Prediction of Reservoir Properties from Processes and Architecture in Deep-Water Clastic Systems

Total Page:16

File Type:pdf, Size:1020Kb

Prediction of Reservoir Properties from Processes and Architecture in Deep-Water Clastic Systems Prediction of reservoir properties from processes and architecture in deep-water clastic systems A thesis submitted to The University of Manchester for the degree of Doctor of Philosophy in the Faculty of Science and Engineering 2019 Daniel Bell School of Natural Sciences Department of Earth and Environmental Sciences TABLE OF CONTENTS TABLE OF CONTENTS ....................................................................................................... 2 LIST OF FIGURES ................................................................................................................. 8 LIST OF TABLES ................................................................................................................. 13 ABSTRACT............................................................................................................................. 14 DECLARATION ................................................................................................................... 15 COPYRIGHT STATEMENT .............................................................................................. 18 ACKNOWLEDGEMENTS ................................................................................................. 19 CHAPTER 1: .......................................................................................................... RATIONALE 21 1.1 CHAPTER 3: HOW DOES DEPOSITIONAL RESERVOIR QUALITY VARY SPATIALLY IN SUBMARINE LOBES AND CHANNEL-FILLS? ............................................................................... 22 1.2 CHAPTER 4: HOW DO BED-SCALE BARRIERS AFFECT SANDSTONE CONNECTIVITY? ... 22 1.3 CHAPTER 5: WHICH HETEROGENEITIES MATTER TO FLOW IN SUBMARINE LOBES, AND HOW ARE THEY DISTRIBUTED? .................................................................................................. 24 1.4 CHAPTER 6: HOW ARE FACIES AND ARCHITECTURE ORGANISED IN THREE DIMENSIONS IN SUBMARINE CHANNEL-FILLS, AND HOW MIGHT THIS AFFECT RESERVOIR PREDICTION? ................................................................................................................................ 25 1.5 CHAPTER 7: DO CONTEMPORANEOUS LOBE DEPOSITS IN A BASIN EXHIBIT THE SAME ARCHITECTURES AND STACKING PATTERNS? .......................................................................... 26 CHAPTER 2: ............... DEEP-WATER DEPOSITIONAL SYSTEMS: PROCESSES, PRODUCTS, AND IMPLICATIONS ..................................................................... 28 2.1 INTRODUCTION ..................................................................................................................... 28 2.2 FLOW PROCESSES .................................................................................................................. 29 Turbulent flows ............................................................................................................................ 29 Debris flows ................................................................................................................................. 32 Transitional flows ........................................................................................................................ 33 2.3 PROCESS CONTROLS ON RESERVOIR QUALITY .................................................................. 35 Introduction ................................................................................................................................. 35 High-density turbidites (HDTs) .................................................................................................. 37 Low-density turbidites (LDTs) .................................................................................................... 38 Hybrid beds ................................................................................................................................. 38 Mudstones ................................................................................................................................... 39 Detrital clays: Hero, and villain? ................................................................................................. 40 2 2.4 COMPONENTS OF DEEP-WATER DEPOSITIONAL SYSTEMS .............................................. 43 Submarine channels ..................................................................................................................... 43 Channel-lobe transition zones ....................................................................................................... 49 Submarine lobes ........................................................................................................................... 50 2.5 BED-SCALE CONTROLS ON RESERVOIR QUALITY DISTRIBUTION ................................... 56 Introduction ................................................................................................................................. 56 Modelling architectural elements ................................................................................................... 57 Bed-scale barriers ......................................................................................................................... 58 CHAPTER 3: ............ SPATIAL VARIABILITY IN DEPOSITIONAL RESERVOIR QUALITY OF DEEP-WATER CHANNEL-FILL AND LOBE DEPOSITS ........ 61 3.1 ABSTRACT ............................................................................................................................... 61 3.2 INTRODUCTION ..................................................................................................................... 62 3.3 GEOLOGICAL SETTING ......................................................................................................... 64 3.4 METHODS ............................................................................................................................... 65 3.5 FACIES ..................................................................................................................................... 67 3.6 ARCHITECTURAL ELEMENT INTERPRETATIONS ............................................................... 73 Figure 3.5: Architectural panels of Lobe 1 of the Upper Broto system ........................................... 74 Gerbe architectural element ........................................................................................................... 75 Broto architectural element ........................................................................................................... 75 3.7 RESULTS .................................................................................................................................. 76 Composition ................................................................................................................................ 76 Gerbe channel-fill element ............................................................................................................. 83 Lobe 1 ........................................................................................................................................ 85 3.8 DISCUSSION ............................................................................................................................ 89 Spatial variation in depositional reservoir quality .......................................................................... 89 Implications of detrital matrix distribution ................................................................................... 95 3.9 CONCLUSIONS ........................................................................................................................ 96 CHAPTER 4: ............. THE EFFECT OF BED-SCALE HETEROGENEITIES ON VERTICAL PERMEABILITY IN CLASTIC SANDSTONES .............................. 98 4.1 ABSTRACT ............................................................................................................................... 98 4.2 INTRODUCTION ..................................................................................................................... 98 4.3 METHODS ............................................................................................................................. 100 4.4 RESULTS ................................................................................................................................ 101 Siltstone-drape test ..................................................................................................................... 101 3 Mudstone-clast test ..................................................................................................................... 104 4.5 DISCUSSION .......................................................................................................................... 105 Effect of siltstone barriers on bed-scale connectivity....................................................................... 105 Effect of mudstone-clasts on bed-scale connectivity ........................................................................ 106 Implications for modelling ........................................................................................................... 108 4.6 CONCLUSIONS ...................................................................................................................... 110 CHAPTER 5: .. BED-SCALE MODELLING OF DEEP-WATER LOBES: WHICH HETEROGENEITIES MATTER TO FLOW? ..................................................... 111 5.1 ABSTRACT ............................................................................................................................
Recommended publications
  • Download Full Article in PDF Format
    A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans Robert W. BOESSENECKER Department of Geology, University of Otago, 360 Leith Walk, P.O. Box 56, Dunedin, 9054 (New Zealand) and Department of Earth Sciences, Montana State University 200 Traphagen Hall, Bozeman, MT, 59715 (USA) and University of California Museum of Paleontology 1101 Valley Life Sciences Building, Berkeley, CA, 94720 (USA) [email protected] Boessenecker R. W. 2013. — A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans. Geodiversitas 35 (4): 815-940. http://dx.doi.org/g2013n4a5 ABSTRACT e newly discovered Upper Miocene to Upper Pliocene San Gregorio assem- blage of the Purisima Formation in Central California has yielded a diverse collection of 34 marine vertebrate taxa, including eight sharks, two bony fish, three marine birds (described in a previous study), and 21 marine mammals. Pinnipeds include the walrus Dusignathus sp., cf. D. seftoni, the fur seal Cal- lorhinus sp., cf. C. gilmorei, and indeterminate otariid bones. Baleen whales include dwarf mysticetes (Herpetocetus bramblei Whitmore & Barnes, 2008, Herpetocetus sp.), two right whales (cf. Eubalaena sp. 1, cf. Eubalaena sp. 2), at least three balaenopterids (“Balaenoptera” cortesi “var.” portisi Sacco, 1890, cf. Balaenoptera, Balaenopteridae gen. et sp. indet.) and a new species of rorqual (Balaenoptera bertae n. sp.) that exhibits a number of derived features that place it within the genus Balaenoptera. is new species of Balaenoptera is relatively small (estimated 61 cm bizygomatic width) and exhibits a comparatively nar- row vertex, an obliquely (but precipitously) sloping frontal adjacent to vertex, anteriorly directed and short zygomatic processes, and squamosal creases.
    [Show full text]
  • APPLICATIONS of QUANTITATIVE METHODS and CHAOS THEORY in ICHNOLOGY for ANALYSIS of INVERTEBRATE BEHAVIOR and EVOLUTION by James
    APPLICATIONS OF QUANTITATIVE METHODS AND CHAOS THEORY IN ICHNOLOGY FOR ANALYSIS OF INVERTEBRATE BEHAVIOR AND EVOLUTION by James Richard Woodson Lehane A dissertation submitted to the faculty of The University of Utah in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geology Department of Geology and Geophysics The University of Utah August 2014 Copyright © James Richard Woodson Lehane 2014 All Rights Reserved The University of Utah Graduate School STATEMENT OF DISSERTATION APPROVAL The dissertation of James Richard Woodson Lehane has been approved by the following supervisory committee members: Allan A. Ekdale , Chair May 5th, 2014 Date Approved Randall B. Irmis , Member June 6th, 2014 Date Approved Marjorie A. Chan , Member May 5th, 2014 Date Approved Elena A. Cherkaev , Member June 12th, 2014 Date Approved Leif Tapanila , Member June 6th, 2014 Date Approved and by John M. Bartley , Chair/Dean of the Department/College/School of Geology and Geophysics and by David B. Kieda, Dean of The Graduate School. ABSTRACT Trace fossils are the result of animal behaviors, such as burrowing and feeding, recorded in the rock record. Previous research has been mainly on the systematic description of trace fossils and their paleoenvironmental implications, not how animal behaviors have evolved. This study analyzes behavioral evolution using the quantification of a group of trace fossils, termed graphoglyptids. Graphoglyptids are deep marine trace fossils, typically found preserved as casts on the bottom of turbidite beds. The analytical techniques performed on the graphoglyptids include calculating fractal dimension, branching angles, and tortuosity, among other analyses, for each individual trace fossil and were performed on over 400 trace fossils, ranging from the Cambrian to the modem.
    [Show full text]
  • Evolution of White and Megatooth Sharks, and Evidence for Early Predation on Seals, Sirenians, and Whales
    Vol.5, No.11, 1203-1218 (2013) Natural Science http://dx.doi.org/10.4236/ns.2013.511148 Evolution of white and megatooth sharks, and evidence for early predation on seals, sirenians, and whales Cajus G. Diedrich Paleologic, Petra Bezruce 96, Zdice, Czech Republic; [email protected], www.paleologic.eu Received 6 April 2013; revised 6 May 2013; accepted 13 May 2013 Copyright © 2013 Cajus G. Diedrich. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. ABSTRACT ments were generally first attributed to “white shark Carcharodon carcharias (Linné, 1758) ancestors”. Con- The early white shark Carcharodon Smith, 1838 troversy has subsequently arisen whether they should be with the fossil Carcharodon auriculatus (Blain- ascribed to the megatooth shark (“Carcharocles”—he- ville, 1818) and the extinct megatooth shark Oto- rein Otodus), or to the white shark (Carcharodon) line- dus Agassiz, 1843 with species Otodus sokolovi age [1]. This controversy is partly a result of non-sys- (Jaeckel, 1895) were both present in the Euro- tematic excavation of single serrated similar looking pean proto North Sea Basin about 47.8 - 41.3 m.y. teeth from many localities around the world, and from ago (Lutetian, early Middle Eocene), as well as in horizons of different ages. DNA studies have at least the Tethys realm around the Afican-Eurasian resolved the general position of the extant form of Car- shallow marine habitats. Both top predators deve- charodon carcharias, placing it between the Isurus and loped to be polyphyletic, with possible two dif- Lamna genera [2,3], without taking into account a revi- ferent lamnid shark ancestors within the Early sion and including of extinct fossil species such as Oto- Paleocene to Early Eocene timespan with Car- dus.
    [Show full text]
  • A Review of the Fossil Seabirds from the Tertiary of the North Pacific
    Paleobiology,18(4), 1992, pp. 401-424 A review of the fossil seabirds fromthe Tertiaryof the North Pacific: plate tectonics,paleoceanography, and faunal change Kenneth I. Warheit Abstract.-Ecologists attempt to explain species diversitywithin Recent seabird communities in termsof Recent oceanographic and ecological phenomena. However, many of the principal ocean- ographic processes that are thoughtto structureRecent seabird systemsare functionsof geological processes operating at many temporal and spatial scales. For example, major oceanic currents,such as the North Pacific Gyre, are functionsof the relative positions of continentsand Antarcticgla- ciation,whereas regional air masses,submarine topography, and coastline shape affectlocal processes such as upwelling. I hypothesize that the long-termdevelopment of these abiotic processes has influencedthe relative diversityand communitycomposition of North Pacific seabirds. To explore this hypothesis,I divided the historyof North Pacific seabirds into seven intervalsof time. Using published descriptions,I summarized the tectonicand oceanographic events that occurred during each of these time intervals,and related changes in species diversityto changes in the physical environment.Over the past 95 years,at least 94 species of fossil seabirds have been described from marine deposits of the North Pacific. Most of these species are from Middle Miocene through Pliocene (16.0-1.6 Ma) sediments of southern California, although species from Eocene to Early Miocene (52.0-22.0 Ma) deposits are fromJapan,
    [Show full text]
  • From the Late Miocene-Early Pliocene (Hemphillian) of California
    Bull. Fla. Mus. Nat. Hist. (2005) 45(4): 379-411 379 NEW SKELETAL MATERIAL OF THALASSOLEON (OTARIIDAE: PINNIPEDIA) FROM THE LATE MIOCENE-EARLY PLIOCENE (HEMPHILLIAN) OF CALIFORNIA Thomas A. Deméré1 and Annalisa Berta2 New crania, dentitions, and postcrania of the fossil otariid Thalassoleon mexicanus are described from the latest Miocene–early Pliocene Capistrano Formation of southern California. Previous morphological evidence for age variation and sexual dimorphism in this taxon is confirmed. Analysis of the dentition and postcrania of Thalassoleon mexicanus provides evidence of adaptations for pierce feeding, ambulatory terrestrial locomotion, and forelimb swimming in this basal otariid pinniped. Cladistic analysis supports recognition of Thalassoleon as monophyletic and distinct from other basal otariids (i.e., Pithanotaria, Hydrarctos, and Callorhinus). Re-evaluation of the status of Thalassoleon supports recognition of two species, Thalassoleon mexicanus and Thalassoleon macnallyae, distributed in the eastern North Pacific. Recognition of a third species, Thalassoleon inouei from the western North Pacific, is questioned. Key Words: Otariidae; pinniped; systematics; anatomy; Miocene; California INTRODUCTION perate, with a very limited number of recovered speci- Otariid pinnipeds are a conspicuous element of the ex- mens available for study. The earliest otariid, tant marine mammal assemblage of the world’s oceans. Pithanotaria starri Kellogg 1925, is known from the Members of this group inhabit the North and South Pa- early late Miocene (Tortonian Stage equivalent) and is cific Ocean, as well as portions of the southern Indian based on a few poorly preserved fossils from Califor- and Atlantic oceans and nearly the entire Southern nia. The holotype is an impression in diatomite of a Ocean.
    [Show full text]
  • Università Di Pisa
    UNIVERSITÀ DI PISA Dottorato di ricerca in scienze della terra XIX Ciclo DISSERTAZIONE FINALE ANALISI SISTEMATICA, PALEOECOLOGICA E PALEOBIOGEOGRAFICA DELLA SELACIOFAUNA PLIO-PLEISTOCENICA DEL MEDITERRANEO Candidato Presidente della Scuola di Dottorato Stefano MARSILI Prof. Paolo Roberto FEDERICI Tutore Prof. Walter LANDINI Dipartimento di scienze della terra 2006 Indice INDICE ABSTRACT CAPITOLO 1 – INTRODUZIONE 1.1. Premessa. 1 1.2. Il Mediterraneo e l’attuale diversità del popolamento a squali. 4 CAPITOLO 2 – MATERIALI E METODI 7 CAPITOLO 3 – INQUADRAMENTO GEOLGICO E STRATIGRAFICO 3.1. Premessa. 15 3.2. Inquadramento geologico e stratigrafico delle sezioni campionate. 16 3.2.1. Le sezioni plioceniche della Romagna. 16 3.2.1.1. Sezione Rio Merli. 17 3.2.1.2. Sezione Rio dei Ronchi. 17 3.2.1.3. Sezione Rio Co di Sasso. 18 3.2.1.4. Sezione Rio Cugno. 19 3.2.2. Le sezioni pleistoceniche dell’Italia Meridionale. 19 3.2.2.1. La sezione di Fiumefreddo. 20 3.2.2.2. La sezione di Grammichele. 22 3.2.2.3. La sezione di Vallone Catrica. 23 3.2.2.4. La sezione di Archi. 23 3.3. Inquadramento geologico e stratigrafico dei bacini centrali del Tora-Fine, di Volterra e di Siena: premessa. 24 3.3.1. Bacino del Tora-Fine. 26 3.3.2. Bacino di Siena-Radicofani. 27 3.3.3. Bacino di Volterra. 29 3.4. Inquadramento geologico e stratigrafico delle principali località storiche. 30 3.4.1. Emilia Romagna. 30 3.4.2. Piemonte. 32 3.4.3. Liguria. 32 3.4.4. Basilicata.
    [Show full text]
  • A Paleodepositional Reconstruction of Middle Miocene Cetacean Bonebeds from the Topanga Formation, Northern San Joaquin Hills, Orange County, Ca ______
    A PALEODEPOSITIONAL RECONSTRUCTION OF MIDDLE MIOCENE CETACEAN BONEBEDS FROM THE TOPANGA FORMATION, NORTHERN SAN JOAQUIN HILLS, ORANGE COUNTY, CA _______________________________________ A Thesis Presented to the Faculty of California State University, Fullerton _______________________________________ In Partial Fulfillment of the Requirements for the Degree Master of Science in Geological Sciences _______________________________________ By Alyssa Beach Adam D. Woods, Committee Chair Nicole Bonuso, Member, Department of Geology Jere Lipps, Member,Department of Geology Spring 2016 ABSTRACT Cetacean bonebeds containing multiple articulated individuals are extremely rare, with only a handful of occurrences documented worldwide. In 1997, three bonebeds containing mostly articulated and well preserved cetacean remains were uncovered during grading in sedimentary rocks assigned to the Paularino Member of the Topanga Formation near Bonita Canyon, Newport Beach, California. Multiple bonebeds within a single stratigraphic unit, such as those discovered at Bonita Canyon Planning Area 26, represent a rare class of deep marine fossil accumulations that have not been previously studied in detail. Taphonomic, stratigraphic, and geochemical data was collected from fourteen jacketed specimens removed from Bonita Canyon Planning Area 26 in order to determine the paleoenvironmental conditions that led to the accumulation of the bonebeds and to shed more light on these types of fossil accumulations. Results of this study indicate that the Bonita Canyon bonebeds do not represent a condensed facies, as previously proposed (The Keith Companies, 1998); rather they represent a composite concentration deposited in a continental shelf environment during a period of high sedimentation rates, where episodes of high energy gravity flows alternated with periods of low energy accumulation along a NE-SW trending submarine fan sequence.
    [Show full text]
  • Geology and Paleontology of the Late Miocene Wilson Grove Formation at Bloomfield Quarry, Sonoma County, California
    Geology and Paleontology of the Late Miocene Wilson Grove Formation at Bloomfield Quarry, Sonoma County, California 2 cm 2 cm Scientific Investigations Report 2019–5021 U.S. Department of the Interior U.S. Geological Survey COVER. Photographs of fragments of a walrus (Gomphotaria pugnax Barnes and Raschke, 1991) mandible from the basal Wilson Grove Formation exposed in Bloomfield Quarry, just north of the town of Bloomfield in Sonoma County, California (see plate 8 for more details). The walrus fauna at Bloomfield Quarry is the most diverse assemblage of walrus yet reported worldwide from a single locality. cm, centimeter. (Photographs by Robert Boessenecker, College of Charleston.) Geology and Paleontology of the Late Miocene Wilson Grove Formation at Bloomfield Quarry, Sonoma County, California By Charles L. Powell II, Robert W. Boessenecker, N. Adam Smith, Robert J. Fleck, Sandra J. Carlson, James R. Allen, Douglas J. Long, Andrei M. Sarna-Wojcicki, and Raj B. Guruswami-Naidu Scientific Investigations Report 2019–5021 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DAVID BERNHARDT, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2019 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S.
    [Show full text]
  • 1 This Is a Postprint That Has Been Peer Reviewed and Published in Biology Letters
    1 This is a postprint that has been peer reviewed and published in Biology Letters. The 2 final, published version of this article is available online. Please check the final 3 publication record for the latest revisions to this article. 4 5 Boessenecker, R.W., and M. Churchill, and J.H. Geisler. 2015. The oldest known fur 6 seal. Biology Letters 11:2:20140835 doi: 10.1098/rsbl.2014.0835 1 7 The oldest known fur seal 8 9 Robert W. Boessenecker 1,2 10 Morgan Churchill 3,4 11 1Department of Geology, University of Otago, Dunedin, New Zealand 9010 12 2Museum of Paleontology, University of California, Berkeley, California, U.S.A. 13 94720 14 3Department of Geology and Geophysics, University of Wyoming, Laramie, 15 Wyoming, U.S.A. 16 4Program in Ecology, University of Wyoming, Laramie, Wyoming, U.S.A. 17 18 Abstract 19 The poorly known fossil record of fur seals and sea lions (Otariidae) does not reflect 20 their current diversity and widespread abundance. This limited fossil record contrasts 21 with the more complete fossil records of other pinnipeds such as walruses 22 (Odobenidae). The oldest known otariids appear 5-6 Ma after the earliest odobenids, 23 and the remarkably derived craniodental morphology of otariids offers few clues to 24 their early evolutionary history and phylogenetic affinities among pinnipeds. We 25 report a new otariid, Eotaria crypta , from the early middle Miocene “Topanga” 26 Formation (15-17.5 Ma) of southern California, represented by a partial mandible 27 with well-preserved dentition. Eotaria crypta is geochronologically intermediate 28 between “enaliarctine” stem pinnipedimorphs (16.6-27 Ma) and previously described 29 otariid fossils (7.3-12.5 Ma), as well as morphologically intermediate by retaining an 30 M2 and a reduced M 1 metaconid cusp and lacking P 2-4 metaconid cusps.
    [Show full text]
  • Papers in Press
    Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2017PR025 Fossil herpetocetine baleen whales (Cetacea, Mysticeti, Cetotheriidae) from the lower Pliocene Horokaoshirarika Formation at Numata, Hokkaido, northern Japan YOSHIHIRO TANAKA1, 2, 3, HITOSHI FURUSAWA4 AND LAWRENCE G. AcceptedBARNES5 1 Osaka Museum of Natural History, Nagai Park 1-23, Higashi-Sumiyoshi-ku, Osaka, 546-0034, Japan (e-mail: [email protected]) 2 Numata Fossil Museum, 2-7-49, Minami 1, Numata town, Hokkaido 078-2225 Japan 3Hokkaido University Museum, Kita 10, Nishi 8, Kita-ku, Sapporo, Hokkaido 060- 0810 Japan manuscript 4Sapporo Museum Activity Center, 5-15-1-6, Hiragishi, Toyohira-ku, Sapporo, Hokkaido 060-0001, Japan. 5Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, U.S.A. Abstract. Two mandibles of fossil mysticetes from the early Pliocene, upper part of the Horokaoshirarika Formation at Numata Town, Hokkaido, Japan, belong to the archaic, extinct cetotheriid baleen whale, Herpetocetinae, gen. et sp. indet. by having an elongated angular process projecting posteriorly beyond the mandibular condyle. The new materials of the Herpetocetinae represent the northernmost occurrence in the North Pacific.
    [Show full text]
  • Preliminary Digital Geological Map of the 30' X 60' Santa Ana Quadrangle, Southern California, Version 2.0 Compiled by D
    Preliminary Digital Geological Map of the 30' X 60' Santa Ana Quadrangle, southern California, version 2.0 Compiled by D. M. Morton1 Version 2.0 digital preparation by Kelly R. Bovard1 and Rachel M. Alvarez1 - 2004 Version 1.0 digital preparation by Rachel M. Hauser1 and Kelly R. Bovard1 - 1999 1Western Surficial Processes Team, U.S. Geological Survey Department of Earth Sciences, University of California, Riverside CA 92521 Pamphlet to accompany Open-File Report 99-172 Version 2.0 - 2004 SCAMP-Southern California Areal Mapping Project A geologic-mapping project sponsored jointly by the U.S. Geological Survey and the California Geological Survey U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U. S. Government. Table of Contents (Blue text indicates hyperlink) Hyperlink index to geologic units ii Units Qaf—Artificial fill to Qvor—Very old regolith iii Units Pauba Formation to Td—Diabase intrusive rocks iv Units Tvss—Vaqueros, Sespe, Santiago, and Silverado Formations, undifferentiated to Kgh—Hypabyssal tonalite v Units Kgct—Coarse-grained biotite-hornblende tonalite to }ds—Metadunite and serpentinite vi Units }sm—Serpentinized metadunite containing magnesite veins to |ms—Marble and schist, undifferentiated Figure 1. Index map showing locations and features referred to in the text Figure 2. Index map showing sources of mapping and digital preparation Geologic setting Summary of major structural elements Faults Quaternary
    [Show full text]
  • Radison Riverfront Hotel Volume 23, Supplement to Number 3 12 September 2003
    VOL. 23, SUPPLEMENT NUMBER 3 JOURNAL TO PALEONTOLOGY ABSTRACTS SEPTEMBER 2003 VERTEBRATE OF Radison Riverfront Hotel Volume 23, Supplement to Number 3 12 September 2003 UPPER LEVEL Breakout Session Room Breakout Session Room STREET LEVEL Speaker Ready Room ABSTRACTS OF PAPERS SIXTY-THIRD ANNUAL MEETING SOCIETY OF VERTEBRATE PALEONTOLOGY SCIENCE MUSEUM OF MINNESOTA ST. PAUL, MINNESOTA Poster SVP Sessions Registration LOWER LEVEL OCTOBER 15-18, 2003 Exhibits SOCIETY OF VERTEBRATE PALEONTOLOGY Plenary/Breakout Session Room ISSN 0272-4634 JOURNAL OF VERTEBRATE PALEONTOLOGY VOLUME 23, SUPPLEMENT TO NUMBER 3 September, 2003 ABSTRACTS OF PAPERS SIXTY-THIRD ANNUAL MEETING SOCIETY OF VERTEBRATE PALEONTOLOGY SCIENCE MUSEUM OF MINNESOTA ST. PAUL, MINNESOTA OCTOBER 15-18, 2003 HOST COMMITTEE: Kristina Curry Rogers (Chair), Chris Brochu, Bruce Erickson, David Fox, Joe Hartman, Jackie Hoff, Ellen Holt-Werle, Ron Lawrenz, Ali Lozoff, Jessica Madole, Rebecca Newberry, Andy Redline, Ray Rogers CONVENORS OF SYMPOSIA: Jason Anderson, Hans-Dieter Sues, Marilyn Fox, Judd Case, Jaelyn Eberle, Mark Goodwin, Sandy Carlson PROGRAM COMMITTEE: Donald Prothero (Chair and Editor), Greg Buckley, Kristina Curry Rogers, David Froehlich, Mike Gottfried, and Eric Dewar PROGRAM AT A GLANCE WEDNESDAY MORNING, OCTOBER 15, 2003 SYMPOSIA EVOLUTIONARY TRANSITIONS AMONG VERTEBRATES A Symposium in Honor of Robert Lynn Carroll MINNESOTA BALLROOM CONVENORS: JASON S. ANDERSON AND HANS-DIETER SUES 8:00 Welcome 8:05 Wilson, M.V.H., and Hanke, G.: HOMOLOGIES OF PAIRED FINS AND TEETH ACROSS THE AGNATHAN- GNATHOSTOME TRANSITION 8:25 Larsson, H.: EVOLUTIONARY INNOVATION OF THE AUTOPODIUM: TESTING DEVELOPMENTAL MECHA- NISMS OF THE FIN-LIMB TRANSITION 8:45 Clack, J., Blom, H., and Ahlberg, P.E.: NEW INSIGHTS INTO THE POSTCRANIAL SKELETON OF ICHTHYOSTEGA 8:55 Anderson, J.
    [Show full text]