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Fractured Shale Gas Potential in New York
FRACTURED SHALE GAS POTENTIAL IN NEW YORK David G. HILL and Tracy E. LOMBARDI TICORA Geosciences, Inc., Arvada, Colorado, USA John P. MARTIN New York State Energy Research and Development Authority, Albany, New York, USA ABSTRACT In 1821, a shallow well drilled in the Devonian age shale ushered in a new era for the United States when natural gas was produced, transported and sold to local establishments in the town of Fredonia, New York. Following this discovery, hundreds of shallow shale wells were drilled along the Lake Erie shoreline and eventually several shale gas fields were established southeastward from the lake in the late 1800’s. Since the mid 1900’s, approximately 100 wells have been drilled in New York to test the fractured shale potential of the Devonian and Silurian age shales. With so few wells drilled over the past century, the true potential of fractured shale reservoirs has not been thoroughly assessed, and there may be a substantial resource. While the resource for shale gas in New York is large, ranging from 163-313 trillion cubic feet (Tcf) and the history of production dates back over 180 years, it has not been a major contributor to natural gas production in New York. A review of the history and research conducted on the shales shows that the resource in New York is poorly understood and has not been adequately tested. Other shales such as the Silurian and Ordovician Utica Shale may also hold promise as new commercial shale gas reservoirs. Experience developing shale gas plays in the past 20 years has demonstrated that every shale play is unique. -
Chapter 4 GEOLOGY
Chapter 4 GEOLOGY CHAPTER 4 GEOLOGY ...................................................................................................................................... 4‐1 4.1 INTRODUCTION ................................................................................................................................................ 4‐2 4.2 BLACK SHALES ................................................................................................................................................. 4‐3 4.3 UTICA SHALE ................................................................................................................................................... 4‐6 4.3.2 Thermal Maturity and Fairways ...................................................................................................... 4‐14 4.3.3 Potential for Gas Production ............................................................................................................ 4‐14 4.4 MARCELLUS FORMATION ................................................................................................................................. 4‐15 4.4.1 Total Organic Carbon ....................................................................................................................... 4‐17 4.4.2 Thermal Maturity and Fairways ...................................................................................................... 4‐17 4.4.3 Potential for Gas Production ........................................................................................................... -
Marcellus/Utica Shale
Marcellus/Utica Shale Presented by Jeff Wlahofsky Jay Meglich George Adams Discussion Topics • Common Industry Terms and Definitions • Video of Horizontal Drilling Process • Overview of Geology Differences Between Marcellus and Utica Shale • Background Regarding Marcellus Activity in PA • Current State of the Shale Gas Industry • Planning Opportunities for Income Deferral or Capital Gain Tax Treatment 2 Industry Terms and Definitions • Abandoned Well – A well no longer in use; a dry hole that, in most states, must be properly plugged • Bonus – Usually, the bonus is the money paid by the lessee for the execution of an oil and gas lease by the landowner. Another form is called an oil or royalty bonus. This may be in the form of an overriding royalty reserved to the landowner in addition to the usual one‐eighth or 12.5% royalty. • Christmas Tree – An assembly of valves mounted on the casing head through which a well is produced. The Christmas tree also contains valves for testing the well and for shutting it in if necessary. The “Christmas Tree” includes blow‐out preventer valves. 3 Industry Terms and Definitions (cont’d) • Completion – To finish a well so that it is ready to produce oil or gas. After reaching total depth (T.D.), casing is run and cemented; casing is perforated opposite the producing zone, tubing is run, and control and flow valves are installed at the wellhead. Well completions vary according to the kind of well, depth, and the formation from which the well is to produce 4 Industry Terms and Definitions (cont’d) • Delay Rentals – These are amounts paid to the lessor for the privilege of deferring the commencement of a well on the lease. -
Regional Drilling Activity and Production
(Sections) 2.0 REGIONAL DRILLING ACTIVITY AND PRODUCTION Naming Convention: 2-digit state code/3-digit county code/5-character identifier Example: 37027_OC12 (Pennsylvania, Butler County, Outcrop Sample 12) For all other wells, the file naming convention leads with the API number. The leading API number/Project ID is then followed by the code for the file category or categories under which the data are classified. For a standard file containing information on a single well or sample, the following naming convention is used: Naming Convention: API number or Project ID_File Type Code(s)_Optional Description Example: 34003636910000_SRA_TOC_BP_Chemical_Plant_Well_4.xls As of July 9, 2014, there were 5696 files organized under this naming convention. In addition to these files, there were an additional 35 files that contain data for multiple wells. These files, which are often final results of data analyzed by service companies or consultants, can contain results for many different wells or samples. For these document types, the following naming convention is used: Naming Convention: 2-digit state code/000/MLTPL_File Type Codes_Optional Description Example: 34000MLTPL_SRA_TOC_XRD_OvertonEnergy.pdf Individual wells contained in the file are stored in a second table, which is linked by the file name, allowing the user to search by any of the individual API numbers/Project IDs contained within the multiple well file. As the data collected, generated, and interpreted by the research team became finalized, new file categories were created and populated with project results. In addition, a general file with all header data was created, allowing users to import project wells into various subsurface mapping programs. -
Where in New York Are the Marcellus and Utica Shales??
Where in New York are the Marcellus and Utica Shales?? How do they get to the gas resource and how do they get the gas out of the ground? What are the concerns about this entire process and what can/should we do about it? Schlumberger, Inc Depth and extent of the Marcellus Shale Marcellus, NY type section Source – dSGEIS, 2009 East-West Geologic Section of the Marcellus Shale Across Southern New York Thickening of Oatka Creek Thinning of Oatka Creek Lash and Engelder, 2009 and Union Springs members North-South Geologic Section Across New York State Source – dSGEIS, 2009 Source – dSGEIS, 2009 Medina SS Central/ Western NY Marcellus Stratigraphy Oatka Creek Cherry Valley Union Springs Oil and Gas wells are not new in Pennsylvania and New York……. …and there are different regulations in and within each state. Multiple steel casings with high-strength cement to isolate well from surrounding aquifers and bedrock units. What is different about Marcellus/Utica shale gas development? East-northeast trending J1 fractures more closely spaced and cross-cut by less well- developed, northwest-trending J2 fractures Dual porosity gas reservoir where fractures drain rapidly and matrix drain slowly Drill horizontal wells to the north-northwest, or south- southeast that cross and Free gas and adsorbed drain densely developed J1 gas in matrix fractures Connect matrix porosity to the wellbore by intersecting multiple J1 fractures Marcellus Shale Gas Development Horizontal Drilling in Black Shale with High-Volume Hydraulic Fracturing 3,500 ft 3,500 4,000 ft Meyer (2009) Meyer (2009) Microseismic Monitoring of Hydraulic Fracturing “Typical” Drillpad Design Water-source pond Drill cuttings pond Drilling Phase – drillrig, pumps, supplies, frack tanks (a month or two) Hydro-fracking Phase – (a week or two) Injection pumps, supplies, and many frack tanks for fresh and flowback waters Where do you get the water for fracking? Inter- basin Trans- fer Each source has its own set of concerns……. -
Stratigraphic Distribution and Suggested Evolution of Dendroid Graptolites from the Silurian of Eastern Australia
University of Wollongong Research Online Faculty of Science - Papers (Archive) Faculty of Science, Medicine and Health 1-1-2010 Stratigraphic distribution and suggested evolution of dendroid graptolites from the Silurian of eastern Australia Barrie Rickards University of Cambridge Anthony Wright University of Wollongong, [email protected] Follow this and additional works at: https://ro.uow.edu.au/scipapers Part of the Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Social and Behavioral Sciences Commons Recommended Citation Rickards, Barrie and Wright, Anthony: Stratigraphic distribution and suggested evolution of dendroid graptolites from the Silurian of eastern Australia 2010, 177-190. https://ro.uow.edu.au/scipapers/634 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Stratigraphic distribution and suggested evolution of dendroid graptolites from the Silurian of eastern Australia Abstract Five evolutionary lineages are proposed for Silurian species of the benthic dendroid graptolite genus Dictyonema, based largely on the exceptional eastern Australian records of the genus, comprising at least 25 species. These are: A, the delicatulum lineage with bifurcating ventral autothecal apertural spines; B, the paululum lineage with single ventral apertural spines or processes; C, the elegans lineage with isolated thecal apertures ± processes; D, the sherrardae lineage with dorsal apertural processes; and E, the venustum lineage with simple autothecal apertures. Brief comments are also made on other dendroid genera occurring in Australian strata, namely: Acanthograptus, Koremagraptus, Callograptus, Dendrograptus, Stelechocladia, Thallograptus and Palaeodictyota. Other non-graptoloid benthic hemichordates also listed are the tuboids Galaeograptus, Reticulograptus and Cyclograptus and the rhabdopleuran ?Rhabdopleura. -
XRF Workshop Book
Workshop Materials (1 of 2) Table of Contents Workshop Materials (book 1 of 2) Page Agenda 1 Welcome Presentation (Steve Kaczmarek) 3 Lectures Introduction to the Chemistry of Rocks and Minerals (Peter Voice) 7 Geology of Michigan (Bill Harrison) 22 XRF Theory (Steve Kaczmarek) 44 Student Research Posters Silurian A-1 Carbonate (Matt Hemenway) 56 Silurian Burnt Bluff Group (Mohamed Al Musawi) 58 Classroom Activities Powder Problem 60 Fossil Free For All 69 Bridge to Nowhere 76 Get to Know Your Pet Rock 90 Forensic XRF 92 Alien Agua 96 Appendices (book 2 of 2) Appendix A: MGRRE Factsheet 105 Appendix B: Michigan Natural Resources Statistics 107 Appendix C: CoreKids Outreach Program 126 Appendix D: Graphing & Statistical Analysis Activity 138 Appendix E: K-12 Science Performance Expectations 144 Appendix F: Workshop Evaluation Form 179 Workshop Facilitators Bridging the Gap between Geology & Chemistry Sponsored by the Western Michigan University, the Michigan Geological Repository for Research and Education, and the U.S. National Science Foundation This workshop is for educators interested in learning more about the chemistry of geologic materials. Wednesday, August 9, 2017 (8 am - 5 pm) Tentative Agenda 8:00-8:20: Welcome (Steve Kaczmarek) Agenda, Safety, & Introductions 8:20-8:50: Introduction to Geological Materials (Peter Voice) An introduction to rocks, minerals, and their elemental chemistry 8:50-9:00: Questions/Discussion 9:00-9:30: Introduction to MI Basin Geology (Bill Harrison) An introduction to the common rock types and economic -
Catalog of Paleontological Type Specimens in the Geological Museum, University of Minnesota
MINNESOTA GEOLOGICAL SURVEY INFORMA TION CIRCULAR 33 CATALOG OF PALEONTOLOGICAL TYPE SPECIMENS IN THE GEOLOGICAL MUSEUM, UNIVERSITY OF MINNESOTA UNIVERSITY OF MINNESOTA Minnesota Geological Survey Priscilla C. Grew, Director Information Circular 33 CATALOG OF PALEONTOLOGICAL TYPE SPECIMENS IN THE GEOLOGICAL MUSEUM, UNIVERSITY OF MINNESOTA By William F. Rice University of Minnesota St. Paul, 1990 ISSN 0544-3105 The University of Minnesota is committed to the policy that all persons shall ha ve equal access to its programs, facilities, and employment without regard to race, religion, color, sex, national origin, handicap, age, veteran status, or sexual orientation. CONTENTS Page FOREWORD, by Robert E. Sloan ...................................................... v INTRODUCTION ............................................................................. 1 ORGANIZATION OF THE CATALOG ........................................... 1 PRIMARY PALEONTOLOGICAL TYPES .................................... 3 PHYLUM ANNELIDA ...................................................................... 4 PHYLUM ARTHROPODA Class Merostomata ..................................................................... 15 Subclass Ostracoda ..................................................................... 16 Class Trilobita ........................................................................... 35 PHYLUM BRACHiOPODA ........................................................... 39 PHYLUM BRYOZOA .................................................................... 45 -
MODE of LIFE of GRAPTOLITES Much of the Substance of This Paper
ACT A PALAEON.TOLOGICA POLONICA Vol. 23 1978 No.4 / .. NANCY HARTSHORNE KIRK MODE OF LIFE OF GRAPTOLITES Abstract. - The probable mode of life of the graptol,ites (crustoids, dendroids and graptoloids) is reconstructed from a, logical interpretation of their rhabdosomal structures. The readaptation of sessile colonial organisms to meet the requirements of a freely-moving existence in the plankton is regarded as the controlling factor in the evolution of the graptoloids. It is suggested that the gradual reduction in the size of the colony in the dicho graptids, biserial and uniserial graptoloids may have been a consequence of the undesirability of coloniality in the new environment, and that the graptoloids might have attained individuality, disappea):'ing into the plankton at t e time of their sup- posed extinction. .. Much of the substance of this paper was read to the Symposium on Coloniality at Durham (Systematics Association) in 1976 and should be published shortly. This version contains some new ideas, however, and also many digressions to discuss points of outstanding disagreement. Since the broad outline of my theme will be familiar to graptolitologists, as was not the case for the Systemahcs Association, I trust that the digres sions will be of use and interest in themselves, and, placed in parentheses, will not obscure too much my main argument. !tis generally believed that crustoids were encrusting, and the dend roids attached benthonic colonies. Their coloniality may have been an adaptation to the benthonic.habit, which could have arisen by failure of asexually budded zooids to separate from the' parent. By forming en crusting or tree-like' colonies small, zooids of comparatively simple orga nisation would have, been able to establish !hemselves upon the crowded sea floor and avoid being overtropped by competitors. -
Lab 8: Graptolites and Trace Fossils
Geos 223 Introductory Paleontology Spring 2006 Lab 8: Graptolites and Trace Fossils Name: Section: AIMS: This lab will introduce you to graptolites (Part A), and to a branch of paleontology known as ichnology (the study of trace fossils; Part B). By the end of Part A this lab you should be familiar with the basic anatomy of graptolites, and have an appreciation for how graptolites are used in the biostratigraphic zonation of the Lower Paleozoic. By the end of Part B of this lab you should be familiar with the basic ethological groups of trace fossils, and have an appreciation for how trace fossils can provide important paleoecological and paleoenvironmental information. PART A: GRAPTOLITES. Graptolites (Class Graptolithina) are an extinct group of colonial hemichordate deuterostomes, similar in morphology and life habit to the modern colonial pterobranch hemichordate Rhabdopleura. The graptolite colony consisted of many clonal zooids, each occupying a theca in the communal skeleton (the rhabdosome). The thecae formed in rows along branches of the rhabdosome called stipes. The rhabdosome was made of a non-mineralized, organic, non-chitinous protein called periderm. Graptolite colonies were either erect fan-like structures growing from the seafloor (most dendroid graptolites, ranging from the Middle Cambrian to the Late Carboniferous) or free-floating in the plankton (the commoner graptoloid graptolites, probably descended from dendroid ancestors and ranging from the Early Ordovician to the Early Devonian). Graptoloid graptolites are very important biostratigraphic zone fossils in Lower Paleozoic strata. 1 DENDROID GRAPTOLITES: A1: Dictyonema. Dendroid graptolite colonies formed fan-like structures with thecae-bearing stipes held apart by horizontal struts (dissepiments). -
Late Ludfordian and Early Pridoli Monograptids from the Polish Lowland
LATE LUDFORDIAN AND EARLY PRIDOLI MONOGRAPTIDS FROM THE POLISH LOWLAND ADAM URBANEK Urbanek, A. 1997. Late Ludfordian and early Pfidoli monograptids from the Polish Low land. In: A. Urbanek and L. Teller (eds), Silur ian Graptolite Faunas in the East European Platform: Stratigraphy and Evolution. - Palaeontologia Polonica 56, 87-23 1. Graptolites etched from the Mielnik-I wellcore (EPoland) reveal the main features of the development of monograptid faunas within the late Ludfordian-early Pi'idoli interval. Fifteen species and subspecies are described and Monog raptus (Slovinog raptus) subgen. n. as well as Neocolonograptu s gen. n. are erected. Morphology of many species has been described adequately for the first time and their systematic position corrected. Four grap tolite zones of the late Ludfordian are distinguished. The late Ludfordian fauna, which appears after the kozlowskii Event, is composed mainly of immigrants dominated by hooded monograptids. They reappear as a result of the Lazarus effect. Some of them initiated the lobate-spinose phyletic line terminating with Mon ograptus (Uncinatograptus) spineus, a highly characteristic index species. The lobate and the lobate-spinose types are accompanied by bilobate forms (Pse udomonoclimac is latilobu s). The graptolite sequence indicates that the appeara nce of the early Pfidoli fauna was preceded by a biotic crisis, namely the spineus Event. Therefore this fauna is made up of a few holdovers and some new elements which developed from Pristiograptus dubiu s stem lineage (Neocolonograptus gen. n., Istrograpt us Tsegelnjuk). This early assemblage, com posed of bilobate forms, was later enriched by hooded monograptid s, reappearing after the spineus Event. -
Early Silurian Graptolites from Southeastern Alaska and Their Correlation with Graptolitic Sequences in North America and the Arctic
Early Silurian Graptolites From Southeastern Alaska and Their Correlation With Graptolitic Sequences in North America and the Arctic GEOLOGICAL SURVEY PROFESSIONAL PAPER 653 Early Silurian Graptolites From Southeastern Alaska and Their Correlation With Graptolitic Sequences in North America and the Arctic By MICHAEL CHURKIN, JR., and CLAIRE CARTER GEOLOGICAL SURVEY PROFESSIONAL PAPER 653 Descriptions and illustrations of $9 species of Graptoloidea and correlation of the assemblages with other graptolitic successions in North America, the Soviet Arctic, and Great Britain UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress Catalog-card No. 78-605140 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1 (paper cover) CONTENTS Page Page Abstract-_ _________________________________________ 1 Standard graptolite zones for the Lower Silurian___-_._- 6 Introduction-______________________________________ 1 Lower Silurian graptolites in western North America-___ 6 Acknowledgments. ____ __--_-_________-____-__-______ 1 Systematic descriptions._____________________________ 13 Graptolites of the Descon Formation, southeastern Alaska__ _____________________________________ 2 Class Graptolithina.____________________________ 13 Description of the Descon Formation.________..___ 2 Order Graptoloidea_-___________---___-__-_- 13 Graywacke sandstone and banded