Plates & Regions

Total Page:16

File Type:pdf, Size:1020Kb

Plates & Regions North American Perspectives II: Appalachians (Paleozoic) Processes in Structural Geology & Tectonics Ben van der Pluijm © WW Norton+Authors, unless noted otherwise 4/25/2016 4:33 PM We Discuss … North American Perspectives II: Appalachians (Paleozoic) • Opening and closing of Proto-Atlantic (Iapetus and Rheic Oceans) based on paleogeography and paleomagnetism. • Appalachians preserve Laurentian (N America) and Gondwanan (Africa) margins, separated by a belt with ocean remnants (ophiolites, arcs, islands/plateaus, subduction complexes), best preserved in the northern segment. • Southern Appalachians dominated by Late Paleozoic deformation from final ocean basin closure, resulting in large overthrusts that are exposed in tectonic windows. • Curved mountain belts (oroclines) and salients/recesses (irregular plate margins) are explored. • Paleogeographic reconstruction shows Appalachian history from late Precambrian ocean opening to closing. Eastern N America ©PSG&T 2 Geologic Timescale (GSA, v.4, 2012) Eastern N America ©PSG&T 3 US and Canadian Appalachians Eastern N America ©PSG&T 5 The Appalachians and Caledonides: Birthplace of Past Plate Tectonics Eastern N America ©PSG&T 6 Paleogeography: Fossil Biozones Paleozoic Paleogeography: Paradoxides davidis intermedius • Fossil biomes (Specimen FMNH PE 28971-B, • Paleomagnetism 240mm or 9.25 inches long) • No ocean floor magnetic anomalies Eastern N America ©PSG&T 7 History of Proto-Atlantic Oceans (Iapetus and Rheic Oceans) Chris Scotese’s PaleoMap Project http://www.scotese.com/ Eastern N America ©PSG&T 8 Appalachian-Caledonian belt and US Appalachians Eastern N America ©PSG&T 9 Zones of the Appalachian Collisional Orogen N America Remnants of Proto-Atlantic (Arcs, Islands, Plateaus) Africa (Gondwana) Eastern N America ©PSG&T 10 Northern Appalachians (Lower and Middle Paleozoic) N America Proto-Atlantic Remnants Africa (Gondwana) Eastern N America ©PSG&T 11 Ophiolite Obduction (Ordovician) Table Mountain peridotite (Gros Morne, Newfoundland) Eastern N America ©PSG&T 12 Southern Appalachians (3D) Eastern N America ©PSG&T 13 3D Geology: Seismic reflection profiling See Chapter 15: Geophysical Imaging Eastern N America ©PSG&T 14 COCORP in the S Appalachians Geological map of southern Appalachians with locations of COCORP seismic reflection profiles. Cook and Vasudevan, 2006 Eastern N America ©PSG&T 15 Alleghanian (Upper Paleozoic) Collision S Appalachian detachment and Grandfather Mountain Window Eastern N America ©PSG&T 16 Extra: Radiometric (Ar) Dating of Appalachian Faults Hnat, 2014 Eastern N America ©PSG&T 17 Orogenic Curvature along the Appalachians Eastern N America ©PSG&T 18 Curved Orogens (=Oroclines): the Pennsylvania Salient From NASA Gray and Stamatakos, 1997 Valley and Ridge, PA • Origin and meaning of curved orogens (Carey’s “orocline”; 1955) • Primary vs. secondary curvature Eastern N America ©PSG&T PA Salient, 19 Oroclines Tennessee Salient Marshak, 2004 Hnat, 2011 Eastern N America ©PSG&T 20 Paleogeography through Paleomagnetism Paleo-inclination: distance from pole: tan(I) = 2 cotan(L) Paleo-declination: rotation relative to (averaged) pole Note: reversal indeterminacy Eastern N America ©PSG&T 21 Oceanic Terranes and Collision (Paleomagnetic evidence) MacNiocaill et al., 1997 Eastern N America ©PSG&T 22 Pangea Family Tree Pangea Early Triassic, ~237 Ma (from www.scotese.com) Scotese, 2004 Eastern N America ©PSG&T 23 Opening and Closing of Proto-Atlantic (Iapetus) Ocean Chris Scotese Eastern N America ©PSG&T 24.
Recommended publications
  • Lines in Paradoxides Forchhammeri - Evidence of Lateral Inhibition
    Spatial organization of tubercles and terrace lines in Paradoxides forchhammeri - evidence of lateral inhibition 0YVIND HAMMER Hammer, 0. 2000. Spatial organization of tubercles and terrace lines in Paradoxides forchhammeri - evidence of lateral inhibition. -Acta Palaeontologica Polonica 45,3, 251-270. Spatial statistics on the positions of trilobite tubercles indicate the existence of a develop- mental spacing mechanism. Similar spacing between sensory bristles, due to lateral inhi- bition, is well known in insects, and the genetic basis for these patterns has been thor- oughly studied. Tubercles (granules) in the Middle Cambrian trilobite Paradoxides forchhammeri are spaced out, but otherwise randomly positioned. Assuming that similar genetic principles are in operation for the positioning of peripheral neuronal elements in all arthropods, it can even be speculated that genes with functions similar to Delta, Notch, achaete and scute were active in trilobite cuticular patterning. Also, in f? forchhammeri, terrace lines (ridges) seem to display transitions into granulation, indicating that these two types of structure share an underlying pattern formation mechanism. Key words : Trilobites, tubercles, terrace lines, pattern formation, evolution, Notch. 0yvind Hammer [[email protected]],Paleontological Museum, University of Oslo, Sars gt. 1, 0562 Oslo, Norway. Introduction Trilobite tubercles (Starrmer 1980; Wilmot 1991; Whittington 1997) are cuticular structures that may have formed in connection with sensory devices such as setae or other mechano- or chemoreceptors. As such, they may be compared with sensilla in the cuticles of other arthropods (Starrmer 1980). In particular, the molecular basis for the development of spaced bristles in Drosophila has been the subject of extensive re- search (reviewed in Simpson et al.
    [Show full text]
  • The Evolution of Trilobite Body Patterning
    ANRV309-EA35-14 ARI 20 March 2007 15:54 The Evolution of Trilobite Body Patterning Nigel C. Hughes Department of Earth Sciences, University of California, Riverside, California 92521; email: [email protected] Annu. Rev. Earth Planet. Sci. 2007. 35:401–34 Key Words First published online as a Review in Advance on Trilobita, trilobitomorph, segmentation, Cambrian, Ordovician, January 29, 2007 diversification, body plan The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The good fossil record of trilobite exoskeletal anatomy and on- 10.1146/annurev.earth.35.031306.140258 togeny, coupled with information on their nonbiomineralized tis- Copyright c 2007 by Annual Reviews. sues, permits analysis of how the trilobite body was organized and All rights reserved developed, and the various evolutionary modifications of such pat- 0084-6597/07/0530-0401$20.00 terning within the group. In several respects trilobite development and form appears comparable with that which may have charac- terized the ancestor of most or all euarthropods, giving studies of trilobite body organization special relevance in the light of recent advances in the understanding of arthropod evolution and devel- opment. The Cambrian diversification of trilobites displayed mod- Annu. Rev. Earth Planet. Sci. 2007.35:401-434. Downloaded from arjournals.annualreviews.org ifications in the patterning of the trunk region comparable with by UNIVERSITY OF CALIFORNIA - RIVERSIDE LIBRARY on 05/02/07. For personal use only. those seen among the closest relatives of Trilobita. In contrast, the Ordovician diversification of trilobites, although contributing greatly to the overall diversity within the clade, did so within a nar- rower range of trunk conditions.
    [Show full text]
  • Smithsonian Miscellaneous Collections
    SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 53, NUMBER 6 CAMBRIAN GEOLOGY AND PALEONTOLOGY No. 6.-0LENELLUS AND OTHER GENERA OF THE MESONACID/E With Twenty-Two Plates CHARLES D. WALCOTT (Publication 1934) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION AUGUST 12, 1910 Zl^i £orb (gaitimovt (pnee BALTIMORE, MD., U. S. A. CAMBRIAN GEOLOGY AND PALEONTOLOGY No. 6.—OLENELLUS AND OTHER GENERA OF THE MESONACID^ By CHARLES D. WALCOTT (With Twenty-Two Plates) CONTENTS PAGE Introduction 233 Future work 234 Acknowledgments 234 Order Opisthoparia Beecher 235 Family Mesonacidas Walcott 236 Observations—Development 236 Cephalon 236 Eye 239 Facial sutures 242 Anterior glabellar lobe 242 Hypostoma 243 Thorax 244 Nevadia stage 244 Mesonacis stage 244 Elliptocephala stage 244 Holmia stage 244 Piedeumias stage 245 Olenellus stage 245 Peachella 245 Olenelloides ; 245 Pygidium 245 Delimitation of genera 246 Nevadia 246 Mesonacis 246 Elliptocephala 247 Callavia 247 Holmia 247 Wanneria 248 P.'edeumias 248 Olenellus 248 Peachella 248 Olenelloides 248 Development of Mesonacidas 249 Mesonacidas and Paradoxinas 250 Stratigraphic position of the genera and species 250 Abrupt appearance of the Mesonacidse 252 Geographic distribution 252 Transition from the Mesonacidse to the Paradoxinse 253 Smithsonian Miscellaneous Collections, Vol. 53, No. 6 232 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. 53 Description of genera and species 256 Nevadia, new genus 256 weeksi, new species 257 Mcsonacis Walcott 261 niickwitzi (Schmidt) 262 torelli (Moberg) 264 vermontana
    [Show full text]
  • Early and Middle Cambrian Trilobites from Antarctica
    Early and Middle Cambrian Trilobites From Antarctica GEOLOGICAL SURVEY PROFESSIONAL PAPER 456-D Early and Middle Cambrian Trilobites From Antarctica By ALLISON R. PALMER and COLIN G. GATEHOUSE CONTRIBUTIONS TO THE GEOLOGY OF ANTARCTICA GEOLOGICAL SURVEY PROFESSIONAL PAPER 456-D Bio stratigraphy and regional significance of nine trilobite faunules from Antarctic outcrops and moraines; 28 species representing 21 genera are described UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-190734 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 70 cents (paper cover) Stock Number 2401-2071 CONTENTS Page Page Abstract_ _ ________________________ Dl Physical stratigraphy______________________________ D6 I&troduction. _______________________ 1 Regional correlation within Antarctica ________________ 7 Biostratigraphy _____________________ 3 Systematic paleontology._____-_______-____-_-_-----_ 9 Early Cambrian faunules.________ 4 Summary of classification of Antarctic Early and Australaspis magnus faunule_ 4 Chorbusulina wilkesi faunule _ _ 5 Middle Cambrian trilobites. ___________________ 9 Chorbusulina subdita faunule _ _ 5 Agnostida__ _ _________-____-_--____-----__---_ 9 Early Middle Cambrian f aunules __ 5 Redlichiida. __-_--------------------------_---- 12 Xystridura mutilinia faunule- _ 5 Corynexochida._________--________-_-_---_----_
    [Show full text]
  • Re-Evaluation of the Stratigraphically Important Olenellid Trilobite Holmia Cf. Mobergi from the Cambrian Series 2, Stage 3
    NORWEGIAN JOURNAL OF GEOLOGY Vol 99 Nr. 1 https://dx.doi.org/10.17850/njg99-1-04 Re-evaluation of the stratigraphically important olenellid trilobite Holmia cf. mobergi from the Cambrian Series 2, Stage 3 and its implications for the lower Cambrian stratigraphy in the Mjøsa area, Norway Magne Høyberget1, Jan Ove R. Ebbestad2 & Bjørn Funke3 1Rennesveien 14, N–4513 Mandal, Norway. 2Museum of Evolution, Uppsala University, Norbyvägen 16, SE–752 36 Uppsala, Sweden. 3Gjelleråsveien 10, N–1481 Hagan, Norway. E-mail corresponding author (Magne Høyberget): [email protected] The olenellid trilobite Holmia cf. mobergi, known from a single cephalon in the upper lower Cambrian strata from a river section in Flagstadelva, Hamar, has played a significant stratigraphic role in interpreting the lower Cambrian informal Series 2, Stage 3 in the Mjøsa area, Norway, since its discovery in the early 1950s. It was considered one of the oldest trilobite taxa in the lower Cambrian of Scandinavia, but the stratigraphic level and biozonation of the cephalon were problematic and a matter of discussion for decades. Moreover, organic-walled microfossil biostratigraphy questioned the supposed age of the trilobite. New specimens of this taxon collected from the type locality show that the species occurs at a different stratigraphic level than first reported, prompting a new description of the species and a re-evaluation of the taxon’s biostratigraphic significance. Holmia cf. mobergi is compared with new and well-preserved topotype material of Holmia inusitata, a very rare taxon hitherto known from one single outcrop in an autochthonous setting in Norway. Holmia cf.
    [Show full text]
  • An Appraisal of the Great Basin Middle Cambrian Trilobites Described Before 1900
    An Appraisal of the Great Basin Middle Cambrian Trilobites Described Before 1900 By ALLISON R. PALMER A SHORTER CONTRIBUTION TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 264-D Of the 2ty species described prior to I(?OO, 2/ are redescribed and 2C} refigured, and a new name is proposedfor I species UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1 (paper cover) CONTENTS Page Abstract..__________________________________ 55 Introduction ________________________________ 55 Original and present taxonomic names of species. 57 Stratigraphic distribution of species ____________ 57 Collection localities._________________________ 58 Systematic descriptions.______________________ 59 Literature cited____________________________ 82 Index __-_-__-__---_--______________________ 85 ILLUSTRATIONS [Plates 13-17 follow page 86] PLATE 13. Agnostidae and Dolichometopidae 14. Dorypygidae 15. Oryctocephalidae, Dorypygidae, Zacanthoididae, and Ptychoparioidea 16. Ptychoparioidea 17. Ptychoparioidea FIGUBE 3. Index map showing collecting localities____________________________ . Page 56 in A SHORTER CONTRIBUTION TO GENERAL GEOLOGY AN APPRAISAL OF THE GREAT BASIN MIDDLE CAMBRIAN TRILOBITES DESCRIBED BEFORE 1900 By ALLISON R. PALMER ABSTRACT the species and changes in their generic assignments All 29 species of Middle Cambrian trilobites
    [Show full text]
  • Boletin Del Instituto Estudios Asturianos
    DIPUTACION PROVINCIAL DE OVIEDO BOLETIN DEL INSTITUTO DE ESTUDIOS ASTURIANOS (SUPLEMENTO DE CIENCIAS) Año I OVIEDO Núm. II SUMARIO Páginas Problemas y posibilidades de la agricultura asturiana, por Gabino Figar Alvarez .................................................................................. 3 Estudio geológico de las sierras de la Coruxera, la Mostayal y Monsacro, por N. Llopis Lladó ..................................................................... 29 El servicio geológico de las “hulleras de la cuenca del norte y del paso de Calais (H. B. N. P. C.)”.—Francia, por J. A. M ar­ tínez A lvarez ............................................................................................................. 159 B ibliografía crítica .....................................*r.. ............... .................. ................171 Biblioteca geológica de A sturias .................................................................180 Una especie forestal, que interesa introducir en los- montes de Asturias, por José Javier Nicolás Isasa ........................................................ ...193 DIPUTACION PROVINCIAL DE OVIEDO BOLETIN DEL INSTITUTO DE ESTUDIOS ASTURIANOS (SUPLEMENTO DE CIENCIAS) Año I OVIEDO Núm; 11 Depósito Legal. O 43—1958 IMPRENTA "LA CRUZ".- SAN VICENTE. 8.—OVIEDO PROBLEMAS Y POSIBILIDADES DE LA AGRICULTURA ASTURIANA POR GABINO FIGAR ALVAREZ INGENIERO AGRONOMO INTRODUCCION Dentro del conjunto de la Economía Nacional de marcado signo agrícola, con cerca del 50 % de la población activa dedi­ cada a la agricultura,
    [Show full text]
  • Th TRILO the Back to the Past Museum Guide to TRILO BITES
    With regard to human interest in fossils, trilobites may rank second only to dinosaurs. Having studied trilobites most of my life, the English version of The Back to the Past Museum Guide to TRILOBITES by Enrico Bonino and Carlo Kier is a pleasant treat. I am captivated by the abundant color images of more than 600 diverse species of trilobites, mostly from the authors’ own collections. Carlo Kier The Back to the Past Museum Guide to Specimens amply represent famous trilobite localities around the world and typify forms from most of the Enrico Bonino Enrico 250-million-year history of trilobites. Numerous specimens are masterpieces of modern professional preparation. Richard A. Robison Professor Emeritus University of Kansas TRILOBITES Enrico Bonino was born in the Province of Bergamo in 1966 and received his degree in Geology from the Depart- ment of Earth Sciences at the University of Genoa. He currently lives in Belgium where he works as a cartographer specialized in the use of satellite imaging and geographic information systems (GIS). His proficiency in the use of digital-image processing, a healthy dose of artistic talent, and a good knowledge of desktop publishing software have provided him with the skills he needed to create graphics, including dozens of posters and illustrations, for all of the displays at the Back to the Past Museum in Cancún. In addition to his passion for trilobites, Enrico is particularly inter- TRILOBITES ested in the life forms that developed during the Precambrian. Carlo Kier was born in Milan in 1961. He holds a degree in law and is currently the director of the Azul Hotel chain.
    [Show full text]
  • Paradoxides Œlandicus Beds of Öland, with the Account of a Diamond
    SVERIGES GEOLOGISKA UNDERSÖKNING SER. c. Avhandlingar och uppsatser. N:o 394· ÅRSBOK 30 (1936) N:o 1. PARADOXIDEs CELANDICUS BEDS OF ÖLAND WITH THE ACCOUNT OF A DIAMOND BORING THROUGH THE CAMBRIAN AT MOSSBERGA BY A. H. WESTERGÅRD Witlt Twelve Plates Pris 3:- kr. STOCKHOLM 1936 KUNGL. BOKTRYCKERIET. P. A. NORSTEDT & SÖNER 36!789 SVERIGES GEOLOGISKA UNDERS ÖKNING SER. c. Avhandlingar och uppsatser. N:o 394· ÅRSBOK 30 (1936) N:o r. PARADOXIDEs CELANDICUS BEDS OF ÖLAND WITH THE ACCOUNT OF A DIAMOND BORING THROUGH THE CAMBRIAN AT MOSSBERGA BY A. H. WESTERGÅRD With Twelve Plates STOCKI-IOLM 1936 KUNGL. BOKTRYCKERIET. P. A. NORSTEDT & SÖNER CONTENT S. Page I. A Diamond Boring through the Cambrian at Mossberga . 5 Quartzite . ... 5 Lower Cambrian Deposits and the Sub-Cambrian Land Surface 7 Paradoxides oolandicus Beds !3 Comparison of the Mossberga and Borgholm Profiles 16 II. Paradoxides oolandicus Beds of Öland . 17 Introduction and History . 17 Distribution, Thickness, and Stratigraphy 19 Acknowledgements 22 Fauna ..... 22 Brachiopoda . 22 M icromitra . 2 2 Lingulella 23 Acrothele . 24 Acrotreta .. 24 Orthoid brachiopod 25 Gastropoda 25 ffilandia .. 25 Hyolithidae 26 Trilobita . 27 Condylopyge 27 Peronopsis 28 Agnostus . 29 Calodiscus 30 Burlingia 32 Paradoxides 33 Ontogeny of Paradoxides 45 Ellipsocephalus 56 Bailiella . 58 Solenopleura . 59 Phyllocarida. Hymenocaris (?) 61 Geographical and Stratigraphical Distribution of the Fauna Elements 62 Bibliography . 64 Explanation of Plates . 67 I. A Diamond Boring through the Cambrian at Mossberga. As a part of the work carried out by the Electrical Prospecting Co. (A.-B. Elektrisk Malmletning) in order to search for gas in the Lower Cambrian of Öland, a deep boring was made in the autumn of 1933 into a little flat dome at Mossberga, about 12 km S of Borgholm.
    [Show full text]
  • 2105248121101000.Pdf
    ELABORACIÓN DE LA CARTOGRAFÍA GEOLÓGICA DE UN CONJUNTO DE PLANCHAS A ESCALA 1:100.000 UBICADAS EN CUATRO BLOQUES DEL TERRITORIO NACIONAL IDENTIFICADOS POR EL SERVICIO GEOLÓGICO COLOMBIANO GRUPO 2: ZONAS SUR A Y SUR B GEOLOGÍA DE LA PLANCHA 285 SAN MARTIN Escala 1: 100.000 Contrato Nº 512 - 2013 MEMORIA EXPLICATIVA Bogotá, D.C., Septiembre de 2015 ELABORACIÓN DE LA CARTOGRAFÍA GEOLÓGICA DE UN CONJUNTO DE PLANCHAS A ESCALA 1:100.000 UBICADAS EN CUATRO BLOQUES DEL TERRITORIO NACIONAL IDENTIFICADOS POR EL SERVICIO GEOLÓGICO COLOMBIANO GRUPO 2: ZONAS SUR A Y SUR B GEOLOGÍA DE LA PLANCHA 326 VISTA HERMOSA Escala 1: 100.000 Contrato Nº 512 - 2013 MEMORIA EXPLICATIVA Elaborado por: UT G&H Director Proyecto Geólogo Fernando Buchely Gerente Administrativo Geólogo PhD. Luís Gómez Asesor Estratigrafía Geólogo PhD. Mario Moreno-Sánchez Asesores Geología Estructural Geólogo PhD. Luís Gómez y Geólogo MSc. Gustavo Hincapié Coordinador Técnico Geólogo José Buitrago Fotogeólogo y Geomorfólogo Geólogo MSc. Alberto Cristancho Coordinador de Campo Geólogo MSc. Juan Manuel Aranzazu Hernández Geólogos de Campo Alejandro Patiño Carlos Quiñonez Mario Moreno José Buitrago Coordinador Social Antropólogo Mauricio Rojas Dirección SIG Talía Berg Coordinadores SIG Lucrecia Nota David Culebra Coordinación de Edición Carolina López Oscar Arias Bogotá, D.C., Septiembre de 2015 Servicio Geológico Colombiano CONTENIDO Pág. RESUMEN 18 ABSTRACT ................................................................................................................... 19 1. INTRODUCCIÓN
    [Show full text]
  • Early Middle Cambrian Fauna from Rogaland, Sw Norway
    NORSK GEOLOGISK TIDSSKRIFT 30 13 EARLY MIDDLE CAMBRIAN FAUNA FROM ROGALAND, SW NORWAY (Pm·udox:ides oelandicus sta(fe = le a) BY GUNNAR HENNINGSMOEN Contents. Abstraot . .. .. 13 Hyolitha . 22 Introduction l� Hyolithes obesus Holm 22 The fossils . 15 Orthotheca teretiuscula (Lin­ Trilobitae . 15 narsson) . 22 Peronopsis faHax (Linnarsson) 15 Portfera . 23 Paradoxides pinus Westergård 16 Pootospongia? sp. 23 Paradoxides oelandicus Sjogren 16 Chancelloria sp. 23 Ptychoparia anderseni sp. n. 17 Problematioa . 24 Brachiopoda . lfl Discussion of fauna . 24 Orthoid brachiopod . 19 List of fossils from the Paradox­ LinguleUa sp. .. ... .. .. 19 ides oelandicus sta@e in Norway 26 Acrothele (Redlichella) granu­ Kambriske fos,siler fra Rogaland 28 lata Linnarsson . 20 References . 29 Acrotreta socialis v. Seebach. 21 Explanation of plates . 32 Abst rac t. Cambrian fossils have, for the first time, been found on the west coast of Norway. They were found by cand. real. Bjørn Ander­ sen in 1949 at Ritland, Hjelmeland district, Rogaland County. The fossils occur in autochthonous dark shale, and belong to the Paradoxides oelandicus stage (Early Middle Cambrian) . Trilobites (including Ptychoparia anderseni sp. n.) , brachiopods, hyolithids, sponge needles, and problematica (including archaeocyathids?) have been collected. The absence of this stage in the autochthonous series in the Oslo region, as well as in the Swedish areas Vastengotland and Scania, suggests a land mass in these areas in P. oelandicus time, bordered to the north by the Caledonian geosyncline, and to the east by a shallow sea. Introduction. Whilc geologicaHy mapping in the northern part of Rogaland County (SW Norway) in the summer 1949, cand. real. Bjørn Ander­ sen found a piece of shale containing the impression of a trilobite (Paradoxides pinus, pl.
    [Show full text]
  • Redalyc.METAGABRO DEL ARIARI, PLUTONISMO MORB
    Boletín de Geología ISSN: 0120-0283 [email protected] Universidad Industrial de Santander Colombia Toro-Toro, Luz Mary; Moreno-Sánchez, Mario; Gómez-Cruz, Arley METAGABRO DEL ARIARI, PLUTONISMO MORB, CORDILLERA ORIENTAL DE COLOMBIA Boletín de Geología, vol. 36, núm. 2, julio-diciembre, 2014, pp. 15-24 Universidad Industrial de Santander Bucaramanga, Colombia Disponible en: http://www.redalyc.org/articulo.oa?id=349632714001 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Boletín de Geología ISSN: 0120-0283 Vol. 36, N° 2, julio-diciembre de 2014 URL: boletindegeologia.uis.edu.co METAGABRO DEL ARIARI, PLUTONISMO MORB, CORDILLERA ORIENTAL DE COLOMBIA Luz Mary Toro-Toro1; Mario Moreno-Sánchez1; Arley Gómez-Cruz1 Forma de citar: Toro-Toro, L.M., Moreno-Sánchez, M., y Gómez-Cruz, A. 2014. Metagabro del Ariari, Plutonismo MORB, Cordillera Oriental de Colombia. Boletín de Geología, 36 (2): 15-24. RESUMEN En este trabajo se dan a conocer las características petrográficas y geoquímicas del Metagabro del Ariari que aflora sobre la quebrada La Cristalina, al este del municipio de El Dorado, departamento del Meta en la Cordillera Oriental. Este cuerpo desarrolla metamorfismo de bajo grado en la facies esquisto verde sin obliterar la textura original de la roca. La composición de las rocas del Metagabro del Ariari indican una afinidad toleítica (gabros; SiO2 = 46,93 -47,69 wt%, FeO +MgO = 18,42 -19,13 wt% y K2O+Na2O= 4,16 -10,42wt%), relaciones Nb/Y = 0,13-0,17 con patrones de REE caracterizados por LREE ligeramente empobrecidos y patrones menos fraccionados y relativamente planos de tierras raras pesadas (HREE).
    [Show full text]