Mar 19980013: Corkscrew Mountain

Total Page:16

File Type:pdf, Size:1020Kb

Mar 19980013: Corkscrew Mountain MAR 19980013: CORKSCREW MOUNTAIN Received date: Jul 24, 1998 Public release date: Jul 25, 1999 DISCLAIMER By accessing and using the Alberta Energy website to download or otherwise obtain a scanned mineral assessment report, you (“User”) agree to be bound by the following terms and conditions: a) Each scanned mineral assessment report that is downloaded or otherwise obtained from Alberta Energy is provided “AS IS”, with no warranties or representations of any kind whatsoever from Her Majesty the Queen in Right of Alberta, as represented by the Minister of Energy (“Minister”), expressed or implied, including, but not limited to, no warranties or other representations from the Minister, regarding the content, accuracy, reliability, use or results from the use of or the integrity, completeness, quality or legibility of each such scanned mineral assessment report; b) To the fullest extent permitted by applicable laws, the Minister hereby expressly disclaims, and is released from, liability and responsibility for all warranties and conditions, expressed or implied, in relation to each scanned mineral assessment report shown or displayed on the Alberta Energy website including but not limited to warranties as to the satisfactory quality of or the fitness of the scanned mineral assessment report for a particular purpose and warranties as to the non-infringement or other non-violation of the proprietary rights held by any third party in respect of the scanned mineral assessment report; c) To the fullest extent permitted by applicable law, the Minister, and the Minister’s employees and agents, exclude and disclaim liability to the User for losses and damages of whatsoever nature and howsoever arising including, without limitation, any direct, indirect, special, consequential, punitive or incidental damages, loss of use, loss of data, loss caused by a virus, loss of income or profit, claims of third parties, even if Alberta Energy have been advised of the possibility of such damages or losses, arising out of or in connection with the use of the Alberta Energy website, including the accessing or downloading of the scanned mineral assessment report and the use for any purpose of the scanned mineral assessment report so downloaded or retrieved. d) User agrees to indemnify and hold harmless the Minister, and the Minister’s employees and agents against and from any and all third party claims, losses, liabilities, demands, actions or proceedings related to the downloading, distribution, transmissions, storage, redistribution, reproduction or exploitation of each scanned mineral assessment report obtained by the User from Alberta Energy. Alberta Mineral Assessment Reporting System CONTINENTAL LIME LTD. 1997 EXPLORATION NEAR CORKSCREW AND IDLEWILDE MOUNTAINS WEST-CENTRAL ALBERTA Metallic and Industrial Minerals Permit 9396020019 Geographic Coordinates 51°58' N to 52°07' N 115°15' W to 115°31' W NTS Sheets 82 0/13, 0/14, 83 B/3, and B/4 1998 06 29 by D.I. Pana., Ph.D. J.R. Dahrouge, B.Sc., P.Geol. Halferdahl & Associates (a division of Dahrouge Geological Consulting Ltd.) 18, 10509 - 81 Avenue Edmonton, Alberta T6E 1X7 I •• TABLE OF CONTENTS 1. Summary ...................................................... 1 2. Introduction .................................................... 2 3. Geographic Setting and Access .................................... 2 4. Property, Exploration, and Expenditures .............................. 3 4.1 Metallic and Industrial Minerals Permit 9396020019 ............... 3 4.2 1997 Exploration .......................................... 3 4.3 Exploration Expenditures .................................... 5 5. Previous Investigations ........................................... 5 6. Regional Geology ............................................... 6 6.1 Stratigraphy .............................................. 6 6.1.1 Palliser Formation ................................... 6 6.1.2 Sanft Assemblage ................................... 6 6.1.3 Rundle Assemblage .................................. 7 6.2 Structure ............................................... 7 7. Permit Geology . ............................................ 8 7 .1 Stratigraphy ............................................. 8 7 .2 Structure ............................................... 9 8. Sampling, Analyses .............................................. 10 8.1 Sampling ............................................... 10 8.2 Analytical Procedures ...................................... 10 8.3 Statistical Examination of Analyses by Analytical Laboratories ....... 11 8.4 Adjustments to Reported Analyses ............................ 11 9. Conclusions 14 10. References 15 11. Qualifications 17 LIST OF TABLES Page Table 4.1 Information on Metallic and Industrial Minerals Permit 9396020019 I_ of Continental Lime Ltd. at Corkscrew Mountain ............ 3 Table 4.2 Locations Sampled ..................................... 4 I I '-- Table 6.1 Generalized Paleozoic Stratigraphy of Foothills and Front Ranges, West-Central Alberta ..................... 8 Table 8.1 Summary of Statistical Tests for Samples Analyzed by - Acme Analytical Laboratories Ltd., and Continental Lime Inc 12 ' '--' LIST OF ILLUSTRATIONS I I L Fig. 3.1 Location Map .......................................... F1 Fig. 4.1 Metallic and Industrial Minerals Permit 9396020019 F2 Fig. 6.1 Schematic Cross-Section Through Limestone and Corkscrew Mountains F3 I_ Fig. 7.1 Geology and Sample Locations . In Pocket Fig. 7.2 Cross-Section Through ldlewilde Mountain . F4 ! Fig. 7.3 Cross-Section Through Marble Mountain . F5 L LIST OF APPENDICES Appendix 1: Statement of Expenditures i for Metallic and Industrial Permit 9396020019A 1 . A 1 I_ Appendix 2: Descriptions and Compositions of Chip Samples . A2 I_' Appendix 3A: Analytical Reports for ICP Analyses from the Quality Assurance Laboratory of Continental Lime Inc . A 11 Appendix 38: Analytical Report for Check Analyses by Whole Rock ICP from Acme Analytical Laboratories Ltd . A 13 Appendix 3C: Analytical Procedure in the Quality Assurance Laboratory of Continental Lime Inc . A 14 L Appendix4: Two-Tailed Student t-Test for Differences, Sign Test, and Test of Confidence Intervals for Constituent Determinations of Samples collected from Metallic and Industrial Minerals Permit 9396020019 A 15 L Appendix 5: Determined, Adjusted, and Preferred Analyses for CaO and LOI . A23 L Appendix6: Determined and Preferred Concentrations of Chemical Constituents A25 1. SUMMARY At Corkscrew and ldlewilde mountains and within metallic and industrial minerals permit 9396020019, the Upper Devonian to Lower Carboniferous Banff Formation and the Lower Carboniferous Rundle Assemblage were examined for high-calcium limestone. Between August 28 and September 4, 1997, Paleozoic limestone units were measured and examined at 10 locations and 73 samples were collected and analyzed for whole rock constituents and LOI. A total sample length of 203% m was collected from a total of about 346 m normal thickness of strata examined. At three sections more than 135 m of the Banff Formation were examined and 19 samples collected from about 50 m normal thickness of strata. For these samples, concentrations of CaO range from 24.12 to 54.86%, with up to 14. 11 % MgO, and up to 31.88% Si02• At seven sections more than 150 m of the lower Rundle Assemblage were examined and 52 samples collected from about 200 m normal thickness of strata. Concentrations of Cao vary from 41.45 to 55.42%, with up to 11.56% MgO, and up to 2.31% Si02• At one section, two samples were collected from about 1% m stratigraphic thickness of the Mount Head Formation of the uppermost Rundle Assemblage. Concentrations of CaO vary from 49.00 to 50.35%, with up to 5.07% MgO, and up to 1.31% Si02 • Carbonate units examined within the Banff and Mount Head formations are of little economic interest for high-calcium limestone, as they exhibit low concentrations of CaO, and elevated concentrations of MgO, Si02, or both. High-calcium limestone units are present locally within the lower Rundle Assemblage, however thickness and constituent concentrations exhibit variability. 2 2. INTRODUCTION Between August 28 and September 4, 1997, Halferdahl & Associates Ltd. on behalf of Continental Lime Ltd. conducted exploration for high-calcium limestone within west-central Alberta. This assessment report describes the exploration conducted within metallic and industrial minerals permit 9396020019 which encompasses parts of ldlewilde and Corkscrew mountains of the Alberta Foothills. This report contains analytical data from 73 samples collected in 1997, as well L as geologic observations made while collecting these samples and an interpretation of the results. 3. GEOGRAPHIC SETTING AND ACCESS Metallic and industrial minerals permit 9396020019 west of Caroline, Alberta, encompasses the southern part of Baseline Ridge southeast to the Limeco Quarry on Corkscrew Mountain, and west to ldlewilde Mountain, Rocky Creek, and Cutoff Creek. The quarry of Limeco Products Ltd. is at the southeast end of Corkscrew Mountain. Access is from lnnisfail on Alberta Highway 2, 70 I L km westerly on Highway 54, and continuing another 34 km westerly on secondary road 591 and the Forestry Trunk Road (Fig. 3.1). The Forestry Trunk Road continues to the northwest along L the southwest side of Corkscrew Mountain. Near the north end of Corkscrew Mountain a spur of the Forestry Trunk Road continues west along Clearwater River and Cutoff Creek past ldlewilde L Mountain. The northern parts
Recommended publications
  • Paleontology and Stratigraphy of Upper Coniacianemiddle
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 2005 Paleontology and stratigraphy of upper Coniacianemiddle Santonian ammonite zones and application to erosion surfaces and marine transgressive strata in Montana and Alberta W. A. Cobban U.S. Geological Survey T. S. Dyman U.S. Geological Survey, [email protected] K. W. Porter Montana Bureau of Mines and Geology Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Cobban, W. A.; Dyman, T. S.; and Porter, K. W., "Paleontology and stratigraphy of upper Coniacianemiddle Santonian ammonite zones and application to erosion surfaces and marine transgressive strata in Montana and Alberta" (2005). USGS Staff -- Published Research. 367. https://digitalcommons.unl.edu/usgsstaffpub/367 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Cretaceous Research 26 (2005) 429e449 www.elsevier.com/locate/CretRes Paleontology and stratigraphy of upper Coniacianemiddle Santonian ammonite zones and application to erosion surfaces and marine transgressive strata in Montana and Alberta W.A. Cobban a,1, T.S. Dyman b,*, K.W. Porter c a US Geological Survey, Denver, CO 80225, USA b US Geological Survey, Denver, CO 80225, USA c Montana Bureau of Mines and Geology, Butte, MT 59701, USA Received 28 September 2004; accepted in revised form 17 January 2005 Available online 21 June 2005 Abstract Erosional surfaces are present in middle and upper Coniacian rocks in Montana and Alberta, and probably at the base of the middle Santonian in the Western Interior of Canada.
    [Show full text]
  • Blind Thrusts and Fault-Related Folds Int Eh Upper Cretaceous Alberta
    BULLETIN OF CANADIAN PETROLEUM GEOLOGY VOL. 55, NO. 2 (JUNE, 2007), P. 125–137 Blind thrusts and fault-related folds in the Upper Cretaceous Alberta Group, deep basin, west-central Alberta: implications for fractured reservoirs BRUCE S. HART BOGDAN L. VARBAN Department of Earth and Planetary Sciences Department of Earth Sciences McGill University University of Western Ontario 3450 University Street London, ON N6A 5B7 Montreal, QC H3A 2A7 KURT J. MARFURT A. GUY PLINT Allied Geophysics Laboratories Department of Earth Sciences Geosciences Department University of Western Ontario University of Houston London, ON N6A 5B7 Houston, TX 77204-5007 ABSTRACT 3-D seismic and log-based mapping of Upper Cretaceous units in the Deep Basin has revealed the presence of fault-related folds in the Cardium Formation and overlying units. The folds formed above low-angle thrust faults that cut clay-rich shales in the lower part of the Kaskapau Formation. Seismic data indicate a fold wavelength of approximately 5 to 8 km at the Cardium level, with fold axes trending NW-SE. Log-based stratigraphic analyses identified fault repeats of Kaskapau allomembers, whereas the 3-D seismic data show details of upward-branching fault splays and related folds. The faults also splay laterally, and transfer strain by overlapping. Post-stack processing of the original 3-D volume, including noise reduction, coherency processing, and volumetric dip analyses significantly improved our ability to image and map these structures. The Cardium Formation produces oil in the study area from fields with orientations that are approximately parallel to the fold axes. These production trends are thought to be related primarily to depositional trends that predate the structural deformation.
    [Show full text]
  • Allostratigraphic Analysis of the Muskiki and Marshybank Formations
    Allostratigraphic analysis of the Muskiki and Marshybank Formations (Coniacian) in the Central Alberta Foothills and Plains: Possible evidence for an eustatic control on deposition Elizabeth Hooper, Department of Earth Sciences, The University of Western Ontario, London, ON, N6A 5B7 [email protected] and A Guy Plint, Department of Earth Sciences, The University of Western Ontario, London, ON, N6A 5B7 [email protected] Summary The Muskiki and Marshybank formations, of Upper Cretaceous (Coniacian) age, form a major transgressive-regressive depositional cycle, about 100 m thick, that can be mapped throughout the Cretaceous foredeep of Western Canada. Detailed allostratigraphic results are lacking for central Alberta between townships 26 and 44; this study is designed to fill that knowledge gap. The investigation is based on detailed outcrop observation in the Foothills, linked to a regional allostratigraphic framework based on wireline logs. The studied rocks represent primarily shallow- marine environments and are abundantly fossiliferous. The rocks are organized into upward shoaling successions of mudstone and fine sandstone, typically 5-15 m thick. Successions are bounded by marine flooding surfaces that commonly bear pebble lags. Although the upward-shoaling successions resemble simple parasequences, the presence of winnowed pebble lags suggest a terminal period of shallowing and even subaerial emergence. The successions may therefore be interpreted as seaward expressions of depositional sequences. Repeated relative sea-level rise-fall cycles, on a timescale of a few hundred kyr, strongly suggest an eustatic control, plausibly attributable to glacio-eustasy in the Milankovitch band. Introduction The Muskiki and Marshybank formations of the Western Canada Cretaceous foredeep (Stott, 1963, 1967), comprise a major transgressive-regressive depositional cycle, about 100 m thick, that can be mapped from NE British Columbia at least as far south as northern Montana.
    [Show full text]
  • Bedrock Geology of Alberta
    Alberta Geological Survey Map 600 Legend Bedrock Geology of Alberta Southwestern Plains Southeastern Plains Central Plains Northwestern Plains Northeastern Plains NEOGENE (± PALEOGENE) NEOGENE ND DEL BONITA GRAVELS: pebble gravel with some cobbles; minor thin beds and lenses NH HAND HILLS FORMATION: gravel and sand, locally cemented into conglomerate; gravel of sand; pebbles consist primarily of quartzite and argillite with minor amounts of sandstone, composed of mainly quartzite and sandstone with minor amounts of chert, arkose, and coal; fluvial amygdaloidal basalt, and diabase; age poorly constrained; fluvial PALEOGENE PALEOGENE PALEOGENE (± NEOGENE) PALEOGENE (± NEOGENE) UPLAND GRAVEL: gravel composed of mainly white quartzite cobbles and pebbles with lesser amounts of UPLAND GRAVEL: gravel capping the Clear Hills, Halverson Ridge, and Caribou Mountains; predominantly .C CYPRESS HILLS FORMATION: gravel and sand, locally cemented to conglomerate; mainly quartzite .G .G and sandstone clasts with minor chert and quartz component; fluvial black chert pebbles; sand matrix; minor thin beds and lenses of sand; includes gravel in the Swan Hills area; white quartzite cobbles and pebbles with lesser amounts of black chert pebbles; quartzite boulders occur in the age poorly constrained; fluvial Clear Hills and Halverson Ridge gravels; sand matrix; ages poorly constrained; extents poorly defined; fluvial .PH PORCUPINE HILLS FORMATION: olive-brown mudstone interbedded with fine- to coarse-grained, .R RAVENSCRAG FORMATION: grey to buff mudstone
    [Show full text]
  • Western Interior Seaway
    () . Paleogeo.graphy of the Late Cretaceous of the Western Interior otMfddle North America+­ j?'oal .Blstribution anct,Sedimen~cumulation By Laura N. Robinson Roberts and Mark A. Kirschbaum U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1561 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1995 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or finn names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Roberts, Laura N. Robinson. Paleogeography of the Late Cretaceous of the western interior of middle North America : coal distribution and sediment accumulation I by Laura N. Robinson Roberts and Mark A. Kirschbaum. p. em.- (U.S. Geological Survey professional paper ; 1561) Includes bibliographical references. Supt. of Docs. no.: I 19.16: 1561 1. Paleogeography-Cretaceous. 2. Paleogeography-West (U.S.). 3. Coal­ Geology-West (U.S.). I. Kirschbaum, Mark A. II. Title. III. Series. QE50 1.4.P3R63 1995 553.2'1'0978-dc20 94-39032 CIP CONTENTS Abstract........................................................................................................................... 1" Introduction ................................................................................................................... Western Interior Seaway ... .. ... ... ... .. .. ..
    [Show full text]
  • Pgof2000-3 Report.Pdf
    i CONTENTS ABSTRACT 1 INTRODUCTION 2 STRUCTURAL AND TECTONIC FRAMEWORK 2 STRATIGRAPHY AND RESERVOIR DEVELOPMENT 6 Precambrian Purcell Supergroup 6 Cambrian Flathead Sandstone, Gordon Shale, Elko and Windsor Mountain Formations 6 Middle and Upper Devonian Yahatinda, Fairholme Group, Alexo and Sassenach Formations 7 Upper Devonian Palliser Formation 10 Uppermost Devonian and Mississippian Exshaw Formation, Mississippian Banff Formation and Rundle Group 11 Pennsylvanian and Permian Rocky Mountain Supergroup 14 Triassic Spray River Group 15 Jurassic Fernie Formation 16 Jurassic and Lowermost Cretaceous Kootenay Group 17 Lower Cretaceous Blairmore Group 17 Lower Cretaceous Crowsnest Formation 19 Upper Cretaceous Alberta Group and Belly River Formation 20 INTRUSIVE ROCKS 21 EXPLORATION ACTIVITY 22 SOURCE ROCKS AND MATURATION 22 CONVENTIONAL PROSPECTIVE ZONES AND PLAY TYPES 23 Thrust Faulted Paleozoic Strata Below the Lewis Thrust 23 Faulted and Folded Paleozoic Strata Above the Lewis Thrust 26 Fairholme Group Stratigraphic and Combined Stratigraphic-Structural Traps 29 Mesozoic Structural-Stratigraphic Traps Below the Lewis Thrust 30 Mesozoic Structural Traps Above the Lewis Thrust 32 Hydrocarbons in Fractured Precambrian Metasediments 32 COALBED METHANE POTENTIAL IN THE MIST MOUNTAIN FORMATION 33 CONCLUSIONS 38 ACKNOWLEDGMENTS 39 REFERENCES 39 MAP 1. Geological Map of the Flathead and Fernie-Elk Valley areas. MAP 2. Principal prospective trends. MAP 3. Distribution of coal-bearing Jurassic-Cretaceous Kootenay Group and younger strata, showing areas of coalbed methane potential. CROSS SECTION 1. Structural cross section across western Front Ranges, northern part of Elk River Valley and Highrock Range. CROSS SECTION 1a, structural cross section through overturned syncline in northern part of Elk River Valley. ii CROSS SECTION 2.
    [Show full text]
  • Characterization of Sedimentary Bedforms of Colorado Group Mudstones Noor H
    Characterization of Sedimentary Bedforms of Colorado Group Mudstones Noor H. Jafri University of Calgary Introduction In this study, the Second White Specks (2WS) Formation, part of the middle Cretaceous Colorado Group, is analyzed for sedimentary heterogeneity. These Cenomanian-Turonian samples are collected from West- central Alberta. The formation primarily consists of laminated calcareous mudstones with abundant fecal pellets composed of calcareous coccoliths debris representing the “white specs”. Integrating CT datasets from core and outcrop samples, 3D geometry of sedimentary bedforms existing in the 2WS Shales and Jumpingpound sandstone are determined. Background Geology In the Western Canada Foreland Basin, the Cretaceous Colorado Group contains several sandstone and conglomerate units. It is deposited in the warm Tethys Sea during global seal level highs and regional tectonic downflexing of the North American craton. This group is of particular interest as it displays considerable hydrocarbon potential. This light-oil bearing mudstone / marlstone “sequence is a recent addition to the global list of shale resource plays, and an active target of drilling programs” (Mainali et.al, 2014) Within the Colorado group, the Cenomian-Turonian aged 2WS formation consists of two major members: Jumping Pound Sandstone and the Second White Speck Shales. Stratigraphically higher, the Jumping Pound is deposited in a high energy environment, consisting abundant sedimentary ripple bedforms. The 2WS Shale consists primarily of laminated calcareous mudstone with characteristic light colored “specks”. These specks are fecal pellets composed of calcareous coccolithic debris (Goodman, 1951) concentrated by currents. It also has foraminifera (dominantly planktonic), fish scales and bones, abundant Inoceramus prisms, and no or sparse bioturbation (Bloch et al., 1993, Schröder-Adams et al., 1996 and Tyagi et al., 2007).
    [Show full text]
  • Sedimentology of the Cardium Formation Lochend
    SEDIMENTOLOGY OF THE CARDIUM FORMATION LOCHEND FIELD, ALBERTA URBAN DOCUMEN N CENTRE RE!l£ARCH UN URBAN STUDIES STER UNIVERSI~ HAMILTON. ONTARIO SEDIMENTOLOGY OF THE CARDIUM FORMATION (UPPER CRETACEOUS), LOCHEND FIELD, ALBERTA CUMENTATION CE"TR~ ~~:~CH U FOR URBAN STUDIES McMASTE IVERSI"" HAMIlJON, RIO By CERI J. CHAMBERLAIN A Research Paper Submitted to the Department of Geography in Fulfilment of the Requirements of Geography 4C6 McMaster University 1985 HONOURS BACHELOR OF SCIENCE (1985) McMASTER UNIVERSITY (Geog~aphyl Geology) HamiltoD,Ontario TITLE: Sedimentology of the Ca~dium Fo~mation, (Upper cretaceous), Lochend, Alberta AUTHOR: Ceri J. Chamberlain SUPERVISOR: Professor R. G. Walker NUMBER OF PAGES: ix; 82 ii ABSTRACT Examination of 22 cores and over 100 petrophysical logs of the Turonian (Upper Cretaceous) Cardium Formation in the Lochend region permitted the identification of 9 facies which could be arranged into 3 major coarsening-upward cycles. At Lochend, the Burnstick Sequence comprises 5 distinct facies that progressively coarsen upward from a silt laminated mudstone through various bioturbated mud and sand facies into a gravelly conglomerate. There is a sharp return to a dark mud facies. The overlying Raven River sequence in this region is characterized by a double coarsening upwards cycle which can be described in terms of 6 facies. The first cycle coarsens upward from a black laminated mudstone into various bioturbated mud and sand facies. The sands become progressively cleaner upwards before returning to a muddier bioturbated facies which marks the base of the second coarsening upward cycle. This cycle similarly decreases in mud content upwards but never 'cleans' to the extent of the lower cycle.
    [Show full text]
  • Integrated Sedimentology, Sequence Stratigraphy, and Reservoir Characterization of the Basal Spirit River Formation, West-Central Alberta
    University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2017 Integrated sedimentology, sequence stratigraphy, and reservoir characterization of the basal Spirit River Formation, west-central Alberta Newitt, Dillon Newitt, D. (2017). Integrated sedimentology, sequence stratigraphy, and reservoir characterization of the basal Spirit River Formation, west-central Alberta (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/26573 http://hdl.handle.net/11023/3926 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Integrated sedimentology, sequence stratigraphy, and reservoir characterization of the basal Spirit River Formation, west-central Alberta by Dillon Jared Newitt A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE GRADUATE PROGRAM IN GEOLOGY AND GEOPHYSICS CALGARY, ALBERTA JUNE, 2017 © Dillon Jared Newitt 2017 Abstract The basal progradational Falher is comprised of five northward accreting wave- dominated deltaic shoreline parasequence sets within this study area. Well and core based sequence stratigraphy reveals broad facies belts and sharp-based shoreline parasequence sets, reflecting progradation into shallow water; and, an initial strongly progradational to subsequently dominantly aggradational parasequence set stacking pattern within the Spirit River Formation clastic wedge.
    [Show full text]
  • Stratigraphy and Sedimentology of the Late Cretaceous (Coniacian) Muskiki and Marshybank Members, Southern Alberta and Northwestern Montana
    Western University Scholarship@Western Electronic Thesis and Dissertation Repository 10-17-2012 12:00 AM Stratigraphy and Sedimentology of the Late Cretaceous (Coniacian) Muskiki and Marshybank Members, Southern Alberta and Northwestern Montana Meriem Grifi The University of Western Ontario Supervisor Dr. A. Guy Plint The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Master of Science © Meriem Grifi 2012 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geology Commons Recommended Citation Grifi, Meriem, "Stratigraphy and Sedimentology of the Late Cretaceous (Coniacian) Muskiki and Marshybank Members, Southern Alberta and Northwestern Montana" (2012). Electronic Thesis and Dissertation Repository. 917. https://ir.lib.uwo.ca/etd/917 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. STRATIGRAPHY AND SEDIMENTOLOGY OF THE LATE CRETACEOUS (CONIACIAN) MUSKIKI AND MARSHYBANK MEMBERS, SOUTHERN ALBERTA AND NORTHWESTERN MONTANA Spine Title: Stratigraphy and Sedimentology of the Muskiki and Marshybank Members Thesis format: Monograph By Meriem GRIFI Graduate Program in Geology A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science The School of Graduate and Postdoctoral Studies The University of Western Ontario London, Ontario, Canada ©Meriem Grifi 2012 i THE UNIVERSITY OF WESTERN ONTARIO SCHOOL OF GRADUATE AND POSDOCTORAL STUDIES CERTIFICATE OF EXAMINATION Supervisor Examiners __________________________ __________________________ Dr. A.
    [Show full text]
  • Prepared For
    Terasen Pipelines (Trans Mountain) Inc. Geotechnical Report TMX - Anchor Loop Project November 2005 EXECUTIVE SUMMARY With the TMX - Anchor Loop Project (the “Project”) Terasen Pipelines (Trans Mountain) Inc. (“Terasen Pipelines”) proposes to loop a portion of its existing National Energy Board (“NEB”) regulated oil pipeline system (the “Trans Mountain pipeline” or “Trans Mountain”) to increase the capacity of the Trans Mountain pipeline to meet growing shipper demand. The Project involves the construction of 158 km of 812 mm or 914 mm (32-inch or 36-inch) diameter pipe between a location west of Hinton, Alberta at Kilometre Post/Kilometre Loop (“KP/KL") 310.1 and a location near Rearguard, British Columbia (BC) (KP/KL 468.0). The Project also includes the installation of two new pump stations at locations along the Trans Mountain pipeline, one in Alberta at Wolf (KP 188.0) and one in BC, at Chappel (KP 555.5), and the installation of associated aboveground facilities including block valves at several locations and a receiving trap for pipeline cleaning and inspection tools at a location near Rearguard, BC (KP/KL 468.0). Construction of the Project will require temporary construction camps and other temporary work yards. The Project will traverse federal, provincial and private lands, including Jasper National Park (JNP) in Alberta and Mount Robson Provincial Park (MRPP) in BC. This technical report has been prepared to support the Environmental and Socio-Economic Assessment section of the Section 52 application to the NEB. It has been designed to satisfy the information requirements identified in the Scope and Requirements of the Environmental Assessment for the Terasen Pipelines (Trans Mountain) Inc.
    [Show full text]
  • (Cretaceous), Western Canada Sedimentary Basin – a Preliminary Report
    Organic Facies Analysis of the Cretaceous Lower and Basal Upper Colorado Group (Cretaceous), Western Canada Sedimentary Basin – A Preliminary Report L. Buckley 1 and R.V. Tyson 1 Buckley, L. and Tyson, R.V. (2003): Organic facies analysis of the Cretaceous Lower and basal Upper Colorado Group (Cretaceous), Western Canada Sedimentary Basin – a preliminary report; in Summary of Investigations 2003, Volume 1, Saskatchewan Geological Survey, Sask. Industry Resources, Misc. Rep. 2003-4.1, CD-ROM, Paper A-10, 13p. Abstract The Cretaceous Colorado Group (Albian-Santonian) is a sequence of dominantly homogeneous organic-rich shales derived from sediments deposited within the Western Interior Seaway of North America. Bulk geochemical analysis (Rock-Eval, TOC, Total Carbon, and Total Sulphur), and palynofacies observations have been conducted on 452 core samples in order to reconstruct the organic facies variations through the lower part of the Group and along transects across the Canadian portion of the Western Interior Seaway. The Viking and Westgate formations are typified by low percentages of poorly preserved (weakly fluorescent) marine amorphous organic matter (AOM) and abundant terrestrial phytoclasts, associated with low TOC and average measured hydrogen indices of only 106 mgHC/gTOC (Type III kerogen). The Fish Scales and Belle Fourche formations have a transitional organic facies reflecting mixing with better preserved marine AOM, and thus exhibit higher mean TOC and measured HI values (158 and 170 respectively). The Second White Specks Formation and the basal Upper Colorado Group are both dominated by moderate to strongly fluorescent AOM, resulting in a mean measured HI of 320 (Type II kerogen).
    [Show full text]