91:. These domes in clockwise direction are known as Cerro Lucho, Cerro Lucha, Cerro Agua Dulce and Cerro Pairique Chico and rise 50–700 metres (160–2,300 ft) above the Bajo de Pairique, the centre of the 8 kilometres (5.0 mi) wide semicircle. Most of these domes have been affected by lateral or centre-ward
538:
Franco, M. Gabriela; Peralta Arnold, Yesica J.; Santamans, Carla D.; LĂłpez
Steinmetz, Romina L.; Tassi, Franco; Venturi, Stefania; Jofré, Cynthia B.; Caffe, Pablo J.; Córdoba, Francisco E. (November 2020). "Chemical and isotopic features of Li-rich brines from the Salar de Olaroz, Central Andes of NW
432:
Borda, Laura G.; Godfrey, Linda V.; Del Bono, Daniela A.; Blanco, Cecilia; GarcĂa, M. Gabriela (September 2023). "Low-temperature geochemistry of B in a hypersaline basin of
Central Andes: Insights from mineralogy and isotopic analysis (δ11B and 87Sr/86Sr)".
129:
and
Coranzuli crop out northwest and east of Pairique, respectively. Some volcanic rocks once attributed to Pairique seem to come from neighbouring volcanic centres such as Lina, Nevado Torona-San Pedro and Pairique Grande.
609:
Kay, Suzanne
Mahlburg; Coira, Beatriz L.; Caffe, Pablo J.; Chen, Chang-Hwa (2010-12-01). "Regional chemical diversity, crustal and mantle sources and evolution of central Andean Puna plateau ignimbrites".
460:
Peralta Arnold, Y.; Cabassi, J.; Tassi, F.; Caffe, P.J.; Vaselli, O. (May 2017). "Fluid geochemistry of a deep-seated geothermal resource in the Puna plateau (Jujuy
Province, Argentina)".
237:
Kay, Suzanne
Mahlburg; Coira, Beatriz; Mpodozis, Constantino (2008-01-01). "Field trip guide: Neogene evolution of the central Andean Puna plateau and southern Central Volcanic Zone".
118:, although the volcanic eruptions of Pairique were less extensive than these from many other APVC volcanoes. Pairique is often considered to be the oldest caldera of the APVC.
149:. The Rio Pairique originates within the volcanic complex and together with the Rio Aguas Calientes from the northwest forms the Rio Rosario, which drains to the southeast.
385:"Geochronological imaging of an episodically constructed subvolcanic batholith: U-Pb in zircon chronochemistry of the Altiplano-Puna Volcanic Complex of the Central Andes"
580:
Cabrera, A. P.; Caffe, P. J. (2009-08-01). "The Cerro Morado
Andesites: Volcanic history and eruptive styles of a mafic volcanic field from northern Puna, Argentina".
348:
Coira, BeatrĂz; Davidson, John; Mpodozis, Constantino; Ramos, Victor (November 1982). "Tectonic and magmatic evolution of the Andes of northern
Argentina and Chile".
303:
204:
99:, the Arco Jara ignimbrite and the Cerro Lucho lavas. All of these do not exceed 5 cubic kilometres (1.2 cu mi) of volume. Right-lateral
258:
654:
115:
383:
Kern, Jamie M.; Silva, Shanaka L. de; Schmitt, Axel K.; Kaiser, Jason F.; Iriarte, A. Rodrigo; Economos, Rita (2016-08-01).
21:
649:
498:
83:
composition. Later it was found that the volcanic complex is better described as a semicircular group of
114:. Later dates imply volcanic activity between 11.5 and 10.3 million years ago. Pairique is part of the
619:
589:
396:
357:
173:
153:
with temperatures of 35–62 °C (95–144 °F) occur at
Pairique and appear to be connected to
146:
134:
96:
520:
414:
304:"El Complejo volcánico Pairique.Volcanismo peraluminoso Tipo S en los Andes Centrales del Sur"
254:
216:
110:
between 8 and 6.7 million years ago, when volcanism reactivated on the
Argentine side of the
627:
597:
556:
548:
510:
477:
469:
442:
404:
365:
246:
154:
53:
100:
92:
623:
593:
400:
361:
57:
643:
631:
473:
369:
274:
203:
Caffe, P. J.; Soler, M. M.; Coira, B.; Cabrera, A. P.; Flores, P. I. (2007-06-01).
126:
122:
446:
601:
552:
250:
169:
165:
150:
138:
72:
524:
515:
418:
220:
125:
volcanic centre is close. It erupted later than Pairique. The ignimbrites of
36:
23:
111:
88:
84:
80:
61:
205:"EstratigrafĂa y centros eruptivos de la region de Pairique, Puna jujeña"
142:
561:
482:
409:
384:
107:
76:
68:
172:
intrusions. Mineral deposits are associated with Pairique, including
161:
141:
sediments which crop out in neighbouring mountain ranges, and by the
95:. Eruption products associated with Pairique are the Pairique Chico
176:; the Rosario river, its main tributary, originates at Pairique.
331:
329:
308:
Consejo Nacional de Investigaciones CientĂficas y TĂ©cnicas
302:
CAFFE, P.; SOLER, M.; RODRĂŤGUEZ, G.; COIRA, B. (2005).
275:"Geology and metal ore deposits in the Argentine Puna"
67:The volcano features what was once thought to be a
320:
87:. These were emplaced on older and partly eroded
71:, which contributed to the formation of regional
297:
295:
198:
196:
194:
192:
190:
188:
612:Journal of Volcanology and Geothermal Research
497:Alonso, R. N.; Viramonte, J. G. (1987-12-30).
462:Journal of Volcanology and Geothermal Research
232:
230:
8:
335:
209:Revista de la AsociaciĂłn GeolĂłgica Argentina
560:
514:
481:
408:
582:Journal of South American Earth Sciences
541:Journal of South American Earth Sciences
184:
7:
499:"GeologĂa y Metalogenia de la Puna"
160:Volcanic rocks at Pairique include
14:
632:10.1016/j.jvolgeores.2010.08.013
474:10.1016/j.jvolgeores.2017.03.030
168:inclusions. Older lavas feature
106:Pairique formed during the late
116:Altiplano-Puna volcanic complex
1:
447:10.1016/j.chemgeo.2023.121620
602:10.1016/j.jsames.2009.03.007
553:10.1016/j.jsames.2020.102742
370:10.1016/0012-8252(82)90042-3
671:
50:Pairique volcanic complex
516:10.3989/egeol.87435-6610
336:Cabrera & Caffe 2009
103:have affected the area.
655:Volcanoes of Argentina
350:Earth-Science Reviews
251:10.1130/2008.0013(05)
624:2010JVGR..198...81K
594:2009JSAES..28..113C
503:Estudios GeolĂłgicos
401:2016Geosp..12.1054K
362:1982ESRv...18..303C
33: /
650:Miocene lava domes
410:10.1130/GES01258.1
97:block and ash flow
260:978-0-8137-0013-7
137:is formed by the
133:The non-volcanic
37:22.917°S 66.833°W
662:
635:
605:
567:
566:
564:
535:
529:
528:
518:
494:
488:
487:
485:
457:
451:
450:
435:Chemical Geology
429:
423:
422:
412:
380:
374:
373:
345:
339:
333:
324:
318:
312:
311:
299:
290:
289:
287:
286:
271:
265:
264:
234:
225:
224:
200:
93:sector collapses
54:volcanic complex
48:
47:
45:
44:
43:
42:-22.917; -66.833
38:
34:
31:
30:
29:
26:
670:
669:
665:
664:
663:
661:
660:
659:
640:
639:
638:
618:(1–2): 81–111.
608:
579:
575:
570:
537:
536:
532:
496:
495:
491:
459:
458:
454:
431:
430:
426:
382:
381:
377:
347:
346:
342:
334:
327:
321:Kay et al. 2010
319:
315:
301:
300:
293:
284:
282:
273:
272:
268:
261:
236:
235:
228:
202:
201:
186:
182:
174:Salar de Olaroz
41:
39:
35:
32:
27:
24:
22:
20:
19:
17:
12:
11:
5:
668:
666:
658:
657:
652:
642:
641:
637:
636:
606:
588:(2): 113–131.
576:
574:
571:
569:
568:
530:
505:(in Spanish).
489:
452:
424:
375:
340:
338:, p. 116.
325:
313:
291:
266:
259:
226:
215:(2): 242–256.
211:(in Spanish).
183:
181:
178:
145:Peña Colorada
58:Jujuy Province
15:
13:
10:
9:
6:
4:
3:
2:
667:
656:
653:
651:
648:
647:
645:
633:
629:
625:
621:
617:
613:
607:
603:
599:
595:
591:
587:
583:
578:
577:
572:
563:
558:
554:
550:
546:
542:
534:
531:
526:
522:
517:
512:
508:
504:
500:
493:
490:
484:
479:
475:
471:
467:
463:
456:
453:
448:
444:
440:
436:
428:
425:
420:
416:
411:
406:
402:
398:
394:
390:
386:
379:
376:
371:
367:
363:
359:
355:
351:
344:
341:
337:
332:
330:
326:
323:, p. 85.
322:
317:
314:
310:(in Spanish).
309:
305:
298:
296:
292:
281:. p. 182
280:
276:
270:
267:
262:
256:
252:
248:
244:
240:
233:
231:
227:
222:
218:
214:
210:
206:
199:
197:
195:
193:
191:
189:
185:
179:
177:
175:
171:
167:
163:
158:
156:
152:
148:
144:
140:
136:
131:
128:
124:
119:
117:
113:
109:
104:
102:
98:
94:
90:
86:
82:
78:
74:
70:
65:
63:
59:
55:
51:
46:
615:
611:
585:
581:
562:2158/1211162
544:
540:
539:Argentina".
533:
509:(5–6): 402.
506:
502:
492:
483:2158/1087501
465:
461:
455:
438:
434:
427:
392:
388:
378:
356:(3–4): 323.
353:
349:
343:
316:
307:
283:. Retrieved
279:ResearchGate
278:
269:
242:
239:Field Guides
238:
212:
208:
159:
132:
127:Cerro Guacha
123:Cerro Morado
121:The younger
120:
105:
66:
49:
18:
468:: 121–134.
395:(4): 1056.
157:degassing.
151:Hot springs
73:ignimbrites
40: /
644:Categories
547:: 102742.
441:: 121620.
285:2017-04-24
180:References
170:rhyodacite
166:cordierite
139:Ordovician
89:lava flows
85:lava domes
525:1988-3250
419:1553-040X
389:Geosphere
221:0004-4822
147:formation
81:rhyolitic
62:Argentina
143:Tertiary
135:basement
16:Landmark
620:Bibcode
590:Bibcode
573:Sources
397:Bibcode
358:Bibcode
245:: 127.
108:Miocene
77:dacitic
69:caldera
56:in the
28:66°50′W
25:22°55′S
523:
417:
257:
219:
162:dacite
155:mantle
101:faults
164:with
52:is a
521:ISSN
415:ISSN
255:ISBN
217:ISSN
112:Puna
628:doi
616:198
598:doi
557:hdl
549:doi
545:103
511:doi
478:hdl
470:doi
466:338
443:doi
439:635
405:doi
366:doi
247:doi
79:to
75:of
646::
626:.
614:.
596:.
586:28
584:.
555:.
543:.
519:.
507:43
501:.
476:.
464:.
437:.
413:.
403:.
393:12
391:.
387:.
364:.
354:18
352:.
328:^
306:.
294:^
277:.
253:.
243:13
241:.
229:^
213:62
207:.
187:^
64:.
60:,
634:.
630::
622::
604:.
600::
592::
565:.
559::
551::
527:.
513::
486:.
480::
472::
449:.
445::
421:.
407::
399::
372:.
368::
360::
288:.
263:.
249::
223:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.