Geology of the Berne Quadrangle Black Hills South Dakota

Total Page:16

File Type:pdf, Size:1020Kb

Geology of the Berne Quadrangle Black Hills South Dakota Geology of the Berne Quadrangle Black Hills South Dakota GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-F Prepared partly on behalf of the U.S. Atomic Energy Commission Geology of the Berne Quadrangle Black Hills South Dakota By JACK A. REDDEN PEGMATITES AND OTHER PRECAMBRIAN ROCKS IN THE SOUTHERN BLACK HILLS GEOLOGICAL SURVEY PROFESSIONAL PAPER 297-F Prepared partly on behalf of the U.S. Atomic Energy Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington, D.C. 20402 CONTENTS Page Page Abstract._ _-------------_-___________-_____________ 343 Pegmatites Continued Introduction.______________________________________ 344 Mineralogy __ _____________-___-___-_-------_--- 378 Previous work__________________________________ 345 Origin.- --___-____-_-_-_---------------------_ 380 Fieldwork and acknowledgments._-_-_--__________ 345 Paleozoic and younger rocks. ________________________ 381 Geologic setting____--__-______________________ ____ 345 Deadwood Formation, __________________________ 381 Metamorphic rocks_________________________________ 347 Englewood Formation.. _ __________--____-_-__--_ 381 Stratigraphic units west of Grand Junction fault___- 347 Pahasapa Limestone- _______-_____.__-----_-- - 381 Vanderlehr Formation.._____________________ 347 Quaternary and Recent deposits. _________________ 382 Biotite-plagioclase gneiss.________________ 347 Structure __ ___________-___-__--___-_-__------_--- 382 Quartzite, meta-arkose, and metaconglom- Major folds and domes. _______________---------_ 382 erate_ _______________________________ 348 Western Star syncline. ______________________ 382 Calcite-tremolite gneiss__________________ 349 Atlantic Hill anticline. _____________---_----_ 382 Quartz-mica-garnet schist--_--___-_______ 351 Folds between the Vestal Springs and Grand Amphibole schist_______________________ 353 Junction faults ____--__-___-_____-__---_-- 384 Mica and graphite schist-________________ 353 Park dome _ ______________-___-_--------_- 384 Origin of formation _____________________ 354 Bear Mountain dome____--_-______---------- 385 Loues Formation.__________________________ 354 Harney Peak dome.__ _______________________ 385 Bugtown Formation. _____ ___________________ 356 Spring Creek area--------------------------- 385 Quartz-mica-feldspar schist______________ 357 Minor structures __ _ ________-_____-__------_-_- 385 Quartz-mica schist-_____________________ 357 Early structures. ________-___-_.__---------- 385 Meta-iron-f ormation ____________________ 358 Intermediate structures- _____________________ 387 Crow Formation,.__________________________ 358 Late structures.- - __________________________ 389 Mayo Formation. __________________________ 359 Boudinage. _________-_-_-__-_--___-----_--_ 390 Amphibolite.-... _ __________________________ 360 Faults..----- -------------- ____-_-____-- 391 Lithologic units east of Grand Junction fault....... 361 Evolution and summary of structures- ________ 392 Quartzite and quartz-mica schist._____________ 361 Metamorphism_ _______________-_______-__---------- 393 Quartz-biotite-garnet schist-_________________ 362 Sillimanite isograd- _____________________________ 393 Mica schist._______________________________ 363 Mineralogic and textural changes __ _ ________ 394 Quartzite- _-------_________---_____________ 366 Retrograde me tamorphism. ______ _________________ 396 Sequence and possible correlation of lithologic Metasomatism ________________-_-_-_-------_--- 396 units-___________________________________ 367 Economic geology ____-.___________-____-_-_----_ 397 Quartz veins.______________________________________ 367 Pegmatite deposits..---------------------------- 397 Age and origin.________________________________ 369 Mica____ ___---------------_--------------- 397 Pegmatites. __ _ _____________________________________ 370 Feldspar _-_--_--------------_----------- 398 Distribution. _ __________________________________ 370 Beryl-.---------. ----------------------- 398 Size, shape, and attitude_________________________ 370 Lithium minerals. __________________________ 399 Classification and internal structures._____________ 373 Other minerals. ___________-_-_-__-----_--__ Zoned pegmatites.__________________________ 373 399 Fracture fillings.___________________________ 376 400 Layered pegmatites.________________________ 377 Quartz deposits. 402 Homogeneous pegmatites.___________________ 377 References cited. ___ 402 Gneissic pegmatites of the Bear Mountain area- 377 Index. _-_--------_ 405 ILLUSTRATIONS Page PLATE 34. Geologic map and sections of the Berne quadrangle.____-_______________-______-_______------------- In pocket 35. Geologic map and section of the Park dome area___________________-___--____----_---_-------_----- In pocket 36. Map showing major structures and planar and plunge data in the Berne quadrangle. _____________-_---- In pocket FIGURE 121. Index map.-------______-_______________________________________________-_-_-__---___------------- 344 122. Generalized geologic map of part of the southern Black Hills, S. Dak__________________-----_------------- 346 123. Photomicrographs of metamorphic rocks________________________----__-__-__----_-_-__---------------- 350 in IV CONTENTS Page FIGURE 124. Photomicrograph of deformed garnet from the Vanderlehr Formation___________________________________ 351 125. Photomicrographs showing replacement textures of metamorphic rocks___________________________________ 352 126. Photograph of outcrop of the Bugtown Formation._____-_-_-__________________.-__-_-__----------___-_- 356 127. Sketch of early folds in quartzite beds.______________________________________________________________ 362 128. Photomicrograph of staurolite-andalusite schist-________-_---___-_______________-_--------------------_ 366 129. Map showing distribution of pegmatites in the southern Black Hills, S. Dak_______________________________ 371 130. Map showing distribution of zoned pegmatites and beryl-bearing pegmatites in the Berne quadrangle_______ 372 131. Sketch showing mineral orientation and tourmaline altered to muscovite._-____-_-_-__----_--____-_____-__ 375 132. Photograph of boudinage structure in pegmatite.________-_-______-_____________---__--------_---____-_ 376 133. Schematic restoration of prefaulting and predoming structure in the Berne quadrangle._____________________ 383 134. Contour diagram of older linear elements in the Park dome.____________________________________________ 386 135. Block diagram of folds near the Park dome._____________________________________-_-_--_-_---_----___- 387 136. Sketch of fold with deformed axial plane and two schistosities____________________-__-_--__---_-__-______ 387 137. Contour diagram of poles to bedding and late foliation northwest of Atlantic Hill.________--_--_____-______ 388 138. Contour diagram of poles to crosscutting foliation in the Graveyard Gulch area.________----__--_-_-______ 389 139. Sketch of foliation folds--__---------__---__________________________________________________ 390 140. Sketch of boudinage structure in lower amphibole schist unit, Vanderlehr Formation._____________________ 390 141. Photomicrograph of elongate garnets and discordant foliation in the miea schist unit.______________________ 394 142. Photomicrographs of elongate garnets in the mica schist unit-___________________---__--_---------______ 395 143. Map of the Campbell-Ventling adit, Grand Junction mine______-__________________----------__-_-_---_- 401 TABLES Page TABLE 1. Modes of rock units of the Vanderlehr Formation____________________________-----_------_---_--__- 348 2. Modes of rocks of the Loues Formation._____________________________________________________________ 355 3. Modes of rocks of the quartz-biotite-garnet schist unit________________________________________________ 363 4. Spectrographic analyses of a composite sample of the quartz-biotite-garnet schist unit, Park School are.a______ 363 5. Modes of rocks of the mica schist unit___________________________________________________________ 365 6. Semi quantitative spectrographic analyses of mica schist from the mica schist unit________________________ 366 7. Description of quartz-rich veins___--____________________-_-----___-__-____-__--__-_----------__----- 368 8. Mineral assemblages of some wall zones______________----_------------------------------------------- 375 9. Mineral assemblages of some intermediate zones__-__--_----------------------------------------------- 375 10. Mineral assemblages of some cores or innermost exposed zones.__________________--------l-_-__-__-___-_ 376 11. Description of minor accessory pegmatite minerals in the Berne quadrangle------------------------------- 380 12. Summary of mineral production from the major pegmatite mines in the Berne quadrangle. _______________ 397 13. Description of gold mines, Berne quadrangle________---_----------------___-_-_----------------------- 402 PEGMATITES AND OTHER PRECAMBRIAN ROCKS IN THE SOUTHERN BLACK HILLS GEOLOGY OF THE BERNE QUADRANGLE, BLACK HILLS, SOUTH DAKOTA By JACK A. REDDEN ABSTRACT hydrothermal fluids were presumably a factor in tl ? formation The Berne quadrangle, in the southern Black Hills, S. Dak., of the veins. is underlain largely by Precambrian metamorphic rocks. Nu­ Approximately 1,150 granitic pegmatites occur in the quad­ merous bodies of granitic pegmatite
Recommended publications
  • Tectonic Interleaving Along the Main Central Thrust, Sikkim Himalaya
    research-articleResearch ArticleXXX10.1144/jgs2013-064C. M. Mottram et al.Tectonic Interleaving Along the Mct 2014 Journal of the Geological Society, London, Vol. 171, 2014, pp. 255 –268. http://dx.doi.org/10.1144/jgs2013-064 Published Online First on January 14, 2014 © 2014 The Authors Tectonic interleaving along the Main Central Thrust, Sikkim Himalaya CATHERINE M. MOTTRAM1*, T. W. ARGLES1, N. B. W. HARRIS1, R. R. PARRISH2,3, M. S. A. HORSTWOOD3, C. J. WARREN1 & S. GUPTA4 1Department of Environment, Earth and Ecosystems, Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR), The Open University, Walton Hall, Milton Keynes MK7 6AA, UK 2Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK 3NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 4Department of Geology & Geophysics, I.I.T., Kharagpur—721 302, India *Corresponding author (e-mail: [email protected]) Abstract: Geochemical and geochronological analyses provide quantitative evidence about the origin, devel- opment and motion along ductile faults, where kinematic structures have been overprinted. The Main Central Thrust is a key structure in the Himalaya that accommodated substantial amounts of the India–Asia conver- gence. This structure juxtaposes two isotopically distinct rock packages across a zone of ductile deformation. Structural analysis, whole-rock Nd isotopes, and U–Pb zircon geochronology reveal that the hanging wall is characterized by detrital zircon peaks at c. 800–1000 Ma, 1500–1700 Ma and 2300–2500 Ma and an εNd(0) signature of –18.3 to –12.1, and is intruded by c. 800 Ma and c.
    [Show full text]
  • Origin, Texture, and Classification of Metamorphic Rocks - Teklewold Ayalew
    GEOLOGY – Vol. II - Origin, Texture, and Classification of Metamorphic Rocks - Teklewold Ayalew ORIGIN, TEXTURE, AND CLASSIFICATION OF METAMORPHIC ROCKS Teklewold Ayalew Addis Ababa University, Ethiopia Keywords: aluminosilicates, assemblage, fabric, foliation, gneissose banding, index mineral, isograd, lineation, lithosphere, metamorphic facies, metasomatism, orogenic belt, schistosity Contents 1. Introduction 2. Occurrence 2.1. Orogenic Metamorphism 2.2. Contact Metamorphism 2.3. Ocean Floor Metamorphism 3. Classification 4. Minerals of Metamorphic Rocks 5. Metamorphic Facies 5.1. Facies of Very Low Grade 5.2. Greenschist Facies 5.3. Amphibolite Facies 5.4. Granulite Facies 5.5. Hornblende Hornfels Facies 5.6. Pyroxene Hornfels Facies 5.7. Blueschist Facies 5.8. Eclogite Facies 6. Tectonic Setting of Metamorphic Facies 7. Textures 7.1. Layering, Banding, and Fabric Development 8. Kinetics 8.1. Diffusion 8.2. Nucleation 8.3. Crystal Growth AcknowledgmentUNESCO – EOLSS Glossary Bibliography Biographical SketchSAMPLE CHAPTERS Summary Metamorphic rocks are igneous, sedimentary, or other metamorphic rocks whose texture and composition has been changed by metamorphism. Metamorphism occurs as a response to changes in the physical or chemical environment of any pre-existing rock, such as variations in pressure or temperature, strain, or the infiltration of fluids. It involves recrystallization of existing minerals into new grains and/or the appearance of new mineral phases and breakdown of others. Metamorphic processes take place ©Encyclopedia of Life Support Systems (EOLSS) GEOLOGY – Vol. II - Origin, Texture, and Classification of Metamorphic Rocks - Teklewold Ayalew essentially in the solid state. The rock mass does not normally disaggregate and lose coherence entirely; however small amounts of fluids are frequently present and may play an important catalytic role.
    [Show full text]
  • Part 629 – Glossary of Landform and Geologic Terms
    Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition.
    [Show full text]
  • Metamorphic Rocks.Pdf
    Metamorphism & Metamorphic Rocks (((adapted from Brunkel, 2012) Metamorphic Rocks . Changed rocks- with heat and pressure . But not melted . Change in the solid state . Textural changes (always) . Mineralogy changes (usually) Metamorphism . The mineral changes that transform a parent rock to into a new metamorphic rock by exposure to heat, stress, and fluids unlike those in which the parent rock formed. granite gneiss Geothermal gradient Types of Metamorphism . Contact metamorphism – – Happens in wall rock next to intrusions – HEAT is main metamorphic agent . Contact metamorphism Contact Metamorphism . Local- Usually a zone only a few meters wide . Heat from plutons intruded into “cooler” country rock . Usually forms nonfoliated rocks Types of Metamorphism . Hydrothermal metamorphism – – Happens along fracture conduits – HOT FLUIDS are main metamorphic agent Types of Metamorphism . Regional metamorphism – – Happens during mountain building – Most significant type – STRESS associated with plate convergence & – HEAT associated with burial (geothermal gradient) are main metamorphic agents . Contact metamorphism . Hydrothermal metamorphism . Regional metamorphism . Wide range of pressure and temperature conditions across a large area regional hot springs hydrothermal contact . Regional metamorphism Other types of Metamorphism . Burial . Fault zones . Impact metamorphism Tektites Metamorphism and Plate Tectonics . Fault zone metamorphism . Mélange- chaotic mixture of materials that have been crumpled together Stress (pressure) . From burial
    [Show full text]
  • Metamorphic Field Gradients Across the Himachal Himalaya
    TECTONICS, VOL. 32, 540–557, doi:10.1002/tect.20020, 2013 Metamorphic field gradients across the Himachal Himalaya, northwest India: Implications for the emplacement of the Himalayan crystalline core Remington M. Leger,1,2 A. Alexander G. Webb,1 Darrell J. Henry,1 John A. Craig,1 and Prashant Dubey3 Received 28 August 2012; revised 23 January 2013; accepted 3 February 2013; published 31 May 2013. [1] New constraints on pressures and temperatures experienced by rocks of the Himachal Himalaya are presented in order to test models for the emplacement of the Himalayan crystalline core here. A variety of methods were employed: petrographic analysis referenced to a petrogenetic grid, exchange and net-transfer thermobarometry, Ti-in-biotite thermometry, and analysis of quartz recrystallization textures. Rocks along three transects (the northern Beas, Pabbar, and southern Beas transects) were investigated. Results reveal spatially coherent metamorphic field gradients across amphibolite-grade and migmatitic metamorphic rocks. Along the northern Beas transect, rocks record peak temperatures of ~650–780C at low elevations to the north of ~3210’ N; rocks in other structural positions along this transect record peak temperatures of <640C that decrease with increasing structural elevation. Rocks of the Pabbar transect dominantly record ~650–700C peak temperatures to the east of ~7755’ E and ~450–620C peak temperatures farther west. Peak temperatures of ~450–600C along the southern Beas transect record a right-way-up metamorphic field gradient. Results are integrated with literature data to determine a metamorphic isograd map of the Himachal Himalaya. This map is compared to metamorphic isograd map pattern predictions of different models for Himalayan crystalline core emplacement.
    [Show full text]
  • Roadside Geology of Taiwan: a Field Guide
    Roadside geology of taiwan: DȱHOGJXLGH 4UFQIBOJF$IFO About the cover 5IFDPWFSQIPUPEFQJDUTUIFGPMEFE HOFJTTFTJO5BSPLP/BUJPOBM1BSL "MMQIPUPTJOUIJTCPPLCZ 4UFQIBOJF$IFO 'PSNZGBNJMZ PREFACE 5IJTCPPLIBTCFFOXSJUUFOBTQBSUPGUIF 6OJWFSTJUZPG5PSPOUP`T#JH*EFBT&YQMPSJOH (MPCBM5BJXBODPNQFUJUJPO*UIBEBMXBZT CFFONZESFBNUPKVTUDBNQPVUBUBMPDBUJPO GPSBNPOUITBOELOPXFWFSZSPDLBOEPVU DSPQMJLFUIFCBDLPGNZIBOE BOEFWFOUVBMMZ XSJUFBpFMEHVJEFMJLFUIFPOFTUIBUHVJEFE NFUISPVHINZPXOHFPMPHZFEVDBUJPO *EJEO`UHFUUPTUBZGPSNPOUIT*OGBDU *XBTPOMZBCMFUPTUBZGPSPOFNPOUI CVUJU XBTTUJMMBOJODSFEJCMFFYQFSJFODF BOEUSVMZ IVNCMJOH 5BJXBO`THFPMPHZJTWFSZEJWFSTFBOE DPOUBJOTTPNBOZMPDBMTDBMFWBSJBUJPOTXIJDI BUNBOZUJNFTBSFIBSEBOEDIBMMFOHJOHUP pOE*U`TIPUBOEIVNJE NPTRVJUPFTBCPVOE BOEWFOPNPVTTOBLFTMVSLCFOFBUIUIFCSVTI #VUGPSUIPTFXIPBSFXJMMJOHUPUBLFUIFDIBM MFOHFBOEFYQFSJFODFXIBUUIJTMJUUMFJTMBOE DPVOUSZIBTUPP⒎FS ZPVXJMMOPUCFEJTBQ QPJOUFE 4UFQIBOJF C9. Tai Shan Tunnel 42 Table of contents C10. He Huan Shan 45 Southeast Coast 49 SE1. Fanshuliao Bridge 49 SE2. Baxian Cave 50 SE3. East Taiwan Ophiolite 52 Introduction i SE4. Wanrong 55 SE5. Taimali 56 Northern Coast 1 SE6. Lichi Badlands 57 N1. Yu-Ao Roadcut 1 SE7. Sanxiantai 61 N2. Yu-Ao Fishing Port 2 Southwest Coast 67 N3. Yehliu Geopark 4 N4. 13-Level Cu Refinery/Golden Waterfall 9 SW1. Wu Shan Ding 68 N5. Nanya Rock 11 SW2. Xing Yang Nu Hu Bee Farm 70 N6. Heping Dao (Peace Island) 14 SW3. Moon World 71 N7. Elephant’s Trunk/Shen Ao Promontory 16 SW4. Laterites in Southern Taiwan 74 N8. Longdong 20 N9. Bitou Cape 21 N10. Turtle Island 22 N11. Miaoli
    [Show full text]
  • GEOLOGIC MAP of the CHELAN 30-MINUTE by 60-MINUTE QUADRANGLE, WASHINGTON by R
    DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I-1661 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE CHELAN 30-MINUTE BY 60-MINUTE QUADRANGLE, WASHINGTON By R. W. Tabor, V. A. Frizzell, Jr., J. T. Whetten, R. B. Waitt, D. A. Swanson, G. R. Byerly, D. B. Booth, M. J. Hetherington, and R. E. Zartman INTRODUCTION Bedrock of the Chelan 1:100,000 quadrangle displays a long and varied geologic history (fig. 1). Pioneer geologic work in the quadrangle began with Bailey Willis (1887, 1903) and I. C. Russell (1893, 1900). A. C. Waters (1930, 1932, 1938) made the first definitive geologic studies in the area (fig. 2). He mapped and described the metamorphic rocks and the lavas of the Columbia River Basalt Group in the vicinity of Chelan as well as the arkoses within the Chiwaukum graben (fig. 1). B. M. Page (1939a, b) detailed much of the structure and petrology of the metamorphic and igneous rocks in the Chiwaukum Mountains, further described the arkoses, and, for the first time, defined the alpine glacial stages in the area. C. L. Willis (1950, 1953) was the first to recognize the Chiwaukum graben, one of the more significant structural features of the region. The pre-Tertiary schists and gneisses are continuous with rocks to the north included in the Skagit Metamorphic Suite of Misch (1966, p. 102-103). Peter Misch and his students established a framework of North Cascade metamorphic geology which underlies much of our construct, especially in the western part of the quadrangle. Our work began in 1975 and was essentially completed in 1980.
    [Show full text]
  • A Systematic Nomenclature for Metamorphic Rocks
    A systematic nomenclature for metamorphic rocks: 1. HOW TO NAME A METAMORPHIC ROCK Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: Web version 1/4/04. Rolf Schmid1, Douglas Fettes2, Ben Harte3, Eleutheria Davis4, Jacqueline Desmons5, Hans- Joachim Meyer-Marsilius† and Jaakko Siivola6 1 Institut für Mineralogie und Petrographie, ETH-Centre, CH-8092, Zürich, Switzerland, [email protected] 2 British Geological Survey, Murchison House, West Mains Road, Edinburgh, United Kingdom, [email protected] 3 Grant Institute of Geology, Edinburgh, United Kingdom, [email protected] 4 Patission 339A, 11144 Athens, Greece 5 3, rue de Houdemont 54500, Vandoeuvre-lès-Nancy, France, [email protected] 6 Tasakalliontie 12c, 02760 Espoo, Finland ABSTRACT The usage of some common terms in metamorphic petrology has developed differently in different countries and a range of specialised rock names have been applied locally. The Subcommission on the Systematics of Metamorphic Rocks (SCMR) aims to provide systematic schemes for terminology and rock definitions that are widely acceptable and suitable for international use. This first paper explains the basic classification scheme for common metamorphic rocks proposed by the SCMR, and lays out the general principles which were used by the SCMR when defining terms for metamorphic rocks, their features, conditions of formation and processes. Subsequent papers discuss and present more detailed terminology for particular metamorphic rock groups and processes. The SCMR recognises the very wide usage of some rock names (for example, amphibolite, marble, hornfels) and the existence of many name sets related to specific types of metamorphism (for example, high P/T rocks, migmatites, impactites).
    [Show full text]
  • Stratigraphic Signature of the Late Palaeozoic Ice Age in the Parmeener Supergroup of Tasmania, SE Australia, and Inter- Regional Comparisons
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Earth and Atmospheric Sciences, Department Papers in the Earth and Atmospheric Sciences of 2010 Stratigraphic signature of the late Palaeozoic Ice Age in the Parmeener Supergroup of Tasmania, SE Australia, and inter- regional comparisons Christopher R. Fielding University of Nebraska-Lincoln, [email protected] Tracy D. Frank University of Nebraska-Lincoln, [email protected] John L. Isbell University of Wisconsin-Milwaukee, [email protected] Lindsey C. Henry University of Wisconsin-Milwaukee Eugene W. Domack Hamilton College, Clinton, NY, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Fielding, Christopher R.; Frank, Tracy D.; Isbell, John L.; Henry, Lindsey C.; and Domack, Eugene W., "Stratigraphic signature of the late Palaeozoic Ice Age in the Parmeener Supergroup of Tasmania, SE Australia, and inter-regional comparisons" (2010). Papers in the Earth and Atmospheric Sciences. 263. https://digitalcommons.unl.edu/geosciencefacpub/263 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Published in Palaeogeography, Palaeoclimatology, Palaeoecology 298 (2010), pp. 70–90; doi:10.1016/j.palaeo.2010.05.023 Copyright © 2010 Elsevier B.V. Used by permission Submitted September 25, 2009; revised April 20, 2010; accepted May 20, 2010; published online June 1, 2010. Stratigraphic signature of the late Palaeozoic Ice Age in the Parmeener Supergroup of Tasmania, SE Australia, and inter-regional comparisons Christopher R.
    [Show full text]
  • Geology of Virginia
    COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE BASSETT QUADRANGLE, VIRGINIA WILTIAM 5. HENIKA REPORT OF INVESTIGATIONS 26 VIRGINIA DIVISION OF MII\ERAL RESOURCES James L. Calver Commissioner of Mineral Resourr:es and State Geologisl CHARLOTTESVITLE, VIRGINIA 1971 COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE BASSETT QUADRANGLE, VIRGINIA WILLIAM S. HENIKA REPORT OF INVESTIGATIONS 26 VIRGINIA DIVISION OF MINERAL RESOURCES James L. Calver Commissioner of Mineral Resources and Staie Geologist CHARLOTTESVILLE. VIRGINIA 1571 CorruoNweerrs on VrncrNre Dnpax.tuer.rr op Puncnlsps eNl Supprv RtcsvroNo 197 t Portions of this publication may be quoted if credit is given to the Virginia Division of Mineral Resources. It is recommended that reference to this report be made in the following form: Henika, William S., 1971, Geology of the Bassett quadrangle, Virginia: Virginia Division of Mineral Resources Rept. lnv.26, 43 p. DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia MmvrN M. Surnnnrttto, Director Cnenrrs A. CnmsropHERsEN, Deputy Director A. S. Rlcnnr,, JR., Executive Assistant BOARD ANonEw A. Fenr,ev, Danville, Chairmen WrrrHu H. KtNc, Burkeville, Vice Chairman Mlron T. BrNror.r, Suffolk Josepg C. Canren, Jn., Richmond Aoorr U. HoNrara, Richmond CreuoB A. Jrssur, Charlottesville Geonce C. McGuun, Middleburg Rosenr PlrrensoN, Charlottesville Coruus SNvosn, Accomac Wrtr,rau H.
    [Show full text]
  • Lab 5: Textures and Identification of Metamorphic Rocks
    LAB 5: TEXTURES AND IDENTIFICATION OF METAMORPHIC ROCKS OBJECTIVES: 1) to become familiar with textures characteristic of metamorphic rocks; 2) to become familiar with properties important in recognizing and classifying metamorphic rocks; 3) to become familiar with the mineralogy of common metamorphic rocks. INTRODUCTION: Metamorphic rocks are formed from pre-existing rocks by recrystallization in the solid state under the effects of heat, pressure, shearing (grinding), or replacement by materials (ions) dissolved in water. They are classified on the basis of texture (foliated vs. non-foliated), grain-size, and mineral composition. Texture: Metamorphic rocks may have either foliated (layered) or non-foliated texture. Foliated texture is a pervasive layering caused by compositional layering or by the parallel orientation of platy (e.g, mica) or elongate (e.g., amphibole) mineral grains. Foliation is caused by recrystallization under directed (compressional) stress. However, if the rock lacks platy or elongate minerals, it will not develop foliation even though it recrystallized under very great pressure (examples are marble and quartzite). Grain size: Grain size reflects pressure and temperature conditions of metamorphism. Generally, higher temperatures and pressures (higher grades of metamorphism) favor larger grains, and lower temperatures and pressures favor smaller grains. Mineral composition: Mineral composition reflects the composition of the parent rock and the pressure and temperature conditions under which the metamorphism occurred. See Marshak p. 241-244 for discussion of metamorphic grades and for the index minerals used to identify them. Classification: Foliated metamorphic rocks: Grain size is the main basis for classification of foliated metamorphic rocks. Slates are very fine-grained, well-foliated (very well-layered) rocks.
    [Show full text]
  • Relationship Between Rock Type, Metamorphic Grade
    Canadian Mineralogist Vol. 25, pp. 485-498(1987) RELATIONSHIPBETWEEN ROCK TYPE, METAMORPHIC GRADE, AND FLUID- PHASECOMPOSITION IN THE GRENVILLESUPERGROUP, LIMERICKTOWNSHIP, ONTARIO P. JAMES LgANDERSON Depaftmentof Geologyand GeologicalEngineering, Colorado School of Mines, Goldm, Colorado8M01, U.S.A. JAMES L. MUNOZ Depafimentof GeologicalSciences, University of Colorado,Boulder, Colorado80309-0250, U.S.A, ABSTRACT entre535 et 550'C dansles marbres et 402et 543"Cou plus dans les lithologies pauvres en carbonate. La valerir de The srudy area in Limerick Township in the southern X(CO) seraitentre 0,45 et 0.55 dansles marbreset moins Grenville Province consistsof a sequenceof late Proterozoic de 0. l0 dansles milieux pauvresen carbonate.La relatlon metabasalts,noncalcareous and calcareousquartzofeld- entre degr€de m6tamorphismeet lithologie refldte la dimi spatlfc granofels,and marblesintruded by two gabbro com- nution du X(CO) du marbre vers les unit€s moins riches plexes.During the Grenville Orogeny,metamorphism of en calcaire.Cette relation pourrait 6tre attribude l) d un marble producedassemblages that are below the titanite, tamponnageinterne de la phasefluide par lesr6actions iso- actinolite - calcite,and hornblende- K-feldsparisograds, gradiquesi des valeurs 6levdesde X(CO) dans les mar- but above the hornblende - K-feldspar isograd in the bres et des valeurs inf6rieures dans les unit6s pauvres en quartzofeldspathicunits and amphibolitss. Calcite-dolomite carbonate, ou 2) d un tamponnagedes fluides i desvaleurs and two-feldspargeothennometry, and calculationof the faibles de X(CO) par les r€actionsisogradiques suite i displacementof intersectingequilibria due to solid-solution, l'infiltration de fluides aqueux au travers des unit€s pau- bracket equilibrium temperaturesbetween 535 and 550'C vres ou sanscarbonate.
    [Show full text]