
1364:
1363:Liquiñe-Ofqui
1361:
1359:
1356:
1354:
1351:
1349:
1346:
1344:
1341:
1339:
1336:
1334:
1331:
1329:
1326:
1324:
1321:
1319:
1316:
1314:
1311:
1309:
1306:
1305:
1303:
1301:
1297:
1293:
1287:
1284:
1282:
1279:
1277:
1276:Malpelo Ridge
1274:
1272:
1269:
1267:
1264:
1262:
1259:
1257:
1254:
1253:
1251:
1249:
1244:
1238:
1235:
1233:
1230:
1228:
1225:
1223:
1220:
1218:
1215:
1213:
1212:Guiana Shield
1210:
1208:
1205:
1203:
1200:
1198:
1195:
1193:
1190:
1189:
1187:
1185:
1181:
1177:
1170:
1160:
1157:
1155:
1152:
1150:
1147:
1145:
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1137:
1135:
1132:
1130:
1127:
1125:
1122:
1120:
1117:
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1114:
1112:
1108:
1099:
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1087:
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1079:
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1056:
1049:
1047:
1038:
1034:
1027:
1012:
1008:
1004:
1000:
996:
992:
991:
986:
979:
977:
975:
955:
951:
947:
943:
939:
935:
931:
928:: 1041–1056.
927:
923:
919:
912:
905:
903:
893:
888:
884:
880:
879:
874:
867:
865:
863:
854:
850:
846:
842:
838:
834:
833:
824:
816:
812:
808:
804:
800:
796:
795:
787:
779:
775:
771:
767:
763:
759:
758:
750:
748:
739:
737:9781862392199
733:
729:
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719:
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706:
702:
698:
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676:
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652:
647:
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633:
629:
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621:
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613:
606:
604:
595:
591:
587:
583:
579:
575:
571:
567:
566:
561:
554:
535:
534:
526:
519:(4): 787–796.
518:
514:
513:
505:
498:
496:
494:
492:
490:
485:
470:
463:
459:
453:
449:
441:
439:
435:
431:
427:
423:
419:
414:
413:allochthonous
410:
407:
403:
399:
395:
392:
389:
385:
384:Iapetus Ocean
381:
377:
373:
369:
365:
362:
357:
355:
351:
348:
344:
340:
337:
336:Iapetus Ocean
333:
329:
319:
317:
313:
309:
305:
301:
297:
293:
289:
285:
283:
282:oceanic crust
279:
275:
271:
268:
263:
260:
255:
253:
250:
246:
241:
237:
233:
229:
225:
215:
213:
210:
206:
201:
199:
195:
191:
188:
183:
181:
177:
176:trondhjemites
173:
172:granodiorites
169:
165:
161:
160:calc-alkaline
157:
156:igneous rocks
153:
149:
145:
141:
137:
133:
129:
125:
121:
117:
113:
112:Late Devonian
109:
108:Late Cambrian
105:
101:
97:
93:
92:South America
89:
85:
81:
77:
73:
65:
61:
57:
53:
49:
45:
41:
37:
32:
19:
1634:
1064:
1058:
1036:
1026:
1016:18 September
1014:. Retrieved
994:
988:
963:18 September
961:. Retrieved
954:the original
921:
917:
882:
876:
836:
830:
823:
798:
792:
786:
761:
755:
727:
688:
682:
675:
666:
660:
619:
615:
569:
563:
553:
543:18 September
541:. Retrieved
532:
525:
516:
510:
469:
457:
452:
411:would be an
402:ocean basins
358:
325:
316:peraluminous
312:metaluminous
308:monzogranite
304:granodiorite
286:
264:
256:
221:
209:Cerro Aspero
202:
185:Part of the
184:
148:magmatic arc
124:metamorphism
103:
99:
71:
69:
66:are omitted.
1493:Salta Rifts
1459:Amazon Rift
1300:shear zones
1286:Nazca Ridge
1281:Nazca Plate
1149:North Andes
651:10810/57221
464:and oceans.
370:could have
361:Appalachian
339:lithosphere
276:during the
267:Precambrian
128:deformation
94:during the
1866:Categories
1657:San Rafael
1640:Gondwanide
1635:Famatinian
1620:Brasiliano
1558:Magallanes
1390:Pernambuco
1323:Cochabamba
1266:Chile Rise
1248:subduction
572:: 103059.
481:References
332:subduction
278:Ordovician
257:In Peru's
249:Quaternary
212:batholiths
18:Famatinian
1829:San Felix
1819:Galápagos
1809:Ascension
1781:Caribbean
1735:Volcanism
1673:Tilcarian
1608:Orogenies
1511:Altiplano
1487:Paramirim
1469:Cuyo Rift
1405:San Ramón
1385:Oca-Ancón
1124:Caribbean
1119:Antarctic
950:1342-937X
801:: 59–78.
594:229455476
422:accreting
394:sediments
388:carbonate
368:Laurentia
343:collision
328:magmatism
298:south of
252:sediments
187:pegmatite
168:tonalites
152:volcanoes
140:intrusion
96:Paleozoic
44:Río Plata
40:Laurentia
1834:Trindade
1801:Hotspots
1710:El Mutún
1598:Solimões
1574:Pantanal
1563:Malvinas
1538:Colorado
1425:El Tigre
1395:El Pilar
616:Minerals
462:terranes
391:platform
376:Gondwana
372:collided
224:outcrops
180:granites
136:eruption
134:and the
82:) is an
64:Chilenia
54:such as
48:Terranes
36:Gondwana
1774:Austral
1764:Central
1652:Pampean
1630:Chonide
1581:Paraíba
1568:Neuquén
1453:Aguapeí
1444:grabens
1400:Romeral
1358:Huincul
1343:Domeyko
1333:Córdoba
1308:Atacama
1184:shields
1180:Cratons
1139:Malpelo
999:Bibcode
990:Geology
930:Bibcode
841:Bibcode
803:Bibcode
766:Bibcode
693:Bibcode
628:Bibcode
626:: 841.
574:Bibcode
409:terrane
406:Cuyania
382:of the
380:closure
350:terrane
347:Cuyania
345:of the
226:lie in
192:of the
164:gabbros
130:in the
84:orogeny
76:Spanish
56:Cuyania
1754:Andean
1662:Sunsás
1615:Andean
1587:Paraná
1516:Amazon
1475:Espino
1420:Sobral
1353:Gastre
1313:Boconó
1296:Faults
1154:Scotia
948:
734:
592:
434:genera
354:Pampia
205:Achala
154:. The
60:Pampia
1769:South
1759:North
1646:Juruá
1592:Salta
1533:Chaco
1440:Rifts
1380:Morón
1144:Nazca
1134:Coiba
1129:Cocos
957:(PDF)
914:(PDF)
622:(7).
590:S2CID
537:(PDF)
507:(PDF)
444:Notes
374:with
352:with
190:dykes
144:magma
132:crust
1543:Cuyo
1442:and
1374:Meta
1298:and
1182:and
1067:(4).
1018:2015
965:2015
946:ISSN
732:ISBN
624:MDPI
545:2015
306:and
294:and
238:the
207:and
174:and
138:and
126:and
70:The
62:and
50:and
38:and
1007:doi
938:doi
887:doi
849:doi
811:doi
774:doi
701:doi
646:hdl
636:doi
582:doi
570:106
458:not
334:of
314:or
230:in
142:of
46:".
1868::
1065:73
1057:.
1045:^
1005:.
995:20
993:.
987:.
973:^
944:.
936:.
920:.
916:.
901:^
883:47
875:.
861:^
847:.
837:32
835:.
809:.
799:35
797:.
772:.
762:17
760:.
746:^
713:^
699:.
689:15
687:.
644:.
634:.
620:12
618:.
614:.
602:^
588:.
580:.
568:.
562:.
517:60
515:.
509:.
488:^
254:.
200:.
182:.
170:,
166:,
78::
58:,
1097:e
1090:t
1083:v
1020:.
1009::
1001::
967:.
940::
932::
922:7
895:.
889::
855:.
851::
843::
817:.
813::
805::
780:.
776::
768::
740:.
707:.
703::
695::
654:.
648::
638::
630::
596:.
584::
576::
547:.
74:(
20:)
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