Geologic Report for the Navarin Basin Planning Area, Bering Sea, A1 Aska
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Geologic History of Siletzia, a Large Igneous Province in the Oregon And
Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Wells, R., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., & Wooden, J. (2014). Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot. Geosphere, 10 (4), 692-719. doi:10.1130/GES01018.1 10.1130/GES01018.1 Geological Society of America Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Downloaded from geosphere.gsapubs.org on September 10, 2014 Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Ray Wells1, David Bukry1, Richard Friedman2, Doug Pyle3, Robert Duncan4, Peter Haeussler5, and Joe Wooden6 1U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025-3561, USA 2Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, 6339 Stores Road, University of British Columbia, Vancouver, BC V6T 1Z4, Canada 3Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East West Road, Honolulu, Hawaii 96822, USA 4College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA 5U.S. Geological Survey, 4210 University Drive, Anchorage, Alaska 99508-4626, USA 6School of Earth Sciences, Stanford University, 397 Panama Mall Mitchell Building 101, Stanford, California 94305-2210, USA ABSTRACT frames, the Yellowstone hotspot (YHS) is on southern Vancouver Island (Canada) to Rose- or near an inferred northeast-striking Kula- burg, Oregon (Fig. -
Heartland of German History
Travel DesTinaTion saxony-anhalT HEARTLAND OF GERMAN HISTORY The sky paThs MAGICAL MOMENTS OF THE MILLENNIA UNESCo WORLD HERITAGE AS FAR AS THE EYE CAN SEE www.saxony-anhalt-tourism.eu 6 good reasons to visit Saxony-Anhalt! for fans of Romanesque art and Romance for treasure hunters naumburg Cathedral The nebra sky Disk for lateral thinkers for strollers luther sites in lutherstadt Wittenberg Garden kingdom Dessau-Wörlitz for knights of the pedal for lovers of fresh air elbe Cycle route Bode Gorge in the harz mountains The Luisium park in www.saxony-anhalt-tourism.eu the Garden Kingdom Dessau-Wörlitz Heartland of German History 1 contents Saxony-Anhalt concise 6 Fascination Middle Ages: “Romanesque Road” The Nabra Original venues of medieval life Sky Disk 31 A romantic journey with the Harz 7 Pomp and Myth narrow-gauge railway is a must for everyone. Showpieces of the Romanesque Road 10 “Mona Lisa” of Saxony-Anhalt walks “Sky Path” INForMaTive Saxony-Anhalt’s contribution to the history of innovation of mankind holiday destination saxony- anhalt. Find out what’s on 14 Treasures of garden art offer here. On the way to paradise - Garden Dreams Saxony-Anhalt Of course, these aren’t the only interesting towns and destinations in Saxony-Anhalt! It’s worth taking a look 18 Baroque music is Central German at www.saxony-anhalt-tourism.eu. 8 800 years of music history is worth lending an ear to We would be happy to help you with any questions or requests regarding Until the discovery of planning your trip. Just call, fax or the Nebra Sky Disk in 22 On the road in the land of Luther send an e-mail and we will be ready to the south of Saxony- provide any assistance you need. -
P1616 Text-Only PDF File
A Geologic Guide to Wrangell–Saint Elias National Park and Preserve, Alaska A Tectonic Collage of Northbound Terranes By Gary R. Winkler1 With contributions by Edward M. MacKevett, Jr.,2 George Plafker,3 Donald H. Richter,4 Danny S. Rosenkrans,5 and Henry R. Schmoll1 Introduction region—his explorations of Malaspina Glacier and Mt. St. Elias—characterized the vast mountains and glaciers whose realms he invaded with a sense of astonishment. His descrip Wrangell–Saint Elias National Park and Preserve (fig. tions are filled with superlatives. In the ensuing 100+ years, 6), the largest unit in the U.S. National Park System, earth scientists have learned much more about the geologic encompasses nearly 13.2 million acres of geological won evolution of the parklands, but the possibility of astonishment derments. Furthermore, its geologic makeup is shared with still is with us as we unravel the results of continuing tectonic contiguous Tetlin National Wildlife Refuge in Alaska, Kluane processes along the south-central Alaska continental margin. National Park and Game Sanctuary in the Yukon Territory, the Russell’s superlatives are justified: Wrangell–Saint Elias Alsek-Tatshenshini Provincial Park in British Columbia, the is, indeed, an awesome collage of geologic terranes. Most Cordova district of Chugach National Forest and the Yakutat wonderful has been the continuing discovery that the disparate district of Tongass National Forest, and Glacier Bay National terranes are, like us, invaders of a sort with unique trajectories Park and Preserve at the north end of Alaska’s panhan and timelines marking their northward journeys to arrive in dle—shared landscapes of awesome dimensions and classic today’s parklands. -
A Guide to 1.000 Foraminifera from Southwestern Pacific New Caledonia
Jean-Pierre Debenay A Guide to 1,000 Foraminifera from Southwestern Pacific New Caledonia PUBLICATIONS SCIENTIFIQUES DU MUSÉUM Debenay-1 7/01/13 12:12 Page 1 A Guide to 1,000 Foraminifera from Southwestern Pacific: New Caledonia Debenay-1 7/01/13 12:12 Page 2 Debenay-1 7/01/13 12:12 Page 3 A Guide to 1,000 Foraminifera from Southwestern Pacific: New Caledonia Jean-Pierre Debenay IRD Éditions Institut de recherche pour le développement Marseille Publications Scientifiques du Muséum Muséum national d’Histoire naturelle Paris 2012 Debenay-1 11/01/13 18:14 Page 4 Photos de couverture / Cover photographs p. 1 – © J.-P. Debenay : les foraminifères : une biodiversité aux formes spectaculaires / Foraminifera: a high biodiversity with a spectacular variety of forms p. 4 – © IRD/P. Laboute : îlôt Gi en Nouvelle-Calédonie / Island Gi in New Caledonia Sauf mention particulière, les photos de cet ouvrage sont de l'auteur / Except particular mention, the photos of this book are of the author Préparation éditoriale / Copy-editing Yolande Cavallazzi Maquette intérieure et mise en page / Design and page layout Aline Lugand – Gris Souris Maquette de couverture / Cover design Michelle Saint-Léger Coordination, fabrication / Production coordination Catherine Plasse La loi du 1er juillet 1992 (code de la propriété intellectuelle, première partie) n'autorisant, aux termes des alinéas 2 et 3 de l'article L. 122-5, d'une part, que les « copies ou reproductions strictement réservées à l'usage privé du copiste et non destinées à une utilisation collective » et, d'autre part, que les analyses et les courtes citations dans un but d'exemple et d'illustration, « toute représentation ou reproduction intégrale ou partielle, faite sans le consentement de l'auteur ou de ses ayants droit ou ayants cause, est illicite » (alinéa 1er de l'article L. -
Kinematic Evolution of the Gulf of Mexico and Caribbean
Kinematic Evolution of the Gulf of Mexico and Caribbean James Pindell Tectonic Analysis, Ltd., Cokes, Barn, West Burton, West Sussex RH20 1HD, England Also: Dept. Earth Science, Rice University, Houston, Texas, USA Email: [email protected] Lorcan Kennan Tectonic Analysis, Ltd., Cokes, Barn, West Burton, West Sussex RH20 1HD, England Abstract We present a series of 14 updated tectonic reconstructions for the Gulf of Mexico and Caribbean region since the Jurassic, giving due attention to plate kinematic and palinspastic accuracy. Primary elements of the model are: 1) a re-evaluation of the Mesozoic break-up of Pangea, to better define the Proto-Caribbean passive margin elements, the geology and kinematics of the Mexican and Colombian intra-arc basins, and the nature of the early Great Caribbean Arc; 2) pre-Albian circum-Caribbean rock assemblages are reconstructed into a primitive, west-facing, Mexico-Antilles-Ecuador arc (initial roots of Great Caribbean Arc) during the early separation of North and South America; 3) the subduction zone responsible for Caribbean Cretaceous HP/LT metamorphic assemblages was initiated during an Aptian subduction polarity reversal of the early Great Arc; the reversal was triggered by a strong westward acceleration of the Americas relative to the mantle which threw the original arc into compression; 4) the same acceleration led to the Aptian-Albian onset of back-arc closure and “Sevier” orogenesis in Mexico, the western USA, and the northern Andes, making this a nearly hemispheric event which must have -
Paper Is Divided Into Two Parts
Earth-Science Reviews 140 (2015) 72–107 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Geologic and kinematic constraints on Late Cretaceous to mid Eocene plate boundaries in the southwest Pacific Kara J. Matthews a,⁎, Simon E. Williams a, Joanne M. Whittaker b,R.DietmarMüllera, Maria Seton a, Geoffrey L. Clarke a a EarthByte Group, School of Geosciences, The University of Sydney, NSW 2006, Australia b Institute for Marine and Antarctic Studies, University of Tasmania, TAS 7001, Australia article info abstract Article history: Starkly contrasting tectonic reconstructions have been proposed for the Late Cretaceous to mid Eocene (~85– Received 25 November 2013 45 Ma) evolution of the southwest Pacific, reflecting sparse and ambiguous data. Furthermore, uncertainty in Accepted 30 October 2014 the timing of and motion at plate boundaries in the region has led to controversy around how to implement a Available online 7 November 2014 robust southwest Pacific plate circuit. It is agreed that the southwest Pacific comprised three spreading ridges during this time: in the Southeast Indian Ocean, Tasman Sea and Amundsen Sea. However, one and possibly Keywords: two other plate boundaries also accommodated relative plate motions: in the West Antarctic Rift System Southwest Pacific fi Lord Howe Rise (WARS) and between the Lord Howe Rise (LHR) and Paci c. Relevant geologic and kinematic data from the South Loyalty Basin region are reviewed to better constrain its plate motion history during this period, and determine the time- Late Cretaceous dependent evolution of the southwest Pacific regional plate circuit. A model of (1) west-dipping subduction Subduction and basin opening to the east of the LHR from 85–55 Ma, and (2) initiation of northeast-dipping subduction Plate circuit and basin closure east of New Caledonia at ~55 Ma is supported. -
Chilopoden Und Diplopoden (Myriapoda) Des Bodetals
Hercynia N. F. 45 (2012): 145 –157 145 Chilopoden und Diplopoden (Myriapoda) des Bodetals. Beiträge zur Myriapodenfauna des Harzes. II. Karin Voigtländer und E. Norman Lindner 1 Abbildung und 6 Tabellen Abstract Voigtländer, K., Lindner, E. N.: Chilopods and diplopods of the Bode Gorge. Contributions to the myriapod fauna of the Harz Mountains. - Hercynia N. F. 45 (2012): 145 – 157. The millipede and centipede fauna of the Bode Gorge within Harz Mountains (Saxony-Anhalt) between Treseburg and Wendefurth including its plateau and upper shelf as well as the Luppbode Valley near All- rode was investigated using pitfall traps from 1997 to 2000. The catches were complemented by recent hand sampling. Altogether 15 chilopod and 22 diplopod species could be recorded. This is nearly the half of the known species inventory of Saxony-Anhalt. The occurrence of some rare species is discussed. The boulder scree slopes and the alder riparian forests are especially valuable and worthy of protection. Key words: Diplopoda, Chilopoda, pitfall trapping, rare species, red list, Saxony-Anhalt 1 Einführung Die vorliegenden Untersuchungen zur Diplopoden- und Chilopodenfauna des Bodetals stellen einen weiteren Beitrag zur Erforschung des Harzes dar, der bis in die jüngere Zeit kaum myriapodologisch untersucht worden ist. Schubart (1934) nennt lediglich sechs Fundorte für einige Diplopoden-Arten, darunter auch das Bodetal bei Thale. Mühlmann (1942) und von Broen et al. (1969) widmeten sich der Höhlenfauna. Eine Intensivierung erfuhren die Arbeiten erst im Zusammenhang mit dem vom Landesamt für Umweltschutz in den 1990er Jahren begonnenen und bis heute fortgeführten Programm zu gefähr- deten Biotoptypen des Landes Sachsen-Anhalt (Voigtländer 2003a, b) sowie durch die von der Na- tionalparkverwaltung Hochharz initiierten Untersuchungen zur Arthropodenfauna des Brockengebietes (Voigtländer 1999). -
Geological Survey of Denmark and Greenland Bulletin 26, 2012
GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN 26 • 2012 Review of Survey activities 2011 Edited by Ole Bennike, Adam A. Garde and W. Stuart Watt GEOLOGICAL SURVEY OF DENMARK AND GREENLAND MINISTRY OF CLIMATE, ENERGY AND BUILDING 1 Geological Survey of Denmark and Greenland Bulletin 26 Keywords Geological Survey of Denmark and Greenland, survey organisations, current research, Denmark, Greenland. Cover photographs from left to right 1. Retrieving a sediment core in Sermilik fjord, South-East Greenland. Photograph: Robert S. Fausto. 2. Field work in Vietnam. Photograph: Flemming Larsen. 3. This Danish beech forest on Fyn was farm land during the Iron Age. Photograph: Ole Bennike. 4. Small-scale miners in Nigeria. Worldwide, c. 100 million people depend on small-scale mining. Photograph: John Tychsen. Frontispiece: facing page In the summer of 2011, GEUS carried out extensive reconnaissance work in South-East Greenland. The aim is to assess the mineral potential of the region, which is one of the least known regions of Greenland. The geologist is panning stream sediments in order to separate heavy minerals, possibly including gold. Photograph: Jakob Lautrup. Chief editor of this series: Adam A. Garde Editorial board of this series: John A. Korstgård, Department of Geoscience, Aarhus University; Minik Rosing, Geological Museum, University of Copenhagen; Finn Surlyk, Department of Geography and Geology, University of Copenhagen Scientific editors: Ole Bennike, Adam A. Garde and W. Stuart Watt Editorial secretaries: Jane Holst and Esben -
X. Paleontology, Biostratigraphy
BIBLIOGRAPHY OF THE GEOLOGY OF INDONESIA AND SURROUNDING AREAS Edition 7.0, July 2018 J.T. VAN GORSEL X. PALEONTOLOGY, BIOSTRATIGRAPHY www.vangorselslist.com X. PALEONTOLOGY, BIOSTRATIGRAPHY X. PALEONTOLOGY, BIOSTRATIGRAPHY ................................................................................................... 1 X.1. Quaternary-Recent faunas-microfloras and distribution ....................................................................... 60 X.2. Tertiary ............................................................................................................................................. 120 X.3. Jurassic- Cretaceous ........................................................................................................................ 161 X.4. Triassic ............................................................................................................................................ 171 X.5. Paleozoic ......................................................................................................................................... 179 X.6. Quaternary Hominids, Mammals and associated stratigraphy ........................................................... 191 This chapter X of the Bibliography 7.0 contains 288 pages with >2150 papers. These are mainly papers of a more general or regional nature. Numerous additional paleontological papers that deal with faunas/ floras from specific localities are listed under those areas in this Bibliography. It is organized in six sub-chapters: - X.1 on modern and sub-recent -
Paleogene History of the Kula Plate: Offshore Evidence and Onshore Implications
Paleogene history of the Kula plate: Offshore evidence and onshore implications PETER LONSDALE Scripps Institution of Oceanography, University of California, San Diego, La Jolia, California 92093 ABSTRACT INTRODUCTION 45-35 mm/yr until the time of Anomaly 25 (late Paleocene, 59 Ma, according to the DNAG Paleocene to middle Eocene magnetic Soon after the present pattern of lithospheric time scale of Berggren and others, 1985, that is anomalies were mapped over oceanic crust plates had been delineated by mapping the char- used throughout this paper). The "half-rate" is that accreted at the Kula-Pacific spreading acteristic structures and seismicity of their the rate of accretion to the Pacific plate; by as- center and is now obliquely entering the boundaries, Pitman and Hayes (1968) recog- suming that spreading had been symmetric, western Aleutian Trench between 179°E and nized that east-west-striking, southward-aging, Engebretson and others (1984,1985) were able 168°E. The strike of anomalies and the pat- magnetic anomalies south of the Aleutian to use these data for quantitative modeling of the tern of abyssal hills and fracture zones Trench implied the former existence of a now- 82-59 Ma motion of the Kula plate relative to changed abruptly during 56-55 Ma, when vanished plate, part of the North Pacific floor the Pacific plate and its hot spots, and thereby north-south spreading veered to northwest- that had moved northward faster than had the relative to the other plates that had bounded it southeast (310°-130°). Kula-Pacific spread- Pacific plate. Grow and Atwater (1970), believ- (Farallon, North American, Eurasia). -
Fj -Lt" ~ ±. ~·~ ~ ~.:&-·;C
fJ -lt" ~ ±. ~·~ ~ ~.:&-·;c. f Transactions and Proceedings of the Palaeontological Society of Japan New Series ·No. 3 --It>• . .. •. ..:.;... .' \ : .,. ........... ...._ .. · , ."': ":~ Palaeontological Society of Japan September 30, 1951 i ... _..... ,I;Jr~ CONTENTS TRANSACTIONS 201. The Occurrence of the Genus Cyclammia in the Tertiary of Kyushu. Sigeo MuRATA 65 202. Notes on Some Tertiary Plants from Tyosen (Korea) II . Kazuo HuziOKA 67 203. On the late Upper Cambrian (Fengshanian} Fauna in Eastern Jehol. Tciichi KonAYASIII "75 204. Nagatoclla Fujimotoi, N. Sp., and a New Studying Method for Fusulinids. Rokuro MoRIKAWA 81 205. On Some Ehrenbergi11a from Japan. Yokichi TAKAYANAGI 85 PROCEEDINGS. ........ 95 President : Hisakatsu Y AOE Councillors: Kiyoshi AsANo, Ryuji ENno, (Business and Accountant), Seido E~mo, Haruyoshi FuJIMoTo, Shoshiro HANZAWA, Ichiro HAYASAKA, Teiichi KoBAYASIII (Editor), Jiro MAKIYAMA, Tatsuro MATSUMoTo, Masao MINATo, Tsuneteru OINOMIKAno (Publication), Tokio SHIKAMA, Koiti SuzuKI, Fuyuji TAKA! (General Affairs), Hisakatsu YABE. All Communications relating to this Journal should be addressed to the PALAEONTOLOGICAL SOCIETY OF JAPAN Geological Institute, Faculty of Science, Tokyo University, Japan Trans. Proc. Palaeont. Soc. Japan. N.S., No. 3, pp. 65-66, S."pt. 1951. 201. THE OCCURRENCE OF THE GENUS CYCLAMMINA IN THE TERTIARY OF KYUSHU* SIGEO MURATA Mining Department, Kyushu Institute of Technology. :ft.ffl~2.~1::~1t¢ Cyclammina QJ.~II:l: /.tfl~:ft.ffiK~<:t1 Cyclammina 11'ftP,Ij·~.fl.."Cir• t.r»··-::J 1:.11:. 4-~~c1Ht Fl.J.v.> t:';:·;~!Jr'!,Q) •ll:tlftll't.: o ~KIJJfVlV: *'¢QJ !lfi~ilttc o tlli'rtr • iiJ;;IiJcJhjlfij/i1' »·b~l}~Q)~nft 6 f!!IQ) Cyclammina ~3EJ!Lt:.QJ-c:Jii:J1J!I.::'*fi->'"oo e,QJrfl;R1,tQJtQJI.tll* -<:t;t, flll'tfilltii·GQJR!i~ID3€Jl.·<:~oo c.tt.b C.vclammina llffll!QJ}ttll:\t~;{Jitt.tlliJb»•l::idll~ .:-:,fi V>:kf!tQJ 1d'.> QJ¥f L ... -
Late Cretaceous and Paleogene Tectonic Evolution of the North Pacific Ocean
Earth and Planetary Science Letters, 65 (1983) 145-166 145 Elsevier Science Publishers B.V., Amsterdam - Printed in The Netherlands [4l Late Cretaceous and Paleogene tectonic evolution of the North Pacific Ocean David K. Rea l and John M. Dixon 2 I Oceanography Program, Department of Atmospheric and Oceanic Science, University of Michigan, Ann Arbor, MI 48109 (U.S.A.) 2 Department of Geological Sciences, Queen's University, Kingston, Ont. KTL 3N6 (Canada) Received March 24, 1983 Revised version received July 11, 1983 The Late Cretaceous history of the northern Pacific Ocean has not been adequately deciphered, largely because a major plate reorganization occurred during the Cretaceous magnetic quiet interval. Using primary data to reconstruct plate motions from fracture zone trends and Late Cretaceous seafloor spreading magnetic anomalies allows formulation of a reasonable sequence of events that accounts for all the geologic features of that region, especially the Emperor and Chinook troughs. The primary event in our reconstruction is the subduction of the old northwest Pacific triple junction. New relative plate motions imposed by formation of convergent boundaries along both the northern Pacific and Farallon plates caused the Farallon plate to crack. This subdivision occurred 82 m.y. ago and resulted in the formation of the Kula and Chinook plates. The Chinook plate was bounded on the north by the Chinook-Kula ridge, the western arm of the Great Magnetic Bight, on the west by the southern Emperor trough, a slowly spreading rift valley, on the south by the Mendocino transform, and on the east by the Chinook-Farallon ridge.