A Robust and Practical Approach to VTI Parameter Estimation in a Non-Structural Setting: Case Study from the Vulcan Field, Alberta

Total Page:16

File Type:pdf, Size:1020Kb

A Robust and Practical Approach to VTI Parameter Estimation in a Non-Structural Setting: Case Study from the Vulcan Field, Alberta A robust and practical approach to VTI parameter estimation in a non-structural setting: case study from the Vulcan field, Alberta Mike Perz*, Warren Pearson**, Darren Betker, and Earl Heather, Divestco Processing, Calgary, Alberta, Canada **Pradera Resources Inc., Calgary, Alberta Canada Natural gas exploration in a mature producing region requires the introduction of innovative techniques in order to optimize resource exploitation. One such approach involves interpreting the AVO characteristics of prospective gas targets in order to improve drilling success and overall project economics. Throughout the plains of Southern Alberta, an inherent problem in AVO analysis is the presence of strong Vertical Transverse Isotropy (VTI) within the marine shales of the Edmonton Group and Colorado Group. Published outcrop based refraction data in the Upper Colorado shales have documented velocity anisotropy in the order of 12%, further confirmed by the analysis of walkaway VSP data. Correcting for the non-hyperbolic moveout effects of VTI is not a new concept; however practical and robust estimation of the anisotropic parameters which underlie such a correction scheme is still a topic of great interest to the explorationist, especially in the absence of external information like walkaway VSP's, checkshot data, or detailed measurements of rock parameters. In this paper we will demonstrate a robust approach to VTI parameter estimation which is consistent with our a priori assumptions of the underlying geology. Compared to conventional isotropic processing, this approach provides superior moveout correction of far offset data for the purposes of AVO analysis, as well as improved focusing in the poststack image. We will show real and synthetic data examples to illustrate the merits of the proposed VTI velocity correction methodology in the context of interpreting the Class II AVO response of the Belly River Group gas resource. GeoCanada 2010 – Working with the Earth 1 .
Recommended publications
  • Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses By
    Histology and Ontogeny of Pachyrhinosaurus Nasal Bosses by Elizabeth Kruk A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Systematics and Evolution Department of Biological Sciences University of Alberta © Elizabeth Kruk, 2015 Abstract Pachyrhinosaurus is a peculiar ceratopsian known only from Upper Cretaceous strata of Alberta and the North Slope of Alaska. The genus consists of three described species Pachyrhinosaurus canadensis, Pachyrhinosaurus lakustai, and Pachyrhinosaurus perotorum that are distinguishable by cranial characteristics, including parietal horn shape and orientation, absence/presence of a rostral comb, median parietal bar horns, and profile of the nasal boss. A fourth species of Pachyrhinosaurus is described herein and placed into its phylogenetic context within Centrosaurinae. This new species forms a polytomy at the crown with Pachyrhinosaurus canadensis and Pachyrhinosaurus perotorum, with Pachyrhinosaurus lakustai falling basal to that polytomy. The diagnostic features of this new species are an apomorphic, laterally curved Process 3 horns and a thick longitudinal ridge separating the supraorbital bosses. Another focus is investigating the ontogeny of Pachyrhinosaurus nasal bosses in a histological context. Previously, little work has been done on cranial histology in ceratopsians, focusing instead on potential integumentary structures, the parietals of Triceratops, and how surface texture relates to underlying histological structures. An ontogenetic series is established for the nasal bosses of Pachyrhinosaurus at both relative (subadult versus adult) and fine scale (Stages 1-5). It was demonstrated that histology alone can indicate relative ontogenetic level, but not stages of a finer scale. Through Pachyrhinosaurus ontogeny the nasal boss undergoes increased vascularity and secondary remodeling with a reduction in osteocyte lacunar density.
    [Show full text]
  • Dinosaur Eggshells from the Lower Maastrichtian St. Mary River Formation of Southern Alberta, Canada
    Canadian Journal of Earth Sciences Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern Alberta, Canada Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2017-0195.R1 Manuscript Type: Article Date Submitted by the Author: 13-Nov-2017 Complete List of Authors: Voris, Jared; University of Calgary, Geoscience; Zelenitsky, Darla; Department of Geoscience, Tanaka, Kohei; Nagoya Daigaku Hakubutsukan; University of Calgary, DepartmentDraft of Geoscience Therrien, François; Royal Tyrrell Museum of Palaeontology, Is the invited manuscript for consideration in a Special N/A Issue? : Keyword: eggshell, dinosaur, Cretaceous, Maastrichtian, Alberta https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 47 Canadian Journal of Earth Sciences 1 2 3 4 5 6 7 8 9 Dinosaur eggshells from the lower Maastrichtian St. Mary River Formation of southern 10 Alberta, Canada 11 12 Jared T. Voris, Darla K. Zelenitsky,Draft François Therrien, Kohei Tanaka 13 J. T. Voris, D. K. Zelenitsky, and K. Tanaka. Department of Geoscience, University of 14 Calgary, 2500 University Dr. NW, Calgary, AB T2N 1N4, Canada; [email protected], 15 [email protected], [email protected] 16 K. Tanaka. Nagoya University Museum, Nagoya University Furocho, Chikusa-Ku, Nagoya, 17 464-8601, Japan; [email protected] 18 F. Therrien. Royal Tyrrell Museum of Palaeontology, Box 7500, Drumheller, AB T0J 0Y0, 19 Canada.; [email protected] 20 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 47 1 2 Abstract–North America is known for its rich uppermost Cretaceous record of dinosaur egg 3 remains, although a notable fossil gap exists during the lower Maastrichtian.
    [Show full text]
  • 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.
    [Show full text]
  • 3Rd-Order Sequence Stratigraphy and Lithostratigraphy of the Bearpaw–Horseshoe Canyon Transition, Alberta Plains
    3rd-order sequence stratigraphy and lithostratigraphy of the Bearpaw–Horseshoe Canyon transition, Alberta plains Ben Hathway, Alberta Geological Survey, Alberta Energy Regulator, Edmonton, Alberta, [email protected] Summary The regional-scale delineation and modelling of upper and lower boundaries and zero edges for the Bearpaw Formation tongues in southern and central Alberta forms an important component of a wider AGS project to construct a digital 3D geological framework for the Alberta subsurface. Core and high-quality wireline logs, generated to a large extent by recent coal-bed methane drilling, permit the establishment of a 3rd-order sequence stratigraphic framework. This provides a context within which lithostratigraphic boundaries of the Bearpaw Formation with laterally equivalent and overlying Horseshoe Canyon and St. Mary River formation strata can be more rigorously mapped. Lower boundaries of the Bearpaw tongues are 3rd-order transgressive, or more proximally, maximum flooding surfaces, and upper boundaries are highly diachronous facies contacts within successive regressive systems tracts. Introduction The complex nature of the intertonguing relationship between Campanian-Maastrichtian (Upper Cretaceous) Bearpaw Formation marine shale and fluviodeltaic nonmarine and shoreline deposits of the Horseshoe Canyon and St. Mary River formations in central and southern Alberta has long been recognized (e.g. Russell, 1932; Irish, 1970). Following earlier work focused on high-resolution, 4th-order sequence analysis of the stratigraphically limited part of the Bearpaw–Horseshoe Canyon transition exposed along the Red Deer River valley (e.g. Rahmani, 1988; Ainsworth, 1994), the first regional sequence stratigraphic study of the succession was undertaken by Catuneanu et al. (1997). In that study increasing and decreasing trends in wireline gamma-ray response were used to delineate up to 11 3rd-order transgressive-regressive (T-R) sequences within the Bearpaw Formation.
    [Show full text]
  • Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
    www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5.
    [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]
  • Possible Evidence of Gregarious Behavior in Tyrannosaurids
    GAIA N'15, LlSBOAlLISBON, DEZEMBRO/DECEMBER 1998, pp. 271-277 (ISSN: 0871-5424) POSSIBLE EVIDENCE OF GREGARIOUS BEHAVIOR IN TYRANNOSAURIDS Philip J. CURRIE Royal Tyrrell Museum of Palaeontology. Box 7500 Drumheller, ALBERTA TOJ OYO. CANADA ABSTRACT: In 1910, a collecting party from the American Museum of Natural History led by Barnum Brown floated down the Red Deer Riverof Alberta. In the Horseshoe Canyon Forma­ tion (Edmonton Group, Campanian-Maastrichtian, Upper Cretaceous) close to the mouth of Big Valley Creek, they excavated semi-articulated skeletons of several individuals of Alber­ tosaurus sarcophagus OSBORN, 1905 from a single quarry. Other than the tyrannosaurids, only two hadrosaur phalanges were recovered. Eight articulated feet with associated limb bones were given catalogue numbers, as was an articulated string oftwenty-five caudal ver­ tebrae_ The remaining tyrannosaurid fossils that could not be associated with any of these specimens or with each other were all assigned a single number. Brown's other discoveries of well-preserved dinosaur skeletons in southern Alberta overshadowed the tyrannosaurid find, and the specimens were largely forgotten. However, it is the best evidence that exists to suggest that tyrannosaurids may have been gregarious animals. The almost complete lack of herbivore bones from the excavation suggests that this was probably not a predator trap, such as has been postulated for the Allosaurus MARSH, 1877 accumulation at the Cleveland-Lloyd Quarry near Price, Utah. Comparative measurements indicate that juvenile tyrannosaurids were probably almost as fast at running as ornithomimids. This suggests a division of labor amongst a hunting pack of tyrannosaurids. INTRODUCTION in the Department of Vertebrate Paleontology, American Museum of Natural History).
    [Show full text]
  • Valley Line Stage 1 Environmental Impact Screening Assessment
    Spencer Environmental Appendix H. Historical Resources Reports July 2013 Valley Line-Stage 1 EISA Page H1 HISTORICAL RESOURCES IMPACT ASSESSMENT SOUTHEAST LRT ALIGNMENT IN LSD 15-33-52-24-W4M IN THE CITY OF EDMONTON FINAL REPORT ARCHAEOLOGY PERMIT 2011-249 Prepared for Art Washuta AECOM 17007 -107 Avenue Edmonton, Alberta T5S 1G3 Tel. (780) 486-7000 Fax (780) 486-7070 E-mail: [email protected] By The Archaeology Group 2526 Bell Court S.W. Edmonton, Alberta T6W 1J8 Tel. 780.438.4262 Fax 780.439.4285 Cell 780.242.4262 E-mail: [email protected] January, 2012 This document contains sensitive information about Historic Resources that are protected under provisions of the Alberta Historical Resources Act. This information is to be used to assist in planning the proposed project only. It is not to be disseminated, and no copies of this document are to be made without written permission of Historic Resources Management Branch, Alberta Culture and Community Spirit. Historical Resources Impact Assessment Southeast LRT Alignment In LSD 15-33-52-24-W4M ii REPORT ABSTRACT At the request of Art Washuta of AECOM, on behalf of the City of Edmonton, an Historical Resources Impact Assessment (HRIA) was conducted for a proposed preliminary design project for a proposed Southeast LRT alignment in LSD 15-33- 52-24-W4M, in the City of Edmonton, Alberta. The fieldwork for this project was undertaken between October 5 and 25, 2011. The HRIA survey area consists of a strip of land approximately 100 metres long by 25 metres wide extending from the sidewalk at the south end of the footbridge over the North Saskatchewan River across a gully up to the edge of 98 Avenue.
    [Show full text]
  • Redalyc.The Last Dinosaurs of Brazil: the Bauru Group and Its
    Anais da Academia Brasileira de Ciências ISSN: 0001-3765 [email protected] Academia Brasileira de Ciências Brasil BRUSATTE, STEPHEN L.; A. CANDEIRO, CARLOS R.; SIMBRAS, FELIPE M. The last dinosaurs of Brazil: The Bauru Group and its implications for the end-Cretaceous mass extinction Anais da Academia Brasileira de Ciências, vol. 89, núm. 3, julio-septiembre, 2017, pp. 1465-1485 Academia Brasileira de Ciências Rio de Janeiro, Brasil Available in: http://www.redalyc.org/articulo.oa?id=32752675010 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Anais da Academia Brasileira de Ciências (2017) 89(3): 1465-1485 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201720160918 www.scielo.br/aabc | www.fb.com/aabcjournal The last dinosaurs of Brazil: The Bauru Group and its implications for the end-Cretaceous mass extinction STEPHEN L. BRUSATTE1, CARLOS R.A. CANDEIRO2 AND FELIPE M. SIMBRAS3 1School of GeoSciences, University of Edinburgh, Grant Institute, James Hutton Road, EH9 3FE, Edinburgh, United Kingdom 2Laboratório de Paleontologia e Evolução, Curso de Geologia, Campus Aparecida de Goiânia, Universidade Federal de Goiás, Rua Mucuri, s/n, Área 03, St. Conde dos Arcos, 74968-755 Aparecida de Goiânia, GO, Brazil 3Petróleo Brasileiro S.A. (PETROBRAS), Av. República do Chile, 330, 17˚ andar, Centro, 20031-170 Rio de Janeiro, RJ, Brazil Manuscript received on December 12, 2016; accepted for publication on March 24, 2017 ABSTRACT The non-avian dinosaurs died out at the end of the Cretaceous, ~66 million years ago, after an asteroid impact.
    [Show full text]
  • Measured Outcrop Section T17-R3W4-01 of the Foremost
    ERCB/AGS Open File Report 2011-04 Measured Outcrop Section T17-R3W4-01 of the Foremost, Oldman and Dinosaur Park Formations (Belly River Group), White Rock Coulée, South Saskatchewan River Valley, Southeastern Alberta (NTS 72L/08) ERCB/AGS Open File Report 2011-04 Measured Outcrop Section T17-R3W4-01 of the Foremost, Oldman and Dinosaur Park Formations (Belly River Group), White Rock Coulée, South Saskatchewan River Valley, Southeastern Alberta (NTS 72L/08) B. Hathway, C.J. Banks and D.C. Hay Energy Resources Conservation Board Alberta Geological Survey June 2011 ©Her Majesty the Queen in Right of Alberta, 2011 ISBN 978-0-7785-8642-5 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS), 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 reference to proprietary software and/or any use of proprietary data formats do not constitute endorsement by ERCB/AGS of any manufacturer's product. If you use information from this publication in other publications or presentations, please acknowledge the ERCB/AGS. We recommend the following reference format: Hathway, B., Banks, C.J. and Hay, D.C. (2011): Measured outcrop section T17-R3W4-01 of the Foremost, Oldman and Dinosaur Park formations (Belly River Group), White Rock Coulée, South Saskatchewan River valley, southeastern Alberta (NTS 72L/08); Energy Resources Conservation Board, ERCB/AGS Open File 2011-04, 14 p. Published June 2011 by: Energy Resources Conservation Board Alberta Geological Survey 4th Floor, Twin Atria Building 4999 – 98th Avenue Edmonton, AB T6B 2X3 Canada Tel: 780.422.1927 Fax: 780.
    [Show full text]
  • Ankylosaur and Theropod Coevolution Dinosauriekrig: Samevolution Hos Ankylosaurier Och Theropoder
    Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 401 Dinosaur Warfare: Ankylosaur and Theropod Coevolution Dinosauriekrig: samevolution hos ankylosaurier och theropoder Christopher Freer INSTITUTIONEN FÖR GEOVETENSKAPER DEPARTMENT OF EARTH SCIENCES Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 401 Dinosaur Warfare: Ankylosaur and Theropod Coevolution Dinosauriekrig: samevolution hos ankylosaurier och theropoder Christopher Freer ISSN 1650-6553 Copyright © Christopher Freer Published at Department of Earth Sciences, Uppsala University (www.geo.uu.se), Uppsala, 2017 Abstract Dinosaur Warfare: Ankylosaur and Theropod Coevolution Christopher Freer Ankylosauria is a clade of armoured dinosaurs that, throughout the Mesozoic, demonstrates divergent evolution of defensive traits, between the robust spikes and osteoderms of nodosaurids to the ankylosaurid tail clubs and lightweight armour. One of the longer-standing hypotheses, which is supported by histological data, stipulates that armament was a direct result of a predator-prey relationship between theropods and ankylosaurians. Such a hypothesis predicts that predatory pressures from Theropoda drive the evolution of armament. Here we investigate the coevolutionary hypothesis in a phylogenetic context by searching for reciprocal selection and clade interactions. We undertake two separate analyses. The first is a host-parasite test (ParaFit), which tests, within a phylogenetic framework, the null hypothesis that the evolutionary history of two groups was independent. The second produced principal coordinates from 30 ankylosaurian armour-related traits and was correlated in a linear regression against theropod body mass. The analysis was conducted across 53 theropod species that were sympatric, within a geological formation, with 44 ankylosaur species.
    [Show full text]
  • A New Arctic Hadrosaurid from the Prince Creek Formation (Lower Maastrichtian) of Northern Alaska
    Editors' choice A new Arctic hadrosaurid from the Prince Creek Formation (lower Maastrichtian) of northern Alaska HIROTSUGU MORI, PATRICK S. DRUCKENMILLER, and GREGORY M. ERICKSON Mori, H., Druckenmiller, P.S., and Erickson, G.M. 2016. A new Arctic hadrosaurid from the Prince Creek Formation (lower Maastrichtian) of northern Alaska. Acta Palaeontologica Polonica 61 (1): 15–32. The Liscomb bonebed in the Price Creek Formation of northern Alaska has produced thousands of individual bones of a saurolophine hadrosaurid similar to Edmontosaurus; however, the specific identity of this taxon has been unclear, in part because the vast majority of the remains represent immature individuals. In this study, we address the taxonomic status of the Alaskan material through a comparative and quantitative morphological analysis of juvenile as well several near adult-sized specimens with particular reference to the two known species of Edmontosaurus, as well as a cladistic analysis using two different matrices for Hadrosauroidea. In the comparative morphological analysis, we introduce a quantitative method using bivariate plots to address ontogenetic variation. Our comparative anatomical analysis reveals that the Alaskan saurolophine possesses a unique suite of characters that distinguishes it from Edmontosaurus, including a premaxillary circumnarial ridge that projects posterolaterally without a premaxillary vestibular promontory, a shallow groove lateral to the posterodorsal premaxillary foramen, a relatively narrow jugal process of the postorbital lacking a postorbital pocket, a relatively tall maxilla, a relatively gracile jugal, a more strongly angled posterior margin of the anterior process of the jugal, wide lateral exposure of the quadratojugal, and a short symphyseal process of the dentary. The cladistic analyses consistently recover the Alaskan saurolophine as the sister taxon to Edmontosaurus annectens + Edmontosaurus regalis.
    [Show full text]