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Conventional Natural Gas Play Atlas Northeast British Columbia
����������������������������������� �������������������������� ������������������������������������� ���������������������� ������������������������������������������ Ministry of Energy, Mines and Petroleum Resources 1 CoverAtlas.indd 1 15/03/2006 1:55:13 PM British Columbia Ministry of Energy, Mines and Petroleum Resources Oil & Gas Division, Resource Development & Geoscience Branch 6th floor – 1810 Blanshard Street Victoria, British Columbia V8W 9N3 Contact: Vic Levson, Director Petroleum & Aggregate Geoscience E-mail: [email protected] Fax: (250) 952-0922 Web site: www.em.gov.bc.ca/oilandgas Library and Archives Canada Cataloguing in Publication Data Main entry under title: Conventional natural gas play atlas, northeast British Columbia (Petroleum geology publication ; 2006:1) Includes bibliographical references: p. ISBN 0-7726-5532-4 1. Natural gas reserves - British Columbia, Northern - Atlases. 2. Geology, Economic - British Columbia, Northern - Atlases. I. British Columbia. Resource Development and Geoscience Branch. II. Series. TN882.C32B74 2006 553.2’8509711870223 C2006-960061-9 2 Conventional Natural Gas Play Atlas: Northeast BC Ministry of Energy, Mines and Petroleum Resources 3 The Northeast BC Play Atlas The Resource Development and Geoscience Branch of the BC Ministry of Energy and Mines and Petroleum Resources (MEMPR) in partnership with the National Energy Board (NEB) have undertaken an assessment of British Columbia’s undiscovered resources. The final report entitled Northeast British Columbia’s Ultimate Potential for Natural Gas Report - 2006A is now available through both the NEB and MEMPR websites. To access the report on the provincial government website, go to: http://www.em.gov.bc.ca/subwebs/oilandgas/resource/cog/cog.htm. While this new report covers all of BC’s gas potential areas, the major focus of the assessment is the quantification of the remaining undiscovered conventional gas potential of NEBC. -
Mapping Known and Potential Karst Areas in the Northwest Territories, Canada
Mapping Known and Potential Karst Areas in the Northwest Territories, Canada Derek Ford, PGeo., PhD, FRSC. Emeritus Professor of Geography and Earth Sciences, McMaster University [email protected] For: Environment and Natural Resources, Government of the Northwest Territories August 2009 (i) Executive Summary The Goal of this Report is to Produce Maps of the Known and Potential Karst Landform Sites in the Northwest Territories (NWT) Karst landforms are those created by the dissolution of comparatively soluble rocks and the routing of the water (from rain or snowmelt) underground via caves rather than at the surface in river channels. The principal karst rocks are salt (so soluble that it is scarcely seen at the surface in the NWT), gypsum and anhydrite (solubility around 2500 mg/l of water), and limestone and dolomite (solubility around 250 -350 mg/l). All of these rock types are common and widespread amongst the sedimentary strata in the NWT. Surface karst landforms include: a) karren, which are spreads of individually small solution pits, shafts, and runnels that, collectively, may cover many hectares (limestone pavements); b) sinkholes of solutional, collapse, or other origin that can be tens to hundreds of metres in diameter and proportionally as deep. Sinkholes are considered the diagnostic karst landform worldwide; c) larger topographically closed depressions that may flood or drain seasonally, poljes if flat-floored, otherwise turloughs; d) extensive dry valleys and gorges, dry because their formative waters have been captured underground. All water sinking underground via karst landforms of all sizes drain quickly in comparison with all other types of groundwater because they are able to flow through solutionally enlarged conduits, termed caves where they are of enterable size. -
Biostratigraphy and Paleoecology of the Upper Devonian Ithaca Formation Near Cortland, New York
Biostratigraphy and Paleoecology of the Upper Devonian Ithaca Formation near Cortland, New York by Jonathan W. Harrington Geological Consultant Groton, New York and W. Graham Heaslip State University College at Cortland Cortland, New York It i s particularly appropriate that we examine the Ithaca Formation in the Cortland area during the Golden Anniversary Meeting of the New York State Geological Association. The rocks of this region are of con siderable historical interest, having received attention since the earli est days of geolog ical investigation in New York State . In fact, the presence of fossil shells in the Devonian rocks of New York was first noted in 1751 at a hillside outcrop in Cortland County by John Bartram, a member of the Lewis Evans Onondaga expedition (We lls, 1963). The New York Devonian is unique in its completeness, fossil content. numerous outcrops, and relatively undisturbed nature. It is the standard reference section for North America and displays a classic example of facies transition. Stratigraphic and paleontologic investigation over the past century has produced a wealth of infonnation, but uDespite this, perhaps another century of rigorous study wi ll be required before a thor ough understanding of its paleontology, lithology, stratigraphy and paleoecology can be attained. n (Rickard. 1964). The early stratigraphic work in the Upper Devonian of New York was done mainly by James Hall. J. M. Clarke. and H. S. Williams between 1840 and 1915 . These workers subdivided the succession, described the faunas and attempted to correlate along the strike. Due to comp l ex interfinger ing of the argillaceous western sequence with the thicker arenaceous eastern sequence, correlations proved difficult. -
Paper 61-13 Camsell Bend and Root River Map-Areas
PAPER 61-13 CAMSELL BEND AND ROOT RIVER MAP-AREAS, DISTRICT OF MACKENZIE, NORTHWEST TERRITORIES 95Jand K (Report, 2 maps, 2 figures) R. J. W. Douglas and D. K. Norris DEC 5 1961 . _.. Price 50 cents 1961 GEOLOGICAL SURVEY OF CANADA CANADA PAPER 61-13 CAMSELL BEND AND ROOT RIVER MAP-AREAS, DISTRICT OF MACKENZIE, NORTHWEST TERRITORIES 95 J,K By R. J. W. Douglas and D. K. Norris DEPARTMENT OF MINES AND TECHNICAL SURVEYS CANADA 51310-1 ROGER DUHAMEL, F. R. S. C. QUEEN'S PR INTER AND CONTROLLER OF STATIONERY OTTAWA, 1961 Pri ce 50 ce nts Cat. No. M44-6 1 11 CONTENTS Page Introduction .•••••••••••••••••••••• • • •••••••••••••••.••.•• References • • • • • • . • • • • • • • • • • • • • • • . • • . • • • • • • • • • • 1 Physical features........ ................................ 3 Stratigraphy......... ....... .................... ......... 5 Table of formations • • • • • • • • • . • . • • • . • . • • • • • • • . • • • • • • • 8-9 Palaeozoic •.•• , .............................. • • • • • • 6 Ordovician and older {?) - Sunblood formation ( 1) • • • . • • • • • • • . • • . • • • • • • • • • • • • • • • • • . 6 Ordovician and younger - map-units 2-10, including the Whittaker (3), Delorme (4), Camsell (5), Mount Kindle (7), a nd Sombre (10) formations • • • • • • • . • . • • • • • • • • • • • . • • • • • • • • . • • • . • 7 Middle Devonian and older { ? ) - map-units 11-17, comprising the Arnica {11), Manetoe (12), Fune ral (13), Bear Rock (14), Landry (15), Headless (16), and Nahanni (17) formations....... 14 Upper Devonian - map-units 18-25, including -
Petroleum Resource Assessment, Peel Plateau and Plain, Yukon Territory, Canada K.G
Energy, Mines and Resources • Yukon Geological Survey • Oil and Gas Management Branch YGS OPEN FILE 2005-3/GSC OPEN FILE 4841 Petroleum Resource Assessment, Peel Plateau and Plain, Yukon Territory, Canada K.G. Osadetz, B.C. MacLean, D.W. Morrow, J. Dixon and P.K. Hannigan Natural Resources Ressources naturelles Canada Canada YGS OPEN FILE 2005-3/GSC OPEN FILE 4841 Petroleum Resource Assessment, Peel Plateau and Plain, Yukon Territory, Canada K.G. Osadetz1, B.C. MacLean1, D.W. Morrow1, J. Dixon1 and P.K. Hannigan1 1Geological Survey of Canada, 3303 33rd Street NW, Calgary, Alberta T2L 2A7 Published under the authority of the Minister of Energy, Mines and Resources, Yukon Government http://www.emr.gov.yk.ca Printed in Whitehorse, Yukon, 2005. © Minister of Energy, Mines and Resources, Yukon Government This report may be obtained from: Geoscience and Information Sales GSC Calgary Publication Sales c/o Whitehorse Mining Recorder 3303-33rd Street N.W. 102-300 Main Street Calgary, Alberta, Canada T2L 2A7 Box 2703 (K102) phone (403) 292-7030 Whitehorse, Yukon, Canada Y1A 2C6 fax (403) 299-3542 phone (867) 667-5200, fax (867) 667-5150 e-mail [email protected] e-mail [email protected] http://gsc.nrcan.gc.ca/org/calgary/pub/bookstore_e.php www.geology.gov.yk.ca In referring to this publication, please use the following citation: Osadetz, KG., MacLean, B.C., Morrow, D.W., Dixon, J. and Hannigan, P.K., 2005. Petroleum Resource Assessment, Peel Plateau and Plain, Yukon Territory, Canada. Yukon Geological Survey Open File 2005-3, Geological Survey of Canada Open File 4841, 76 p. -
General 29 April 2011
United Nations ECE /MP.WAT/WG.2/2011/13 Economic and Social Council Distr.: General 29 April 2011 English only Economic Commission for Europe Meeting of the Parties to the Convention on the Protection and Use of Transboundary Watercourses and International Lakes Working Group on Monitoring and Assessment Twelth meeting Geneva, 2–4 May 2011 Item 5 (b) of the provisional agenda Assessment of the status of transboundary waters in the UNECE 1 region: assessment of transboundary rivers, lakes and groundwaters in the Caucasus. Assessment of transboundary rivers, lakes and groundwaters discharging into the Black Sea 2 Note prepared by the secretariat* Summary This document was prepared pursuant to decisions taken by the Meeting of the Parties to the Convention on the Protection and Use of Transboundary Watercourses and International Lakes at its fifth session (Geneva, 10–12 November 2009) (ECE/MP.WAT/29, para. 81 (e)), and by the Working Group on Monitoring and Assessment at its eleventh meeting (Geneva, 6–7 July 2010), requesting the secretariat to finalize the sub regional assessments of South-Eastern Europe, Caucasus, Eastern and Northern Europe and Central Asia for the second Assessment of Transboundary Rivers, Lakes and Groundwaters in time for its submission to the Seventh “Environment for Europe” Ministerial Conference (Astana, 21–23 September 2011). This document contains the draft assessments of the different transboundary rivers, lakes 1 United Nations Economic Commission for Europe. 2 This document was submitted for publication without formal editing. * The present document has been submitted on the present date due to late receipt of inputs by concerned countries and resource constraints in the secretariat. -
Liard Basin – Middle Devonian Exploration
LIARD BASIN – MIDDLE DEVONIAN EXPLORATION Warren Walsh1, Osman Salad Hersi2, Mark Hayes1 ABSTRACT The Liard Basin is a sub-basin of the Western Canada Sedimentary Basin (WCSB) system, straddling the Northwest and Yukon Territories boundary with the Province of British Columbia. The basin contains over 5 km of sedimentary strata of Cambrian through Upper Cretaceous age. Exploration for Manetoe Dolomite reservoirs hosted within middle Devonian carbonates of the Dunedin and Nahanni formations began in the 1950’s. Several pools have been found within the fold and thrust belt both in Northeastern British Columbia and the Yukon and Northwest Territories. Recent gas discoveries within the Devonian Nahanni Formation north of Fort Liard, NWT has renewed interest in this play. Resource assessments for the middle Devonian play in the Liard Basin estimates between 2.8 and 6.6 Tcf undiscovered gas, with approximately 2.5 Tcf estimated to be located within Northeastern British Columbia. The British Columbia Ministry of Energy and Mines (BC MEM) is currently working with the University of Regina and the Geological Survey of Canada (GSC) to expand our knowledge and understanding of the Liard Basin. Through a contribution agreement, the BC MEM, in conjunction with Dr. Osman Salad Hersi of the University of Regina, is supporting graduate level studies on the sedimentology, stratigraphy and diagenesis of Middle Devonian, shallow-marine carbonates of the Dunedin Formation of subsurface Liard Basin, with application to petroleum exploration. The BC MEM also continues their relationship with the GSC, who has recently published a reinterpretation of the Bovie Structure which included the identification of new conceptual plays within the Liard Basin. -
The Letters F and T Refer to Figures Or Tables Respectively
INDEX The letters f and t refer to figures or tables respectively "A" Marker, 312f, 313f Amherstberg Formation, 664f, 728f, 733,736f, Ashville Formation, 368f, 397, 400f, 412, 416, Abitibi River, 680,683, 706 741f, 765, 796 685 Acadian Orogeny, 686, 725, 727, 727f, 728, Amica-Bear Rock Formation, 544 Asiak Thrust Belt, 60, 82f 767, 771, 807 Amisk lowlands, 604 Askin Group, 259f Active Formation, 128f, 132f, 133, 139, 140f, ammolite see aragonite Assiniboia valley system, 393 145 Amsden Group, 244 Assiniboine Member, 412, 418 Adam Creek, Ont., 693,705f Amundsen Basin, 60, 69, 70f Assiniboine River, 44, 609, 637 Adam Till, 690f, 691, 6911,693 Amundsen Gulf, 476, 477, 478 Athabasca, Alta., 17,18,20f, 387,442,551,552 Adanac Mines, 339 ancestral North America miogeocline, 259f Athabasca Basin, 70f, 494 Adel Mountains, 415 Ancient Innuitian Margin, 51 Athabasca mobile zone see Athabasca Adel Mountains Volcanics, 455 Ancient Wall Complex, 184 polymetamorphic terrane Adirondack Dome, 714, 765 Anderdon Formation, 736f Athabasca oil sands see also oil and gas fields, Adirondack Inlier, 711 Anderdon Member, 664f 19, 21, 22, 386, 392, 507, 553, 606, 607 Adirondack Mountains, 719, 729,743 Anderson Basin, 50f, 52f, 359f, 360, 374, 381, Athabasca Plain, 617f Aftonian Interglacial, 773 382, 398, 399, 400, 401, 417, 477f, 478 Athabasca polymetamorphic terrane, 70f, Aguathuna Formation, 735f, 738f, 743 Anderson Member, 765 71-72,73 Aida Formation, 84,104, 614 Anderson Plain, 38, 106, 116, 122, 146, 325, Athabasca River, 15, 20f, 35, 43, 273f, 287f, Aklak -
Phylogenetics, Classification, and Biogeography of the Treefrogs (Amphibia: Anura: Arboranae)
Zootaxa 4104 (1): 001–109 ISSN 1175-5326 (print edition) http://www.mapress.com/j/zt/ Monograph ZOOTAXA Copyright © 2016 Magnolia Press ISSN 1175-5334 (online edition) http://doi.org/10.11646/zootaxa.4104.1.1 http://zoobank.org/urn:lsid:zoobank.org:pub:D598E724-C9E4-4BBA-B25D-511300A47B1D ZOOTAXA 4104 Phylogenetics, classification, and biogeography of the treefrogs (Amphibia: Anura: Arboranae) WILLIAM E. DUELLMAN1,3, ANGELA B. MARION2 & S. BLAIR HEDGES2 1Biodiversity Institute, University of Kansas, 1345 Jayhawk Blvd., Lawrence, Kansas 66045-7593, USA 2Center for Biodiversity, Temple University, 1925 N 12th Street, Philadelphia, Pennsylvania 19122-1601, USA 3Corresponding author. E-mail: [email protected] Magnolia Press Auckland, New Zealand Accepted by M. Vences: 27 Oct. 2015; published: 19 Apr. 2016 WILLIAM E. DUELLMAN, ANGELA B. MARION & S. BLAIR HEDGES Phylogenetics, Classification, and Biogeography of the Treefrogs (Amphibia: Anura: Arboranae) (Zootaxa 4104) 109 pp.; 30 cm. 19 April 2016 ISBN 978-1-77557-937-3 (paperback) ISBN 978-1-77557-938-0 (Online edition) FIRST PUBLISHED IN 2016 BY Magnolia Press P.O. Box 41-383 Auckland 1346 New Zealand e-mail: [email protected] http://www.mapress.com/j/zt © 2016 Magnolia Press All rights reserved. No part of this publication may be reproduced, stored, transmitted or disseminated, in any form, or by any means, without prior written permission from the publisher, to whom all requests to reproduce copyright material should be directed in writing. This authorization does not extend to any other kind of copying, by any means, in any form, and for any purpose other than private research use. -
Mississippian Ostracoda of the Amsden Formation (Mississippian and Pennsylvanian) of Wyoming
Mississippian Ostracoda of the Amsden Formation (Mississippian and Pennsylvanian) of Wyoming GEOLOGICAL SURVEY PROFESSIONAL PAPER 848-G Mississippian Ostracoda of the Amsden Formation (Mississippian and Pennsylvanian) of Wyoming By I. G. SOHN THE AMSDEN FORMATION (MISSISSIPPIAN AND PENNSYLVANIAN) OF WYOMIN(;. GEOLOGICAL SURVEY PROFESSIONAL PAPER 848-G Descriptions and illustrations of 22 species of ostracodes UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Sohn, Israel Gregory, 1911- Mississippian ostracoda of the Amsden Formation (Mississippian and Pennsylvanian) of Wyoming. (Geological Survey professional paper ; 848-G) Bibliography: p. Includes index. Supt. of Docs. no.: I 19.16 :848-G 1. Ostracoda, Fossil. 2. Paleontology-Mississippian. 3. Paleontology-Wyoming. I. Title. II. Series: United States. Geological Survey. Professional paper ; 848-G. QE817.08S573 565' .33'09787 74-31457 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02639-2 CONTENTS Page Abstract ________ --.-----__ - _--------------------------------------------- G1 Introduction ------------------------------------------------------------ 1 Acknowledgments -------------------------.------------------------------- 2.. Ostracode localities ___________________________________________ ---------- •) Systematic descriptions -------------------------------------------------- -
Hdl 86511.Pdf
PUBLISHED VERSION Susan E. Evans, Joseph R. Groenke, Marc E. H. Jones, Alan H. Turner, David W. Krause New material of Beelzebufo, a hyperossified frog (Amphibia: anura) from the Late Cretaceous of Madagascar PLoS One, 2014; 9(1):e87236-1-e87236-61 © 2014 Evans et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Originally published at: http://doi.org/10.1371/journal.pone.0087236 PERMISSIONS http://creativecommons.org/licenses/by/4.0/ http://hdl.handle.net/2440/86511 New Material of Beelzebufo, a Hyperossified Frog (Amphibia: Anura) from the Late Cretaceous of Madagascar Susan E. Evans1*, Joseph R. Groenke2, Marc E. H. Jones1,3, Alan H. Turner2, David W. Krause2 1 Department of Cell and Developmental Biology, University College London, London, United Kingdom, 2 Department of Anatomical Sciences, Stony Brook University, Stony Brook, New York, United States of America, 3 School of Earth and Environmental Sciences, The University of Adelaide, Adelaide, South Australia, Australia Abstract The extant anuran fauna of Madagascar is exceptionally rich and almost completely endemic. In recent years, many new species have been described and understanding of the history and relationships of this fauna has been greatly advanced by molecular studies, but very little is known of the fossil history of frogs on the island. Beelzebufo ampinga, the first named pre-Holocene frog from Madagascar, was described in 2008 on the basis of numerous disarticulated cranial and postcranial elements from the Upper Cretaceous (Maastrichtian) Maevarano Formation of Madagascar. -
Pa 74-11.Pdf
Energy, Mines and Energie, Mines et I+ Resources Canada Ressources Canada GEOLOGICAL SURVEY PAPER 74-11 BIOSTRATIGRAPHIC DETERMINATIONS OF FOSSILS FROM THE SUBSURFACE OF THE NORTHV\IEST AND YUKON TERRITORIES C. R. BARNES, W. W. BRIDEAUX, T. P. CHAMNEY, D. R. CLOWSER, R. E. DUNAY, M . .J. FISHER, W. H. FRITZ, WILLIAM S. HOPKINS, .JR., .J. A . .JELETZKY, D. C. McGREGOR, B. S. NORFORD, A. W. NORRIS, A. E. H. PEDDER, P . .J. RAUWERDA, P. F. SHERRINGTON, W. V. SLITER, E. T. TOZER, T. T. UYENO and .J.B. WATERHOUSE 1974 ©Crown Copyrights reserved Available by mail from Information Canada, Ottawa from the Geological Survey of Canada 601 Booth St., Ottawa and Information Canada bookshops in HALIFAX - 1683 Barrington Street MONTREAL - 640 St. Catherine Street W. OTTAWA - 171 Slater Street TORONTO - 221 Yonge Street WINNIPEG - 393 Portage A venue VANCOUVER - 800 Granville Street or through your bookseller A deposit copy of this publication is also available for reference in public libraries across Canada Price: $3. 00 Catalogue No. M44- 74- 11 Price subject to change without notice Information Canada Ottawa 1974 CONTENTS Page Abstract, Resume. .... .. ... .. ...... ......... .. ........ .. .. ... ..... ... .. ......... .. ...... v Introduction .... ...... ..... ... ... .. .. ... ·. 1 Wells studied and shown in figures la and lb . ... ... ..... .... .. ... .... ... ... ... 1 Corre l ations and identifications of fossils.............. .... .......... ...... .. ... .... .. ..... 4 I .O.E. Taglu G-3 3 .. ...... .. .... .. 4 Elf et aZ . Storker son Bay A-15. .... ... .. .. .. ... .... .... ... ...... ..... .. ..... .. ... 6 Gulf-Mob il East Reindeer G-04. 6 Gulf-Mobil East Reindeer A-01.. ... .. .. .. ... .. ... ... .. .. .. ........... ..... ... 7 B. A.-Shell-I.O . E. Reindeer D- 27 ....... .. .. .. .. .. .. .... ... .. .... ......... .. ....... 7 Banff-Aquitaine - A.R.C. O. Rat Pass K-35 . .. ... .. .. ... .. ....... .......... ... ... ..... .... 7 I .