Besa River Formation in Liard Basin, Southeast Yukon: Report on 2012 Reconnaissance Fieldwork
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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. -
Faults and Associated Karst Collapse Suggest Conduits for Fluid Flow That Influence Hydraulic Fracturing-Induced Seismicity
Faults and associated karst collapse suggest conduits for fluid flow that influence hydraulic fracturing- induced seismicity Elwyn Gallowaya, Tyler Haucka, Hilary Corlettb, Dinu Pana˘ a, and Ryan Schultza,1 aAlberta Geological Survey, Alberta Energy Regulator, Edmonton, AB T8N 3A3, Canada; and bDepartment of Physical Sciences, MacEwan University, Edmonton, AB T5J 4S2, Canada Edited by Paul Segall, Stanford University, Stanford, CA, and approved August 21, 2018 (received for review May 1, 2018) During December 2011, a swarm of moderate-magnitude earth- bore [up to hundreds of meters (18–21)]. Furthermore, geo- quakes was induced by hydraulic fracturing (HF) near Cardston, mechanical modeling reveals that poroelastic changes from HF Alberta. Despite seismological associations linking these two processes, are transmitted only locally (20). These results are in direct the hydrological and tectonic mechanisms involved remain unclear. In contradiction to HF-related earthquakes that are located kilo- this study, we interpret a 3D reflection-seismic survey to delve into the meters away from the closest well bore (e.g., refs. 2, 6, 11, 22, and geological factors related to these earthquakes. First, we document a 23). Specific to the Cardston case, earthquakes (located on re- basement-rooted fault on which the earthquake rupture occurred that gional arrays) were observed within the uppermost crystalline ∼ – extends above the targeted reservoir. Second, at the reservoir’s strati- basement, 1.5 km deeper than the target upper Stettler Big SI Appendix graphic level, anomalous subcircular features are recognized along the Valley Reservoir zone ( ,Fig.S1); this observation is fault and are interpreted as resulting from fault-associated karst pro- further complicated by the fact that the fault slip response oc- ∼ – cesses. -
Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area
ERCB/AGS Special Report 093 Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Stefan Bachu Maja Buschkuehle Kristine Haug Karsten Michael Alberta Geological Survey Alberta Energy and Utilities Board ©Her Majesty the Queen in Right of Alberta, 2008 ISBN 978-0-7785-6950-3 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS) and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions. The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release, do not constitute endorsement by the ERCB/AGS of any manufacturer's product. If this product is an ERCB/AGS Special Report, the information is provided as received from the author and has not been edited for conformity to ERCB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the ERCB/AGS. The following reference format is recommended: Bachu, S., Buschkuehle, M., Haug, K., Michael, K. (2008): Subsurface characterization of the Pembina-Wabamun acid-gas injection area; Energy Resources Conservation Board, ERCB/AGS Special Report 093, 60 p. -
Geochemical, Petrophysical and Geomechanical Properties Of
Geochemical, petrophysical and geomechanical properties of stratigraphic sequences in Horn River Shale, Middle and Upper Devonian, Northeastern British Columbia, Canada by TIAN DONG A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Earth and Atmospheric Sciences University of Alberta © Tian Dong, 2016 ABSTRACT The Middle and Upper Devonian Horn River Shale, comprising the Evie and Otter Park members and the Muskwa Formation, northeast British Columbia, Canada is recognized as a significant shale gas reservoir in the Western Canada Sedimentary Basin. However, many aspects of this shale formation have not been adequately studied, and the published geochemical, petrophysical and geomechanical data are limited. This work aims to document the controls of geochemical composition variation on petrophysical and geomechanical properties and the relationship of rock composition to lithofacies and stratigraphic sequences. A detailed core-based sedimentological and wireline log analysis was conducted by my colleague Dr. Korhan Ayranci as a parallel study, in order to classify lithofacies, interpret depositional environments and establish sequence stratigraphic framework across the basin. Major and trace elements concentrations, key trace element ratios and Corg-Fe-S relationships were used to understand the effect of sea level fluctuation on detrital flux, redox conditions, productivity and therefore organic carbon enrichment patterns. Detrital sediment flux indicated by the concentration of aluminum and titanium to the basin was found to be higher during transgressions than regressions. Redox conditions, exhibiting strong correlation to TOC content, were the primary controls on the organic carbon deposition. The bottom water conditions are more anoxic during transgressions than regressions. -
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. -
Liard Basin Hydrocarbon Project: Shale Gas Potential of Devonian-Carboniferous Strata in the Northwest Territories, Yukon and Northeastern British Columbia
Liard Basin Hydrocarbon Project: Shale Gas Potential of Devonian-Carboniferous Strata in the Northwest Territories, Yukon and Northeastern British Columbia Kathryn M. Fiess, Northwest Territories Geoscience Office, Yellowknife, NT [email protected] and Filippo Ferri, Oil and Gas Division, BC Ministry of Energy, Mines and Natural Gas, Victoria, BC [email protected] and Tiffani L. Fraser, Yukon Geoscience Survey, Whitehorse, YT [email protected] and Leanne J. Pyle, VI Geoscience Services Ltd., Brentwood Bay, BC [email protected] and Jonathan Rocheleau, Northwest Territories Geoscience Office, Yellowknife, NT [email protected] Summary The Liard Basin Hydrocarbon Project was initiated in 2012 to examine the shale gas potential of Middle Devonian to Carboniferous strata based on integrated subsurface and outcrop-based field studies. The project is a collaboration of the Northwest Territories Geoscience Office (NTGO) with the Yukon Geological Survey, the British Columbia Ministry of Energy, Mines and Natural Gas and the Geological Survey of Canada. The primary objective of the project is to evaluate source rocks and refine stratigraphic correlation within the basinal succession of the Middle to Upper Devonian Besa River Formation and its Horn River “Formation” equivalents (Evie, Otter Park, and Muskwa members), as well as the Upper Devonian to Mississippian Exshaw Formation and Mississippian Golata Formation. The Liard Basin lies within three jurisdictions: the Northwest Territories (NT), Yukon (YK) and British Columbia (BC). In northeast BC it hosts several gas fields but remains largely underexplored in the NT and YK. During the initial field season, more than 500 m of strata were measured and described from three sections: 1) Golata Formation in the NT; 2) Besa River Formation in the YK; and 3) Besa River Formation in northeast BC. -
Appendix E-1-1: Acid Rock Drainage and Metal Leaching Field Investigation
AMEC Earth & Environmental a division of AMEC Americas Limited 2227 Douglas Road, Burnaby, BC Canada V5C 5A9 Tel +1 (604) 294-3811 Fax +1 (604) 294-4664 www.amec.com Acid Rock Drainage and Metal Leaching Field Investigation Enbridge Northern Gateway Project Submitted to: Northern Gateway Pipelines Inc. Calgary, AB Submitted by: AMEC Earth & Environmental, a division of AMEC Americas Limited Burnaby, BC October 2009 Revised February 16, 2010 AMEC File: EG09260.2300 Document Control No.: 1128-RG-20091022 Northern Gateway Pipelines Inc. Acid Rock Drainage and Metal Leaching Field Investigation October 2009 Revised February 16, 2010 TABLE OF CONTENTS Page LIST OF ABBREVIATIONS .......................................................................................................... v GLOSSARY ................................................................................................................................ vi EXECUTIVE SUMMARY .............................................................................................................. 1 1.0 INTRODUCTION .................................................................................................................. 2 1.1 Background ................................................................................................................. 2 1.2 Scope of Work ............................................................................................................. 2 2.0 INTRODUCTION TO ACID ROCK DRAINAGE .................................................................. -
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 -
Upper Devonian and Lower Mississippian Stratigraphy
UPPER DEVONIAN AND LOWER MISSISSIPPIAN STRATIGRAPHY OF NORTHWESTERN MONTANA: A PETROLEUM SYSTEM APPROACH by Paul S. Schietinger A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date _____________ Signed: ____________________________ Paul S. Schietinger Signed: ____________________________ Dr. Stephen A. Sonnenberg Thesis Advisor Golden, Colorado Date _____________ Signed: ____________________________ Dr. John D. Humphrey Professor and Head Department of Geology and Geological Engineering ii ABSTRACT The Upper Devonian and Lower Mississippian stratigraphy in the Antler foreland basin of northwestern Montana is the current focus of exploration for several petroleum companies. Conodont zonation indicates that the Exshaw Formation of southern Alberta and northern Montana is Late Devonian and Early Mississippian in age, and is stratigraphically equivalent to the Bakken Formation in the Williston Basin and the Sappington Member of the Three Forks in southwestern Montana. The Exshaw, Bakken and Sappington are lithologically similar. Each formation is comprised of basal organic-rich shale, middle dolomitic siltstone and sandstone, and upper organic-rich shale. The Three Forks Formation in northwestern Montana consists of two members: the older Logan Gulch Member and the younger Trident Member. The Logan Gulch is 100 ft to over 450 ft thick and was subdivided in this study into three facies that were deposited in salina to sabkha environments. Locally, the Logan Gulch is termed the Potlatch Anhydrite. The Three Forks Formation in northwestern Montana is equivalent to the Stettler and Big Valley formations in southern Alberta. The younger Trident Member was subdivided into two facies that are transgressive, open marine deposits. -
Bc12 Report.Pdf
Soils of the Fort Nelson Area of British Columbia K.W. G. VALENTINE Canada Department of Agriculture, Vancouver, B.C. REPORT No. 12 British Columbia Soi1 Survey Research Branch - Canada Department of Agriculture. 1971 3 ACKNOWLEDGMENTS The author wishes to acknowledge the help of Mr. L. Farstad, Canada Depart- ment of Agriculture, Vancouver, and Mr. P. N. Sprout, British Columbia Depart- ment of Agriculture, Kelowna, who initiated the project and gave constructive advice during various parts of the field and office work. Mr. D. Hodgson helped with the field work in the summer of 1967. Soi1 analyses were carried out by Mr. S. K. Chan and Miss M. E. Turnbull. Mr. J. M. Wallace, Department of Energy, Mines, and Resources, Water Resources Branch, Vancouver, B.C., provided valuable information on the seasonal flood levels of the Muskwa and Fort Nelson rivers., Mr. R. A. Nemeth, pipeline engineer, Westcoast Transmission CO. Ltd., Van- couver, gave permission for information from his company’s Yoyo pipeline muskeg survey to be used in Fig. 5. Dr. H. Vaartnou, Research Station, Canada Department of Agriculture, Beaverlodge, Alta., identified many of the plant specimens that were collected during the survey. Mr. G. W. Robertson, Agrometeorology Section, Canada Department of Agri- culture, Ottawa, supplied estimates of agroclimatic normals based on the Hopkins regression formulas. Mr. R. Marshall, Agroclimatology, British Columbia Depart- ment of Agriculture, also supplied much climatic data. The soi1 map and Fig. l-5, 11, 13, 15, and 16 were prepared by the Cartogra- phy Section, Soi1 Research Institute, Canada Department of Agriculture, Ottawa. Messrs. -
Quarterly Report on Short-Term Water Approvals and Use
Quarterly Report on Short-Term Water Approvals and Use April to June 2011 About the BC Oil and Gas Commission The BC Oil and Gas Commission is an independent, single-window regulatory agency with responsibilities for overseeing oil and gas operations in British Columbia, including exploration, development, pipeline transportation and reclamation. The Commission’s core roles include reviewing and assessing applications for industry activity, consulting with First Nations, ensuring industry complies with provincial legislation and cooperating with partner agencies. The public interest is protected through the objectives of ensuring public safety, protecting the environment, conserving petroleum resources and ensuring equitable participation in production. TABLE OF CONTENTS Introduction Page 2 Processes and Requirements Page 3 Results Page 4 Summary Page 7 Appendix A Page 8 Appendix B Page 9 Appendix C Page 12 1 BC Oil and Gas Commission Quarterly Report on Short-Term Water Approvals and Use Introduction The Oil and Gas Activities Act (OGAA) provides authority to the BC Oil and Gas Commission (Commission) to issue short-term water use approvals under Section 8 of the Water Act to manage short-term water use by the oil and gas industry. Approvals under Section 8 of the Water Act authorize the diversion and use of water for a term not exceeding 12 months. This report details the Commission’s responsibilities and authorities under Section 8 of the Water Act; it does not include the diversion and use of water approved by other agencies (such as the Ministry of Forests, Lands and Natural Resource Operations, which has responsibility for water licensing) or for purposes other than oil and gas activities.