20:
96:
Age and isotope data show that southern North
America is composed of a series of northeast-trending provinces representing island arc terranes accreted onto the 1800 Mya core of Laurentia. These are the Yavapai province (1800–1700 Mya), the Mazatzal province (1700–1650 Mya), the Granite-Rhyolite
143:
passive margins that indicate the orogenic system once extended much further. This is part of the basis for the AUSWUS reconstruction of
Rodinia, which places Australia adjacent to the southwestern US from 1800 to 1000 Mya. Other supporting evidence includes correspondence of 1450 and 1000 Ga
97:
province (1500–1300 Mya), and the Llano-Grenville province (1300–1000 Mya). Each is interpreted as juvenile crust of an island arc, together with smaller amounts of reworked older crust, that accreted to
Laurentia in an orogenic pulse accompanied by
480:"Revised regional correlations and tectonic implications of Paleoproterozoic and Mesoproterozoic metasedimentary rocks in northern New Mexico, USA: New findings from detrital zircon studies of the Hondo Group, Vadito Group, and Marqueñas Formation"
239:
in
Arizona, deposited during the transition from the Yavapai to the Mazatzal orogens at 1700 Mya. The extensional basin in which the Mazatzal Group was deposited lasted about 30 Ma, from the Payson Ophiolite at 1730 Mya to the
590:"Detrital zircon evidence for non-Laurentian provenance, Mesoproterozoic (ca. 1490-1450 Mya) deposition and orogenesis in a reconstructed orogenic belt, northern New Mexico, USA: Defining the Picuris orogeny"
101:
emplacement. The plutons sutured new and existing orogens together and helped convert the juvenile terranes to mature crust. The orogen pulses are identified as the
Yavapai orogeny at 1710–1680 Mya, the
876:
304:
Mako, Calvin A.; Williams, Michael L.; Karlstrom, Karl E.; Doe, Michael F.; Powicki, David; Holland, Mark E.; Gehrels, George; Pecha, Mark (December 2015).
247:
A number of regional orogenies fall within the time span of the
Yavapai orogeny and are regarded as parts of the overall orogenic system. These include the
772:
KARLSTROM, KARL E.; BOWRING, SAMUEL A.; CONWAY, CLAY M. (1987). "Tectonic significance of an Early
Proterozoic two-province boundary in central Arizona".
809:"REVISED LOCATION FOR THE YAVAPAI-MAZATZAL CRUSTAL PROVINCE BOUNDARY IN NEW MEXICO: HF ISOTOPIC DATA FROM PROTEROZOIC ROCKS OF THE NACIMIENTO MOUNTAINS"
191:, then northeastward to the mid-continent region. The southern boundary is somewhat poorly defined, possibly because it corresponds to a shallow relic
216:
350:"Long-lived (1.8–1.0 Ga) convergent orogen in southern Laurentia, its extensions to Australia and Baltica, and implications for refining Rodinia"
921:
Sims, P. K.; Petermar, Z. E. (1986). "Early
Proterozoic Central Plains orogen: A major buried structure in the north-central United States".
707:
Goodge, J. W.; Vervoort, J. D.; Fanning, C. M.; Brecke, D. M.; Farmer, G. L.; Williams, I. S.; Myrow, P. M.; DePaolo, D. J. (11 July 2008).
971:
679:"On the edge: U–Pb, Lu–Hf, and Sm–Nd data suggests reworking of the Yilgarn craton margin during formation of the Albany-Fraser Orogen"
348:
Karlstrom, Karl E; Åhäll, Karl-Inge; Harlan, Stephen S; Williams, Michael L; McLelland, James; Geissman, John W (1 October 2001).
875:
Cox, RĂłnadh; Martin, Mark W.; Comstock, Jana C.; Dickerson, Laura S.; Ekstrom, Ingrid L.; Sammons, James H. (December 2002).
694:"Late Mesoproterozoic (ca 1.2 Ga) palaeomagnetism of the Albany–Fraser orogen: no pre-Rodinia Australia–Laurentia connection"
976:
961:
589:
553:
Condie, Kent C. (1982). "Plate-tectonics model for
Proterozoic continental accretion in the southwestern United States".
981:
433:
199:. Individual island arc terranes accreted to Laurentia during the Yavapai Orogeny include the Elves Chasm block in the
413:
403:
306:"Polyphase Proterozoic deformation in the Four Peaks area, central Arizona, and relevance for the Mazatzal orogeny"
136:
imbricated the successions. That is, faulted blocks of rock were stacked atop each other like shingles on a roof.
900:
842:
808:
434:"The Yavapai-Mazatzal boundary: A long-lived tectonic element in the lithosphere of southwestern North America"
942:
793:
148:
between
Australia and Laurentia. The northeastern extension of the orogenic belt would then correspond to the
574:
643:
678:
349:
966:
69:
with the proto-North American continent. This was the first in a series of orogenies within a long-lived
36:
877:"Sedimentology, stratigraphy, and geochronology of the Proterozoic Mazatzal Group, central Arizona"
19:
241:
160:. However, the placement of Australia has been disputed on the basis of paleomagnetic data. The
807:
Grambling, Tyler A.; Holland, Mark; Karlstom, Karl E.; Gehrels, George E.; Pecha, Mark (2015).
256:
252:
843:"The reconstruction of a middle Proterozoic orogenic belt in north-central New Mexico, U.S.A."
709:"A Positive Test of East Antarctica-Laurentia Juxtaposition Within the Rodinia Supercontinent"
635:
282:
157:
930:
888:
841:
Daniel, Christopher G.; Karlstrom, Karl E.; Williams, Michael L.; Pedrick, Jane N. (1995).
781:
720:
601:
562:
445:
361:
317:
23:
Precambrian provinces of western North America, showing the Yavapai Province (in dark grey)
708:
8:
70:
934:
892:
785:
724:
693:
605:
566:
449:
365:
321:
744:
277:
172:
161:
145:
373:
736:
409:
377:
272:
78:
748:
259:
orogeny at 1708–1750 Mya that produced the Cheyenne belt, the Colorado province or
938:
896:
789:
728:
652:
636:"Timing of Gothian structural evolution in SE Norway: A Rb-Sr whole-rock age study"
609:
570:
533:
491:
453:
369:
325:
260:
204:
122:
121:
at 1700 and 1650 Mya that accumulated sand and high-silica volcanic debris to form
103:
51:
47:
478:
Jones, James V. III; Daniel, Christopher G.; Frei, Dirk; Thrane, Kristine (2011).
248:
212:
196:
192:
165:
149:
107:
223:. Quartzite-rhyolite successions associated with extensional basins include the
236:
208:
140:
118:
82:
16:
Mountain building event 1.7 billion years ago in the southwestern United States
588:
Daniel, C. G.; Pfeifer, L. S.; Jones, J. V.; McFarlane, C. M. (23 July 2013).
955:
381:
188:
114:
732:
656:
88:, which ended an 800-million-year episode of convergent boundary tectonism.
740:
224:
200:
133:
228:
538:
521:
496:
479:
330:
305:
232:
63:
55:
44:
40:
62:, it is interpreted as the collision of the 1800-1700 Mya age Yavapai
613:
457:
405:
Early recumbent folding during Proterozoic orogeny in central Arizona
220:
125:
74:
184:
132:
successions. Subsequent convergent tectonics closed the basins and
129:
432:
Magnani, M.B.; Miller, K.C.; Levander, A.; Karlstrom, K. (2004).
180:
176:
153:
85:
66:
59:
32:
806:
691:
98:
840:
431:
676:
110:
at 1450–1300 Mya, and the Grenville orogeny at 1300–950 Mya.
522:"Tectonic model for the Proterozoic growth of North America"
347:
901:
10.1130/0016-7606(2002)114<1535:SSAGOT>2.0.CO;2
706:
587:
874:
943:
10.1130/0091-7613(1986)14<488:EPCPOA>2.0.CO;2
794:
10.1130/0016-7606(1987)99<529:TSOAEP>2.0.CO;2
575:
10.1130/0091-7613(1982)10<37:PMFPCA>2.0.CO;2
303:
39:
that occurred between 1710 and 1680 million years ago (
771:
850:
New Mexico Geological Society Field Conference Series
816:
New Mexico Geological Society Field Conference Series
477:
251:(1710–1680 Mya) in the New York Mountains area; the
168:
on the southwest extension of the Yavapai Province.
343:
341:
519:
401:
139:The northeast-trending provinces are truncated by
633:
427:
425:
953:
696:. Geophysical Journal International. p. F6.
338:
520:Whitmeyer, Steven; Karlstrom, Karl E. (2007).
422:
408:. Geological Society of America. p. 156.
299:
297:
581:
35:(mountain-building) event in what is now the
920:
294:
868:
767:
765:
800:
546:
537:
495:
329:
834:
692:Pisarevsky, S.A. and co-authors (2003).
634:Graversen, Ole; Pedersen, Svend (1999).
515:
513:
511:
509:
507:
113:Some of the orogens were accompanied by
18:
762:
471:
171:The Yavapai Province was named for the
954:
914:
881:Geological Society of America Bulletin
774:Geological Society of America Bulletin
677:Kirkland, C.J. and co-authors (2011).
594:Geological Society of America Bulletin
552:
438:Geological Society of America Bulletin
156:and the southwestern extension to the
77:that ended with the ca. 1200–1000 Mya
504:
681:. Precambrian Research. p. 223.
203:, Green Mountain, Dubois-Cochetopa,
13:
14:
993:
972:Precambrian geology of New Mexico
219:. The latter includes the Payson
81:during the final assembly of the
700:
685:
670:
627:
395:
91:
1:
374:10.1016/S0301-9268(01)00154-1
288:
195:, but runs roughly along the
7:
402:Karlstrom, Karl E. (1989).
266:
117:. This created short-lived
54:. Recorded in the rocks of
10:
998:
977:Paleoproterozoic orogenies
962:Orogenies of North America
644:Norsk Geologisk Tidsskrift
255:in the mid-continent; the
37:Southwestern United States
982:Proterozoic North America
244:sometime after 1700 Mya.
733:10.1126/science.1159189
657:10.1080/002919699433906
242:Mazatzal Peak Quartzite
253:Central Plains orogeny
164:reconstruction places
24:
283:Geology of New Mexico
158:Albany-Fraser orogeny
106:at 1650–1600 Ga, the
22:
354:Precambrian Research
935:1986Geo....14..488S
893:2002GSAB..114.1535C
786:1987GSAB...99..529K
725:2008Sci...321..235G
606:2013GSAB..125.1423D
600:(9–10): 1423–1441.
567:1982Geo....10...37C
450:2004GSAB..116.1137M
366:2001PreR..111....5K
322:2015Geosp..11.1975M
146:paleomagnetic poles
71:convergent boundary
967:Geology of Arizona
539:10.1130/GES00055.1
497:10.1130/GES00614.1
331:10.1130/GES01196.1
278:Geology of Arizona
263:at 1780–1700 Mya.
179:. It extends from
173:Yavapai Supergroup
119:extensional basins
25:
887:(12): 1535–1549.
719:(5886): 235–240.
273:List of orogenies
79:Grenville orogeny
989:
947:
946:
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907:
872:
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663:
651:(47–56): 47–56.
640:
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614:10.1130/B30804.1
585:
579:
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458:10.1130/B25414.1
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393:
392:
390:
388:
345:
336:
335:
333:
316:(6): 1975–1995.
301:
261:Colorado orogeny
211:-Gold Hill, and
205:Irving Formation
123:Paleoproterozoic
104:Mazatzal orogeny
52:Paleoproterozoic
997:
996:
992:
991:
990:
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952:
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291:
269:
249:Ivanpah orogeny
197:Jemez Lineament
193:subduction zone
166:East Antarctica
150:Gothian orogeny
108:Picuris orogeny
94:
73:along southern
29:Yavapai orogeny
17:
12:
11:
5:
995:
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984:
979:
974:
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949:
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833:
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580:
545:
503:
490:(4): 974–991.
470:
421:
414:
394:
337:
292:
290:
287:
286:
285:
280:
275:
268:
265:
237:Mazatzal Group
141:Neoproterozoic
93:
90:
83:supercontinent
15:
9:
6:
4:
3:
2:
994:
983:
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978:
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189:Cheyenne belt
187:south of the
186:
182:
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174:
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167:
163:
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155:
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142:
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115:slab rollback
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53:
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21:
926:
922:
916:
904:. Retrieved
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858:. Retrieved
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849:
836:
824:. Retrieved
819:
815:
802:
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773:
752:. Retrieved
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662:15 September
660:. Retrieved
648:
642:
629:
617:. Retrieved
597:
593:
583:
558:
554:
548:
529:
525:
487:
483:
473:
461:. Retrieved
441:
437:
404:
397:
385:. Retrieved
357:
353:
313:
309:
257:Medicine Bow
246:
225:Vadito Group
201:Grand Canyon
170:
138:
112:
95:
28:
26:
444:(9): 1137.
360:(1): 5–30.
229:Hondo Group
175:in central
92:Description
956:Categories
929:(6): 488.
780:(4): 529.
532:(4): 220.
289:References
233:New Mexico
64:island arc
56:New Mexico
45:Statherian
43:), in the
822:: 175–184
561:(1): 37.
526:Geosphere
484:Geosphere
382:0301-9268
310:Geosphere
221:Ophiolite
213:Ash Creek
126:quartzite
75:Laurentia
906:19 April
860:19 April
826:19 April
754:19 April
749:11799613
741:18621666
619:19 April
463:19 April
387:19 April
267:See also
235:and the
185:Colorado
130:rhyolite
33:orogenic
931:Bibcode
923:Geology
889:Bibcode
782:Bibcode
721:Bibcode
713:Science
602:Bibcode
563:Bibcode
555:Geology
446:Bibcode
362:Bibcode
318:Bibcode
181:Arizona
177:Arizona
154:Baltica
86:Rodinia
67:terrane
60:Arizona
50:of the
31:was an
747:
739:
412:
380:
217:Payson
209:Moppin
134:thrust
99:pluton
48:Period
856:: 193
846:(PDF)
812:(PDF)
745:S2CID
639:(PDF)
162:SWEAT
908:2020
862:2020
828:2020
756:2020
737:PMID
664:2015
621:2020
465:2020
410:ISBN
389:2020
378:ISSN
227:and
58:and
27:The
939:doi
897:doi
885:114
790:doi
729:doi
717:321
653:doi
610:doi
598:125
571:doi
534:doi
492:doi
454:doi
442:116
370:doi
358:111
326:doi
231:in
183:to
152:in
41:Mya
958::
937:.
927:14
925:.
895:.
883:.
879:.
854:46
852:.
848:.
820:66
818:.
814:.
788:.
778:99
776:.
764:^
743:.
735:.
727:.
715:.
711:.
649:79
647:.
641:.
608:.
596:.
592:.
569:.
559:10
557:.
528:.
524:.
506:^
486:.
482:.
452:.
440:.
436:.
424:^
376:.
368:.
356:.
352:.
340:^
324:.
314:11
312:.
308:.
296:^
207:,
945:.
941::
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830:.
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530:3
500:.
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488:7
467:.
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391:.
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334:.
328::
320::
215:-
128:-
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