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Early Mesoproterozoic evolution of midcontinental Laurentia: Defining the geon 14 Baraboo orogeny

Geoscience Frontiers 2021年第5期12卷 37-53页

作者： L.Gordon Medaris Jr Brad S.Singer Brian R.Jicha David H.Malone Joshua J.Schwartz Esther K.Stewart amanda van lankvelt Michael L.Williams Peter W.Reiners Department of Geoscience University of Wisconsin-MadisonMadisonWI 53706USA Department of Geography Geology&EnvironmentIllinois State UniversityNormalIL 61790USA Department of Geological Sciences California State University-NorthridgeNorthridgeCA 91330USA Wisconsin Geological&Natural History Survey MadisonWI 53705USA Cameca Instruments 5470 Nobel Dr.MadisonWI 54711USA Department of Geosciences University of Massachusetts-AmherstAmherstMA 01003USA Department of Geosciences University of ArizonaTucsonAZ 85721USA

New geochronologic data from midcontinental Laurentia demonstrate that emplacement of the 1476-1470 Ma Wolf River granitic batholith was not an isolated igneous event,but was accompanied by regional metamorphism,deformation,and *** for such metamorphism and deformation is best seen in siliciclastic sedimentary rocks of the Baraboo Interval,which were deposited closely following the 1.65-1.63 Ga Mazatzal *** Baraboo Interval strata,muscovite parallel to slatey cleavage,in hydrothermal veins,in quartzite breccia,and in metamorphosed paleosol yielded ^(40)Ar/^(39)Ar plateau ages of 1493-1465 *** addition,U-Th-total Pb dating of neoblastic overgrowths on detrital monazite gave an age of 1488±20 Ma,and recrystallized hematite in folded metapelite gave a mean U/Th-He age of 1411±39 ***-Baraboo,arkosic polymictic conglomerate,which contains detrital zircon with a minimum peak age of 1493 Ma,was intruded by a 1470 Ma granite porphyry at the northeastern margin of the Wolf River *** episode of magmatism,regional deformation and metamorphism,and sedimentation,which is designated herein as the Baraboo orogeny,provides a midcontinental link between the Picuris orogeny to the southwest and the Pinware orogeny to the northeast,completing the extent of early Mesoproterozoic(Calymmian)orogenesis for 5000 km along the southern margin of *** transcontinental orogen is unique among Precambrian orogenies for its great width(-1600 km),the predominance of ferroan granites derived from partial melting of lower continental crust,and the prevalence of regional high T-P metamorphism related to advective heating by granitic magmas emplaced in the middle to upper crust.

关键词： Mesoproterozoic orogeny Ferroan granite Detrital zircon ^(40)Ar/^(39)Ar geochronology U-Th-total Pb geochronology U/Th-He geochronology

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