Bulletin 1056-A
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Pamphlet to Accompany Scientific Investigations Map 3131
Bedrock Geologic Map of the Seward Peninsula, Alaska, and Accompanying Conodont Data By Alison B. Till, Julie A. Dumoulin, Melanie B. Werdon, and Heather A. Bleick Pamphlet to accompany Scientific Investigations Map 3131 View of Salmon Lake and the eastern Kigluaik Mountains, central Seward Peninsula 2011 U.S. Department of the Interior U.S. Geological Survey Contents Introduction ....................................................................................................................................................1 Sources of data ....................................................................................................................................1 Components of the map and accompanying materials .................................................................1 Geologic Summary ........................................................................................................................................1 Major geologic components ..............................................................................................................1 York terrane ..................................................................................................................................2 Grantley Harbor Fault Zone and contact between the York terrane and the Nome Complex ..........................................................................................................................3 Nome Complex ............................................................................................................................3 -
Hot Rocks from Cold Places: a Field, Geochemical and Geochronological Study from the High Arctic Large Igneous P Rovince (HALIP) at Axel Heiberg Island, Nunavut
! !"#$%"&'($)*"+$,"-.$/-0&1(2$3$451-.6$71"&81+5&0-$09.$ 71"&8*"9"-":5&0-$;#<.=$)*"+$#81$!5:8$3*&$>0*:1$ ?:91"<($/*"@59&1$A!3>?/B$0#$3C1-$!15D1*:$?(-09.6$ E<90@<#$ $ $ by Cole Girard Kingsbury A thesis submitted to the Faculty of Graduate and Postdoctoral Affairs in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Earth Sciences Ottawa – Carleton Geoscience Centre and Carleton University Ottawa, Ontario © 2016 Cole Girard Kingsbury ! ! !"#$%&'$() ) ) ) ) ) ) ) ) ) ) The geology of the Arctic is greatly influenced by a period of widespread Cretaceous magmatic activity, the High Arctic Large Igneous Province (HALIP). Two major tholeiitic magmatic pulses characterize HALIP: an initial 120 -130 Ma pulse that affected Arctic Canada and formally adjacent regions of Svalbard (Norway) and Franz Josef Land (Russia). In Canada, this pulse fed lava flows of the Isachsen Formation. A second 90-100 Ma pulse that apparently only affected the Canadian side of the Arctic, fed flood basalts of the Strand Fiord Formation. The goal of this thesis is to improve understanding of Arctic magmatism of the enigmatic HALIP through field, remote sensing, geochemical and geochronology investigations of mafic intrusive rocks collected in the South Fiord area of Axel Heiberg Island, Nunavut, and comparison with mafic lavas of the Isachsen and Strand Fiord Formations collected from other localities on the Island. Ground-based and remote sensing observations of the South Fiord area reveal a complex network of mafic sills and mainly SSE-trending dykes. Two new U-Pb baddeleyite ages of 95.18 ± 0.35 Ma and 95.56 ± 0.24 Ma from South Fiord intrusions along with geochemical similarity confirm these intrusions (including the SSE-trending dykes) are feeders for the Strand Fiord Formation lavas. -
Metadefender Core V4.12.2
MetaDefender Core v4.12.2 © 2018 OPSWAT, Inc. All rights reserved. OPSWAT®, MetadefenderTM and the OPSWAT logo are trademarks of OPSWAT, Inc. All other trademarks, trade names, service marks, service names, and images mentioned and/or used herein belong to their respective owners. Table of Contents About This Guide 13 Key Features of Metadefender Core 14 1. Quick Start with Metadefender Core 15 1.1. Installation 15 Operating system invariant initial steps 15 Basic setup 16 1.1.1. Configuration wizard 16 1.2. License Activation 21 1.3. Scan Files with Metadefender Core 21 2. Installing or Upgrading Metadefender Core 22 2.1. Recommended System Requirements 22 System Requirements For Server 22 Browser Requirements for the Metadefender Core Management Console 24 2.2. Installing Metadefender 25 Installation 25 Installation notes 25 2.2.1. Installing Metadefender Core using command line 26 2.2.2. Installing Metadefender Core using the Install Wizard 27 2.3. Upgrading MetaDefender Core 27 Upgrading from MetaDefender Core 3.x 27 Upgrading from MetaDefender Core 4.x 28 2.4. Metadefender Core Licensing 28 2.4.1. Activating Metadefender Licenses 28 2.4.2. Checking Your Metadefender Core License 35 2.5. Performance and Load Estimation 36 What to know before reading the results: Some factors that affect performance 36 How test results are calculated 37 Test Reports 37 Performance Report - Multi-Scanning On Linux 37 Performance Report - Multi-Scanning On Windows 41 2.6. Special installation options 46 Use RAMDISK for the tempdirectory 46 3. Configuring Metadefender Core 50 3.1. Management Console 50 3.2. -
Persistence of Branchinecta Paludosa (Anostraca) in Southern Wyoming, with Notes on Zoogeography
This file was created by scanning the printed publication. Errors identified by the software have been corrected; however, some errors may remain. JOURNAL OF CRUSTACEAN BIOLOGY, 13(1): 184-189, 1993 PERSISTENCE OF BRANCHINECTA PALUDOSA (ANOSTRACA) IN SOUTHERN WYOMING, WITH NOTES ON ZOOGEOGRAPHY James F. Saunders III, Denton Belk, and Richard Dufford ABSTRACT The fairy shrimp Branchinectapaludosa is a persistentresident of aestival ponds at high elevation in the Medicine Bow Mountains of southernWyoming. These populationsare far removed from the Arctic tundrahabitat that typifiesthe distributionof the species, and appear to representthe southern margin of the range in North America. All of the records for the northernUnited States and southernCanada appear to lie along the CentralFlyway that is a major migrationroute for waterfowland shorebirdsthat nest in the Arctic. Passive dispersal probablyprovides for frequentcolonization of marginalhabitats and gene flow to established populations. The fairy shrimp Branchinectapaludosa have been deposited in the University of (Muller)is widely distributedin the circum- Colorado Museum (UCM 2192, 2193, polar tundra of the Holarctic region (Vek- 2194). The Snowy Range is an axial rem- hoff, 1990). In Europe, it occurs chiefly at nant which rises about 300 m above the latitudes above 60?N, but there are isolated surrounding Medicine Bow Mountains recordsfrom the High Tatra Mountains on (Houston and others, 1978). The ponds are the borderbetween Czechoslovakiaand Po- mainly in the upperTelephone Creek drain- land at about 49?N (Brtek, 1976). Records age at elevations of 3,200-3,350 m. Most for Russia are typically along the Arctic of the ponds are underlainby the Nash Fork margin, but include the southern tip of the formation (Houston and others, 1978), and Kamchatka Peninsula at 52?N (Linder, the characteristicmetadolomite is present 1932). -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
A King-Size Theropod Coprolite
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/232796267 A king-size theropod coprolite Article in Nature · June 1998 DOI: 10.1038/31461 CITATIONS READS 154 2,385 4 authors, including: Karen Chin Tim Tokaryk University of Colorado Boulder Royal Saskatchewan Museum 32 PUBLICATIONS 1,143 CITATIONS 39 PUBLICATIONS 488 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: The Dinosaur Park Formation of Saskatchewan View project Paleobiodiverity and the K-Pg Boundary View project All content following this page was uploaded by Tim Tokaryk on 10 June 2015. The user has requested enhancement of the downloaded file. letters to nature compositions, though the ground mass contains more silicon and aluminium (Table 2). X-ray powder-diffraction analyses indicate A king-sized theropod that carbonate fluorapatite is the predominant phosphate mineral in both the bone and the ground mass. coprolite Several factors confirm that this specimen is a coprolite. The most diagnostic feature is a phosphatic composition, which is character- Karen Chin, Timothy T. Tokaryk*, Gregory M. Erickson†‡ istic of carnivore coprolites9. As phosphorus normally constitutes & Lewis C. Calk 10 only about 0.1% of the Earth’s crustal rocks , concentrated phos- United States Geological Survey, 345 Middlefield Road, MS 975, Menlo Park, phate deposits usually indicate biotic accumulations, and the overall 8 California 94025, USA configuration of the mass is consistent with the irregular faecal * Eastend Fossil Research Station, Royal Saskatchewan Museum, Box 460, deposits produced by very large animals. The matrix-supported Eastend, Saskatchewan S0N 0T0, Canada distribution of bone fragments argues against the possibility that the † Department of Integrative Biology & Museums of Vertebrate Zoology and mass represents regurgitated material or fluvially aggregated bone Paleontology, University of California, Berkeley, California 94720, USA debris. -
TGI Strat Column 2009.Cdr
STRATIGRAPHIC CORRELATION CHART TGI II: Williston Basin Architecture and Hydrocarbon Potential in Eastern Saskatchewan and Western Manitoba EASTERN MANITOBA PERIOD MANITOBA SUBSURFACE SASKATCHEWAN OUTCROP ERA glacial drift glacial drift glacial drift Quaternary Wood Mountain Formation Peace Garden Peace Garden Member Tertiary Member Ravenscrag Formation CENOZOIC Formation Goodlands Member Formation Goodlands Member Turtle Mountain Turtle Mountain Turtle Frenchman Formation Whitemud Formation Boissevain Formation Boissevain Formation Eastend Formation Coulter Member Coulter Member Bearpaw Formation Odanah Member Belly River “marker” Odanah Member Belly River Formation “lower” Odanah Member Millwood Member Lea Park Formation Millwood Member MONTANA GROUP Pembina Member Pembina Member Pierre Shale Pierre Shale Milk River Formation Gammon Ferruginous Member Gammon Ferruginous Member Niobrara Formation Chalky Unit Boyne Member Boyne Member Boyne Calcareous Shale Unit Member Carlile Morden Member Carlile upper Formation Morden Member Formation Morden Member Carlile Formation Assiniboine Marco Calcarenite Assiniboine Member Member CRETACEOUS Second White Specks Laurier Limestone Beds Favel Favel Keld Keld Member Member Formation Formation Belle Fourche Formation Belle Fourche Member MESOZOIC COLORADO GROUP Belle Fourche Member upper Fish Scale Formation Fish Scale Zone upper Base of Fish Scale marker Base of Fish Scale marker Westgate Formation Westgate Member lower Westgate Member Newcastle Formation Newcastle Member lower Viking Sandstone -
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air
Summits on the Air – ARM for Canada (Alberta – VE6) Summits on the Air Canada (Alberta – VE6/VA6) Association Reference Manual (ARM) Document Reference S87.1 Issue number 2.2 Date of issue 1st August 2016 Participation start date 1st October 2012 Authorised Association Manager Walker McBryde VA6MCB Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged Page 1 of 63 Document S87.1 v2.2 Summits on the Air – ARM for Canada (Alberta – VE6) 1 Change Control ............................................................................................................................. 4 2 Association Reference Data ..................................................................................................... 7 2.1 Programme derivation ..................................................................................................................... 8 2.2 General information .......................................................................................................................... 8 2.3 Rights of way and access issues ..................................................................................................... 9 2.4 Maps and navigation .......................................................................................................................... 9 2.5 Safety considerations .................................................................................................................. -
LATE MIOCENE FISHES of the CACHE VALLEY MEMBER, SALT LAKE FORMATION, UTAH and IDAHO By
LATE MIOCENE FISHES OF THE CACHE VALLEY MEMBER, SALT LAKE FORMATION, UTAH AND IDAHO by PATRICK H. MCCLELLAN AND GERALD R. SMITH MISCELLANEOUS PUBLICATIONS MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN, 208 Ann Arbor, December 17, 2020 ISSN 0076-8405 P U B L I C A T I O N S O F T H E MUSEUM OF ZOOLOGY, UNIVERSITY OF MICHIGAN NO. 208 GERALD SMITH, Editor The publications of the Museum of Zoology, The University of Michigan, consist primarily of two series—the Miscellaneous Publications and the Occasional Papers. Both series were founded by Dr. Bryant Walker, Mr. Bradshaw H. Swales, and Dr. W. W. Newcomb. Occasionally the Museum publishes contributions outside of these series. Beginning in 1990 these are titled Special Publications and Circulars and each is sequentially numbered. All submitted manuscripts to any of the Museum’s publications receive external peer review. The Occasional Papers, begun in 1913, serve as a medium for original studies based principally upon the collections in the Museum. They are issued separately. When a sufficient number of pages has been printed to make a volume, a title page, table of contents, and an index are supplied to libraries and individuals on the mailing list for the series. The Miscellaneous Publications, initiated in 1916, include monographic studies, papers on field and museum techniques, and other contributions not within the scope of the Occasional Papers, and are published separately. Each number has a title page and, when necessary, a table of contents. A complete list of publications on Mammals, Birds, Reptiles and Amphibians, Fishes, I nsects, Mollusks, and other topics is available. -
Critical Infrastructure Intelligence Assessment
PROTECTED A/ !CANADIAN f.VES OtilLY ,:;, CRITICAL INFRASTRUCTURE INTELLIGENCE ASSESSMENT Criminal Threats to the Canadian Petroleum Industry 2014-01-24 The RCMP, in support of the Government of canada's (GoC) strategy to ensure critical infrastructure (Cl) resiliency, assesses, evaluates and reports on information regarding threats and criminality to Canada's Cl. This intelligence and/or information may be used to assist in the protection of Canada's Cl Critical Infrastructure Intelligence Team Assessments are issued to provide critical infrastructure stakeholders with a law enforcement intelligence assessment of current Cl protection issues. This Assessment is current as of 2014-01-24. KEY FINDINGS The Canadian petroleum industry is requesting government approval to construct many large petroleum projects which, if approved, will be situated across the country; There is a growing, highly organized and well-financed, anti-Canadian petroleum movement, that consists of peaceful activists, militants and violent extremists, who are opposed to society's reliance on fossil fuels; The anti-petroleum movement is focused on challenging the energy and environmental policies that promote the development of Canada's vast petroleum resources; Governments and petroleum companies are being encouraged, and increasingly threatened, by violent extremists to cease all actions which the extremists believe, contributes to greenhouse gas emissions; • Recent protests in New Brunswick are the most violent of the national anti-petroleum protests to date; Violent anti-petroleum extremists will continue to engage in criminal activity to promote their anti-petroleum ideology; These extremists pose a realistic criminal threat to Canada's petroleum industry, its workers and assets, and to first responders. -
U.S. Department of the Interior U.S. Geological Survey
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Prepared in cooperation with New Mexico Bureau of Mines and Mineral Resources 1997 MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Cover: View looking south to the east side of the northeastern Organ Mountains near Augustin Pass, White Sands Missile Range, New Mexico. Town of White Sands in distance. (Photo by Susan Bartsch-Winkler, 1995.) MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO By SUSAN BARTSCH-WINKLER, Editor ____________________________________________________ U. S GEOLOGICAL SURVEY OPEN-FILE REPORT 97-521 U.S. Geological Survey Prepared in cooperation with New Mexico Bureau of Mines and Mineral Resources, Socorro U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Shaefer, Interim Director For sale by U.S. Geological Survey, Information Service Center Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO Susan Bartsch-Winkler, Editor Summary Mimbres Resource Area is within the Basin and Range physiographic province of southwestern New Mexico that includes generally north- to northwest-trending mountain ranges composed of uplifted, faulted, and intruded strata ranging in age from Precambrian to Recent. -
Evolution of Canada's Oil and Gas Industry
Evolution Of Canada’s oil and gas industry A historical companion to Our Petroleum Challenge 7th edition EVOLUTION of Canada’s oil and gas industry Copyright 2004 by the Canadian Centre for Energy Information Writer: Robert D. Bott Editors: David M. Carson, MSc and Jan W. Henderson, APR, MCS Canadian Centre for Energy Information Calgary, Alberta, Canada T2R 0C5 Telephone: (403) 263-7722 Facsimile: (403) 237-6286 Toll free: 1-877-606-4636 E-mail: [email protected] Internet: www.centreforenergy.com Canadian Cataloguing in Publications Data Main entry under title: EVOLUTION of Canada’s oil and gas industry Includes bibliographical references 1. Petroleum industry and trade – Canada 2. Gas industry – Canada 3. History – petroleum industry – Canada I. Bott, Robert, 1945-II. Canadian Centre for Energy Information ISBN 1-894348-16-8 Readers may use the contents of this book for personal study or review only. Educators and students are permitted to reproduce portions of the book, unaltered, with acknowledgment to the Canadian Centre for Energy Information. Copyright to all photographs and illustrations belongs to the organizations and individuals identified as sources. For other usage information, please contact the Canadian Centre for Energy Information in writing. Centre for Energy The Canadian Centre for Energy Information (Centre for Energy) is a non-profit organization created in 2002 to meet a growing demand for balanced, credible information about the Canadian energy sector. On January 1, 2003, the Petroleum Communication Foundation (PCF) became part of the Centre for Energy. Our educational materials will build on the excellent resources published by the PCF and, over time, cover all parts of the Canadian energy sector from oil, natural gas, coal, thermal and hydroelectric power to nuclear, solar, wind and other sources of energy.