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Pamphlet PDF File Geologic Map of Precambrian Rocks, Rawhide Buttes West Quadrangle and Part of Rawhide Buttes East Quadrangle, Hartville Uplift, Goshen and Niobrara Counties, Wyoming By W.C. Day, P.K. Sims, G.L. Snyder, A.B. Wilson, and T.L. Klein, with a section on Geochronology by Zell E. Peterman, Kiyoto Futa, and R.E. Zartman Pamphlet to accompany map Geologic Investigations Series I–2635 1999 U.S. Department of the Interior U.S. Geological Survey CONTENTS Introduction 1 Stratigraphy 2 Granitic rocks 3 Structure 3 Deformations D1 and D2 4 Deformations D3 and D4 4 Terranes Delineated in map area 5 Rawhide Buttes terrane 6 Flattop Butte terrane 6 Rawhide Creek terrane 7 Muskrat Canyon terrane 8 Wildcat Hills terrane 8 Acknowledgments 8 Geochronology 10 Flattop Butte Granite 10 Rawhide Buttes Granite 12 References cited 14 FIGURES 1. Index map of Hartville uplift showing outline of Rawhide Buttes West and Rawhide Buttes East quadrangles 1 2. Precambrian basement map of north-central United States and adjacent Canada 1 3. K-Q-P diagram showing compositions (volume percent) of 2.65-Ga Flattop Butte Granite and 2.66-Ga Rawhide Buttes Granite 3 4. Index to tectonostratigraphic terranes in Rawhide Buttes West and Rawhide Buttes East quadrangles 5 5. Equal-area projections (lower hemisphere) of structures in Rawhide Buttes Granite in Rawhide Buttes terrane 6 6. Equal-area projections (lower hemisphere) of structures in Bald Butte domain of Rawhide Buttes terrane 7 7. Equal-area projection (lower hemisphere) of structures in southern part of Flattop Butte terrane 7 8. Equal-area projections (lower hemisphere) of D2 structures in Flattop Butte Granite 8 9. Map showing localities of geochronology samples 9 10. Rubidium-strontium isochron diagram for whole-rock samples of the Flattop Butte Granite 11 11. Uranium-lead concordia diagram for the zircons from the gneiss at Cassa anticline and the Flattop Butte Granite 12 12. Rubidium-strontium isochron diagram for Rawhide Buttes Granite 12 TABLES 1. Tectonic evolution of Hartville Uplift during the Precambrian 2 2. Approximate modes of Rawhide Buttes Granite (percent by volume) 4 3. Approximate modes of Flattop Butte Granite (percent by volume) 4 4. Rubidium and strontium data for whole-rock samples and minerals from the Flattop Butte Granite and Rawhide Buttes Granite 10 5. Samarium-neodymium data for whole-rock samples from the Hartville Uplift 11 6. Uranium, thorium, and lead data for zircons from the Flattop Butte Granite and gneiss at Cassa anticline 12 ii INTRODUCTION 112° 108° 104° 100° 96° YXs XAm Detailed geologic mapping (scale 1:24,000) of Precam- 56° brian rocks in the Hartville Uplift, southeastern Wyoming OROGEN (Day and others, 1994; fig. 1) following earlier regional CREE LAKE ZONE/HEARNE Thompson geologic mapping (scale 1:48,000) by Snyder (1980) has PROVINCE belt shown that the Late Archean granite and supracrustal rocks (Whalen Group) of the Wyoming province (fig. 2) were ONTARIO deformed during three convergent (tectonic) events in the Early Proterozoic, extending from between ~2.1 Ga to 52° ALBERTA pre-1.7 Ga (table 1). These events are recorded in the SASKATCHEWAN XAi Guernsey quadrangle (Sims and others, 1997) (fig. 1) and RAE AND HEARNE TRANS-HUDSON are expressed in part in this map area. From oldest to PROVINCES XAm ° 104 45´ 104°30´ 42° 45´ EXPLANATION MANITOBA NORTH DAKOTA Haystack Range Granite, GFTZ 1.73 Ga 48° Twin Hills Diorite, 1.74 Ga SUPERIOR WYOMING PROVINCE MINNESOTA Flattop Butte Granite, PROVINCE 2.65 Ga Rawhide Buttes Granite, Boundary of Rawhide 2.66 Ga Buttes quadrangles SOUTH Whalen Group GLTZ DAKOTA MONTANA Contact WYOMING Thrust fault BH 44° Transcurrent YXs movement HU on fault LM Xp FAULT NEBRASKA MB CB Xcp 42° 30´ 0100 200 300 MILES Map area 0 200 400 KILOMETERS EXPLANATION HARTVILLE Tectonic features CB Cheyenne belt Middle and Early Proterozoic GFTZ Great Falls tectonic zone GLTZ YXs Athabasca Sandstone Great Lakes tectonic zone Laramide uplifts and Sioux Quartzite Early Proterozoic (2.5–1.6 BH Black Hills Uplift HU Ga) Hartville Uplift Xcp Central Plains orogen LM Laramie Mountains (1.78–1.64 Ga) MB Medicine Bow Mountains Xp Penokean orogen (2.2–1.84 Ga) Thrust fault—Sawteeth on Early Proterozoic and upper plate; dashed Archean Trans-Hudson where approximately orogen located Hartville XAi Juvenile terranes Fault—Dashed where Study (Reindeer zone) approximately located area XAm Area of Miogeoclinal belt Boundary between exposed I–2567 geologic domains Archean (2.5 Ga and older) Boundary between domains WYOMING Rae and Hearne in the subsurface 26 42° Guernsey provinces Edge of exposed Precam- 15´ Wyoming province brian rocks—Hachures 0 5 10 MILES point toward exposed Superior province area 0 5 10 KILOMETERS Figure 2.MMPrecambrian basement map of north-central United States and adjacent Canada. The Hartville Uplift Figure 1.MMIndex map of Hartville Uplift showing out- (HU) is at the intersection of the Trans-Hudson and line of Rawhide Buttes West and Rawhide Buttes East Central Plains orogens, and rocks in the uplift were quadrangles. Outline of published map I–2567 (Sims deformed by both Early Proterozoic orogenies, as well as and others, 1997) also shown. by an earlier unnamed deformation (D2). 1 Table 1. Tectonic evolution of Hartville Uplift during the doming caused by emplacement of bodies equivalent to the Precambrian. 1.72-Ga Haystack Range Granite. The Precambrian episodes of deformation expressed in Age (Ga) Event the Rawhide Buttes area are similar to those in the Guernsey 1.32 Cryptic event indicated by biotite ages. area. Two regional deformations (D2 and D3) are recognized in the Rawhide Buttes East and Rawhide Buttes West ca. 1.4 Emplacement of mafic dikes; undeformed. 1:24,000 quadrangles. They compose a fold-and-thrust belt ca. 1.6 Cryptic thermal event, indicated by sphene, apatite, (D3) on the western, continental margin of the Trans-Hudson and monazite. orogen. A generally prominent ductile S-surface (S3) con- 1.72 Emplacement of Haystack Range Granite as domes, taining a stretching lineation (L3) is present locally. The with deformed and metamorphosed margins— stretching lineation (X direction of the strain ellipsoid) Deformation D4. plunges moderately southeast, indicating a northwest direc- tion of tectonic transport (see map) during deformation D . 1.74 Emplacement of Twin Hills Diorite as a predecessor 3 Deformation D affected the entire uplift. It was a compres- to Haystack Range Granite. 2 sional deformation characterized by south-vergent folds. D4 Deformation D3—West-vergent fold-and-thrust belt resulted in the formation of mullion structures and strong on western continental margin of Trans- Hudson gneissic foliation in the margin of ~1.7-Ga plutons as well as orogen; extends length of uplift. a doming of the supracrustal rocks adjacent to the plutons. 2.1–1.98 Deformation D2—Intense folding on east-west Since publication of map I–2567 (Sims and others, axes and accompanying metamorphism; south- 1997), the Precambrian geology of the Guernsey and Case- vergent. Dated by Rb-Sr whole-rock and sphene bier Hills quadrangles, in the southern part of the Hartville methods on Flattop Butte Granite. Uplift, we have determined that the layered supracrustal ca. 2.0 Emplacement of mafic dike swarm in rift fractures. rocks throughout the Hartville Uplift, assigned to the Whalen Group, are Late Archean. On the earlier published 2.65 Crystallization of Rawhide Buttes and Flattop Butte map, we classified these rocks as being either Early Protero- Granite plutons. zoic or Late Archean. The Flattop Butte Granite, previously Deformation D1—Nappe Formation thought to date from 1.98 Ga but now known to be Late Archean (2.65 Ga), cuts and intrudes the layered rocks. Deposition of Whalen Group. Also, on the earlier map, we erroneously considered the ca 3.0 Crystalline basement, indicated by Sm-Nd ages. Rawhide Buttes Granite as basement to the Whalen Group. Instead, the basement is an unidentified crystalline sequence youngest, the deformation events are (1) inversion of (>2.8 Ga), as indicated by Sm-Nd isotopic data (see table 5). supracrustal succession (deformation D1), at least in parts of In this report, we use informal lithologic names to the uplift; (2) south-vergent folding of rocks on east-west describe the supracrustal rocks of the Whalen Group axes (D2) with concomitant prograde metamorphism; and (Smith, 1903). We propose the formal name "Rawhide (3) west-vergent folding on north-trending axes and accom- Buttes Granite" for the bodies of granitic rocks exposed at panying thick-skinned thrusting with concomitant prograde Rawhide Buttes (type area) and Rawhide Creek, west of the metamorphism (D3). A subsequent deformation event (D4) Hartville fault. This rock unit was previously called "Gran- was associated with post-tectonic intrusion of granites that ite of Rawhide Buttes" by Snyder (1980). We also propose resulted in doming of the supracrustal rocks. For the Guern- that the Granite of Flattop Butte of Snyder (1980) be for- sey quadrangle D2 is attributed to an older, Early Protero- mally named "Flattop Butte Granite." zoic unnamed orogeny (~1.98 Ga), that produced fold The term "terrane" is used herein in the same way as in nappe(s). Sims and others (1997) assigned the D3 deforma- the North American cordillera (Jones and others, 1977). It tion to the Trans-Hudson orogeny (THO; fig. 2) (post-1.8 comprises a distinctive crustal segment characterized by a Ga; Lewry and others, 1996). However, the absolute age of unique stratigraphy and structural style and is fault the D3 event is poorly constrained. To date, the effects of bounded. the 1.76-Ga Cheyenne Belt deformation, as recorded in the Laramie Range to the west and the Medicine Bow Moun- tains to the southwest (Resor and others, 1996) on the rocks STRATIGRAPHY of the Hartville Uplift are unknown.
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