DOCSLIB.ORG

Palaeomagnetic Applications in Hydrocarbon Exploration and Production: Introduction

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Palaeomagnetic Applications in Hydrocarbon Exploration and Production: Introduction Downloaded from http://sp.lyellcollection.org/ by guest on September 30, 2021 Palaeomagnetic Applications in Hydrocarbon Exploration and Production: Introduction PETER TURNER 1 & AMANDA TURNER 2 1School of Earth Sciences, The University of Birmingham, Birmingham B15 2TT, UK 2TERRASCIENCES Ltd, 8 Canfield Place, London NW6 3BT, UK Abrief outline of palaeomagnetism include the classic work of Irving (1964) and the more recent books by McElhinny (1973), Tar- Although the study of magnetism is one of the ling (1983) and Butler (1992). oldest sciences, palaeomagnetism is a relatively Palaeomagnetism and rock magnetism have young geoscience which incorporates aspects of considerable value in hydrocarbon exploration geomagnetism, rock magnetism and geology. Its and production although there have, as yet, application to sedimentary sequences developed been few subsurface palaeomagnetic studies. rapidly in the post-war era as a result of both The main areas in which palaeomagnetic data theoretical and technological advances. The may be useful to the petroleum geologist are: theoretical advances included an ever-increasing palaeomagnetic dating and magnetostratigra- understanding of the Earth's magnetic field and phy; susceptibility logging of cores; magnetic a much more detailed knowledge of the physical fabric studies for palaeocurrent analysis; using properties of those minerals capable of carrying remagnetization to date diagenetic events, in- magnetism (natural remanence) under Earth cluding those associated with hydrocarbon mi- surface conditions. Also, applications to a wide gration; and the identification of magnetic variety of geological problems in many different anomalies associated with hydrocarbon plumes parts of the world led rapidly to a much greater and oil seeps. Basic susceptibility and rem- awareness of the way in which rocks acquired anence measurements are also required for the their magnetization, how it might be altered interpretation of aeromagnetic surveys. during later geological history and how the For the benefit of the non-specialist some of derived palaeomagnetic directions might be the basic concepts in palaeomagnetism will be used to unravel the movement of large crustal dealt with here. These concern the Earth's blocks (apparent polar wandering) and the more magnetic field, magnetic minerals and rem- localized rotation of smaller tectonic blocks. A anence acquisition and the main applications key phase in the development of palaeomag- relevant to hydrocarbon exploration and pro- netism was the recognition that marine magnetic duction. anomalies represented reversals of the Earth's magnetic field. Subsequent systematic sampling and measurement of the ocean basins by the The Earth's magnetic field ODP (ocean drilling project) has resulted in a The Earth's magnetic field roughly corresponds sophisticated geomagnetic polarity time scale to that of a geocentric axial dipole. In this simple (GPTS) from the middle Jurassic to present day. model a magnetic dipole at the centre of the It is beyond the scope of this overview to Earth is aligned parallel to the rotation axis provide more background information but there (Fig. 1). The geographic latitude (h) ranges from are a number of excellent texts which cover all +90 ~ at the north pole and -90 ~ at the south pole aspects of palaeomagnetic theory and appli- and the inclination of the field and geographic cation. For theoretical background there is a latitude are related by: thorough introduction to geomagnetism by tan I = 2 tan h (1) Parkinson (1983); O'Reilly (1984) provides a rigorous and concise treatment of rock and In fact, the Earth's field is more complicated and mineral magnetisms and the techniques of a more accurate model is that of an inclined sampling and measurement are very clearly geocentric dipole with the dipole inclined at an described by Collinson (1983). Textbooks which angle of 11.5 ~ to the rotation axis. This accounts describe the application of palaeomagnetism for about 90% of the field and the other 10% is From TURNER, P. & TURNER, A. (eds), 1995, PalaeomagneticApplications in Hydrocarbon Exploration and Production, Geological Society Special Publication No. 98, 1-5. Downloaded from http://sp.lyellcollection.org/ by guest on September 30, 2021 2 P. TURNER & A. TURNER geomagnetic A B north.pole N north magneticpole ~..~._~raphic pole) magnetic equator I ~~---/ geoorahic ,i_ o,o )-~ o0oa,or- P geomagnetic .1~r~'- best-fi{ling I\ / equator X dipole- I X / I \ ./~_.. south magneticpole [I = -90~ Fig. 1. (A) The geocentric axial dipole model. The magnetic dipole M is at the centre of the Earth and aligned with the rotation axis k is the geographic latitude and re is the radius of the Earth and N the north geographic pole. The magnetic field vector H for one location with inclination is shown. (B) The inclined geocentric dipole model. The diagram shows the difference between magnetic poles and geomagnetic poles and also a comparison between the magnetic and geomagnetic equators. The difference between magnetic poles and geomagnetic pole is due to the non-dipole field which accounts for 10% of the total field. (A and B after Butler 1992). attributed to non-dipole contributions. Short- ations of about 2 x 103 A/m. Titanomagnetites term variations of the non-dipole field (<3000 have the ideal formula Fe3_xTixO4(0< x< 1) years), for example the eastward shift in decli- and crystallize in the spinel structure. They are nation since about AD 1800 in the UK, constitute ferrimagnetic and have saturation magnetiz- the geomagnetic secular variation. ations of about 4.8 x 10 -5 A/m. They are thus The relationship tan I = tan k has important magnetically much stronger than haematite - a implications for palaeomagnetic measurements fact which must be taken into consideration of core material. Because most core material is when assessing the rock magnetic composition unorientated, any palaeomagnetic measure- of sedimentary rocks. They typically form from ments will be unorientated in the horizontal igneous melts and in the sedimentary environ- plane and thus have only arbitrary declinations. ment are usually at least partially oxidized to Inclination, however, can be related directly to their non-stoichiometric equivalents, the titano- geographic latitude. Since the magnetic incli- maghemites, which have the ideal formula nation at the equator is 0 ~ the magnetic polarity Fe(3_x)RTixRI-]3(I_R)O4 where [] are vacancies in from core can only be determined if the sampling cation sites of the structure. site is sufficiently far from the palaeoequator There are also some magnetic iron sulphides (say >10~ such as some pyrrhotites (Fe,_xS where 0<x<0.13 and greigite (Fe3S4). Most other Magnetic minerals and remanence iron-bearing minerals in the sedimentary en- acquisition vironment are paramagnetic or diamagnetic. These include the iron carbonates (paramag- There are only a relatively small number of netic) and pyrite (diamagnetic). Of particular minerals which are capable of carrying natural interest to the petroleum industry are magnetite permanent magnetization and are therefore of spherules (cc. 50 Ixm) which may be the oxi- importance in palaeomagnetic studies. These dation products of framboidal pyrite and magne- include the iron oxides, including haematite tosomes, small magnetite crystals which formed (et-Fe203) the titanomagnetites and the titano- in magnetotactic bacteria. These are especially maghemites (Fig. 2). In general, haematite and significant because of their microbial origin and ferric oxyhydroxides are magnetically weak the possible link to hydrocarbon environments antiferromagnets with saturation magnetiz- and also because they lie in the single domain Downloaded from http://sp.lyellcollection.org/ by guest on September 30, 2021 INTRODUCTION 3 TiO 2 1 ~" Fe 2 TiO 4 ulvospinel , [maghemitization ~ ~Se/.,.. "//t@,.~ . TMI subsolvus Fe 0 r precipitation, ~iC--I~Fe304 r- m~i-i-i-i-i-i-i-i-i-~a~n, "] ~'Fe203 wust~te ~ oxidation of silicates, .~/~/fl Isupergene alterationl haematite alteration of clay minerals | martitization J maghemite serpentinization Fig. 2, The FEO-TiO2-FeO3 ternary diagram of rock magnetism. Points in the triangle correspond to oxide compounds or mixtures of compounds containing FeE+, Fe3+ and Ti4+. The point TM60 represents the idealized titanomagnetite with composition Fe2.4Ti0,604. Some of the paths which may be followed by the magnetic mineral fraction of crustal rocks in the course of geological history are indicated (after O'Reilly 1984). size range (<1 ~m) and are thus palaeomag- relaxation time may be greatly reduced and such netically very stable. grains may contribute to unstable magnetiz- A key concept in palaeomagnetism is the time ation. When the relaxation time is very short dependence of magnetization. All magnetic (several seconds to a few minutes) the magnetiz- particles have a relaxation time (.r) which is ation is said to be viscous. Viscous remanent determined by grain volume, coercivity, satu- magnetization (VRM), because of its short ration magnetization and temperature as fol- relaxation time, will align itself in the ambient lows: magnetic field direction, which may be the geomagnetic field. "r -= 1/C exp (vJsBc/21T) (2) Equation 2 also explains why thermal demag- Where C is a frequency factor of c. 101~s -1, v is netization is of such fundamental importance in the volume of the grain of coercivity, Be, and palaeomagnetism. By progressively increasing spontaneous magnetization, Js, and k is
Load more

Recommended publications
  • Sophisticated Stratigraphy – How We Got Here Andrew D
    Sophisticated Stratigraphy – How we got here Andrew D. Miall University of Toronto Summary Stratigraphy is the key to the understanding of Earth history. “Sophisticated stratigraphy” is the science that is now being practiced. It refers to new tools, the application of advanced analytical techniques, and new forms of interpretation. Refinement of the geological time scale is an essential part of this work. and has been joined by new concepts of cyclostratigraphy and astrochronology. The modern stratigraphic record has been rendered comprehensible by developments in sedimentology and sequence stratigraphy, and has been fleshed out by the addition of much primary data obtained from the Deep-Sea Drilling Project and its successors. This paper summarizes the history of progress that was accelerated by the needs of petroleum exploration, beginning in the early 20th century. The history of modern stratigraphic methods The first stratigrapher was the canal engineer, William Smith, who enunciated the principle of the orderly succession of strata and their contained fossils, and produced the first comprehensive regional geological map, in 1815. It has taken 200 years and a revolution to bring all the necessary modern developments together to create the dynamic science of Fig. 1. sophisticated stratigraphy. Until the 1960s, stratigraphy was largely a descriptive science, concerned primarily with the documentation of the lithologic and biostratigraphic successions of sedimentary basins as a basis for locating and exploiting fossil fuel and mineral deposits. The distinguished petroleum geologist Levorsen (1954) initiated many new ideas. However, over the last fifty years a profound change in approach has taken place, initially under the rubric of Sedimentology, which took sedimentary geologists away from description and classification into a focus on processes (Fig.
    [Show full text]
  • Md Golam Kibria
    CURRICULUM VITAE Md. Golam Kibria Address: Apt#23, 1700 Hillcrest Drive Kansas State University Manhattan, KS 66502 USA E-mail: [email protected] RESEARCH INTEREST: Hydrogeology Contaminant Hydrogeology Geochemistry Stable Isotope Geochemistry Environmental geology Engineering Geology EDUCATION: M.S in Petroleum Geology & Geophysics, University of Dhaka, (1st Class 4th) 2011 Thesis Title: Effect on Hydrogeology due to Longwall Mining activity in Barapukuria Coal Basin, Dinajpur, Bangladesh. B.Sc (Honours ) in Geology,University of Dhaka (1 st Class 6th ) 2009 3. WORK HISTORY: Year: April 2011 to April 2012 Project: Sustainable Arsenic Mitigation Project (SASMIT) Organization: NGO FORUM (employed under NGO FORUM component of SASMIT Project) Position held: Geologist (Full Time) Location: Bangladesh Activities performed: • Collected and reviewed existing data from all relevant sources to make a preliminary assessment and to identify the data gaps. • Assessed union wise safe water access for whole Matlab area based on the tubewell screening information available with NAMIC/BAMWSP database. • Assessed village wise safe water access based on information available from Arsenic contaminated tube-well surveyed under AsMat Project and thereby made a priority list of all the villages to rank the need of Arsenic safe tube-wells. • Completed Vertical Electric Soundings (VES) covering entire Matlab area and delineated a gross subsurface lithologic and stratigraphic sequence to delineate the aquifer systems of the project area. • Selected sites, supervised test borings up to a depth of 800 feet, constructed borelogs from the collected sediment samples, designed test wells and piezometers, supervised installation of 36 Piezometers at different depths and different locations of the project area.
    [Show full text]
  • Ron Broadhead: Petroleum Geologist Extraordinaire
    Ron Broadhead: Petroleum geologist extraordinaire —By Kristin Pearthree hen Ron Broadhead was a child, he lived in a house in Danville, Illinois with hard shale rock flooring. WA fitting precursor of things to come. As a graduate student at the University of Cincinnati, he would study shale rocks containing hydrocarbon resources in northern Ohio. And thirty years later, when horizontal fracturing made possible the extraction of unconventional gas resources from shale rocks, he would again return to the subject as a petroleum geologist at the New Mexico Bureau of Geology and Mineral Resources. In March 2020, Ron retired from the Bureau of Geology and gained emeritus status, all while sporting his signature hat. Ron was born in Racine, Wisconsin in 1955 on the west- ern shore of Lake Michigan. His family moved through a few Midwestern states before settling in Illinois. His parents tried to interest him in many things to see what stuck. They even gave him a paleontology kit one year for Christmas. While in his senior year of high school, he elected to take a semester of earth science and a semester of geography, both courses his councilor assured him were for “the students who could not pass any other kind of science.” But he took them anyway. Through these courses, he developed a keen interest in the earth sciences. His high school had a room with filing cabinets full of literature from potential colleges. Ron found the postcard for New Mexico Tech and mailed it to request more information. He received a glossy brochure in return.
    [Show full text]
  • 3-D Geostatistical Model and Volumetric Estimation of 'Del' Field
    logy & eo G G e f o o p l h a y n s r i c u Oluwadare et al., J Geol Geophys 2017, 6:3 s o J Journal of Geology & Geophysics DOI: 10.4172/2381-8719.1000291 ISSN: 2381-8719 Research Article Open Access 3-D Geostatistical Model and Volumetric Estimation of ‘Del’ Field, Niger Delta Oluwadare OA, Osunrinde OT, Abe SJ* and Ojo BT Department of Applied Geophysics, Federal University of Technology, Nigeria Abstract There is an insatiable thirst for oil and gas consumption and increased production will be made possible only through effective reservoir characterization and modeling. A suite of wire-line logs for four wells from ‘DEL’ oil field together with 3D seismic data were analyzed for reservoir characterization of the field. Two reservoirs were identified using the resistivity log. A synthetic seismogram was generated in order to perform seismic to well tie process as well as picking of horizons throughout the section. Time and depth structural maps were generated. Geostatistical simulation such as the sequential Gaussian stimulation and sequential indicator stimulation were carried out to provide equiprobable representations of the reservoirs, and the distribution of reservoir properties within the geological cells. The modeled reservoir properties resulted in an improved description of reservoir distribution and inter connectivity. The analysis indicated the presence of hydrocarbon in the reservoirs. There is also a fault assisted closure on the structural map which is of interest in exploration. A fluid distribution plot and map of the field were also obtained. The modeled properties gave an average porosity of 24%, average water saturation ranging from 12%-24% and moderate net-gross.
    [Show full text]
  • Simple Seismics for the Petroleum Geologist, the Reservoir Engineer, the Well- Log Analyst, the Processing Technician, and the Man in the Field
    springer.com Earth Sciences : Economic Geology Anstey, N.A. Simple Seismics for the petroleum geologist, the reservoir engineer, the well- log analyst, the processing technician, and the man in the field Springer This little book is different. It is written, primarily, for geologists, reservoir engineers, and log Softcover reprint of the analysts. Why? Because today's seismic method is more than a tool for reconnaissance 1st original 1st ed. 1982, 168 p. exploration, for finding structures; it has become a tool for studying the discovered reservoir-its edition extent, its barriers, its variations of thickness, and its trends of porosity. Today, the geophysicist, the geolog• ist, the engineer, and the log analyst can do great things together. Because the book is not written primarily for geophysi• cists, it can skip much of the "mechanics" of the Printed book seismic method. The reader who reaches the last page (bless him!) will not be able to practise Softcover the seismic method, but he will understand how the seismic method can help to solve his Printed book problems. It may also be of value to those practitioners of the seismic method-in the field or Softcover in the processing centre-who already know the mechanics of the method, but would like to ISBN 978-94-011-7456-5 take a broader view. 1 1 Seismics and Structure Of all the geophysical methods working from the surface, there is only one which is widely accepted for studies of individual petroleum $ 109,99 reservoirs-the seismic reflection method. We would dearly love to have something better, but Available alas ..
    [Show full text]
  • What Can I Do with a Major In
    Geology is the study of the earth’s history as well as the processes that continue to shape the earth today. Geologists view the earth as a place where physical and chemical processes interact within the atmospheric, ocean, and land systems. Understanding these systems allows geologists to protect and improve groundwater and surface water resources; develop wise land-use practices; search for natural resources such as oil, gas, or metals; and evaluate potential risks associated with volcanic eruptions, earthquakes, and landslides. Students at University of Wisconsin–Eau Claire can choose a comprehensive geology major with an emphasis in general geology, hydrogeology and water chemistry, environmental science, or marine geology. A liberal arts geology major and minor are also available. Typical interests and values of geology majors: Developing evaluation strategies Strong interest and aptitude in the sciences Extracting important information Enjoy the outdoors (hiking, camping, traveling) Initiating new ideas Interested in the environment Ability to apply classroom knowledge to field Related student and professional organizations: situations Student: Ability to think in three dimensions Geology Club Ability to use computers to solve problems The Conservationists Hobnailers Club Knowledge and skills gained from studying geology: Sigma Gamma Epsilon, a national honor society for Knowledge: students in earth sciences Geology majors acquire knowledge concerning processes of the earth such as the formation of rocks, mountains Professional: and volcanoes; the shaping of the land by wind, water, American Association of Petroleum Geologists gravity and ice; the formation of soils and caves; and the Association for Women Geoscientists motion of groundwater. They also become familiar with The Geological Society of America (GSA) environmental regulations and laws.
    [Show full text]
  • A Geologist Is Someone Who Studies the Earth and the Processes Which Shape It
    КАЗАНСКИЙ ФЕДЕРАЛЬНЫЙ УНИВЕРСИТЕТ ИНСТИТУТ МЕЖДУНАРОДНЫХ ОТНОШЕНИЙ, ИСТОРИИ И ВОСТОКОВЕДЕНИЯ Кафедра английского языка в сфере медицины и биоинженерии В.В. ТАРАСОВА Э.Р. ДАМИНОВА Р. Н. САБИРОВА READING SCIENCE Учебное пособие по английскому языку для студентов естественнонаучных направлений Казань – 2016 УДК 821.111.09 ББК Ш3(4) Рекомендовано учебно-методической комиссией ИМОИиВ Протокол № __ от _____ 2016 года Рецензенты: кандидат филологических наук, доцент кафедры английского языка в сфере медицины и биоинженерии КФУ Н. М. Хабирова кандидат филологических наук, доцент кафедры иностранных языков в профессиональной коммуникации КНИТУ Г. Х. Шамсеева Тарасова В.В., Даминова Э.Р., Сабирова Р.Н. Reading science. –учеб. пособие. – Казань: Казан. ун-т, 2016 – 145с. Предлагаемое учебное пособие предназначено для студентов естественнонаучных направлений: геология, геофизика, геология, геохимия нефти и газа и др. Основная цель пособия познакомить студентов с материалами учебно-профессиональной сферы. Разделы пособия включают тексты, содержащие профессиональную терминологию, а также задания и упражнения, способствующие формированию навыков говорения в рамках профессионального общения. © Казанский университет, 2016 2 CONTENTS Unit One 5 Text 1.1 The Science of Geology 5 Text 1.2 Geologist 7 Text 1.3 Alexander Karpinsky 10 Unit Two 13 Text 2.1 History of Geology 13 Text 2.2 Petroleum Geologist 15 Text 2.3 James Hutton 18 Unit Three 22 Text 3.1 Mineralogy 22 Text 3.2 Mineralogist 25 Text 3.3 Charles Lyell 27 Unit Four 30 Text 4.1 Geophysics 30 Text
    [Show full text]
  • Geologic Past
    GEOLOGIC PAST Highlighting Articles from Past Issues of GSA Bulletin “The Problem of Petroleum” Frederick G. Clapp, GSA Bulletin, March 1939 In an “Anniversary Day” address to the Society at its semicen- Clapp, was “how to produce and distribute the volume of tennial celebration in December 1938, Frederick G. Clapp tack- petroleum which is economically necessary at any given time” les “the problem of petroleum” with a global historical view of (p. 368). Clapp blames fl uctuations in the balance between the science of petroleum geology, an analysis of the economics supply and demand for price swings “between 10 and 20 cents of “over- or undersupply” (p. 370), and a call for scientifi c fore- per barrel” (p. 369)—perhaps a pittance given the present-day sight. His speech was published in GSA Bulletin in March 1939 economic situation, but still, a 100% variance. (v. 50, p. 361–374). Clapp emphasizes the fact, as is widely acknowledged today, First, Clapp addresses the question, “Who was the fi rst petro- that “there are only a certain number of possible oil-bearing leum geologist?” (p. 362). Clapp wisely States, as is likewise the case with argues that this person or persons foreign countries. Consequently, would not “be found among our fa- even if technique should advance to thers, uncles, or contemporary teach- an unlimited extent, new discoveries ers” (p. 362), but rather would have … will in time cease” (p. 369). Clapp lived at the edge of recorded history. also predicts that even if the United The fi rst petroleum geologist could States curtailed its consumption of have been a Chinese engineer, a Baby- oil products, other nations would in- lonian navigator, a general of Alexan- crease demand, “particularly the Asi- der the Great, or even Lot, the nephew atic countries, some of which have of Abraham.
    [Show full text]
  • Profiles of Geoscientists
    Profiles of Geoscientists Susan Landon Petroleum Geologist Thomasson Partner Associates Denver, CO Education: BS, Knox College (Geology) MS, SUNY Binghamton (Geology) Job Description: Petroleum Geologist Advice to Students: "My only advice to a woman who is interested in petroleum geology is that there are tremendous opportunities." Video Transcript 1: "I have a career that is flexible enough that it sort of becomes part of every dimension of my life. My hobbies are mountain climbing, skiing, travel, and it's hard not to incorporate those sorts of activities into looking at the rocks, the geomorphology, the earth history that I'm being exposed at the same time. My family - my husband is an astronomer, so we heavens and the earth covered in our - in our partnership and it gives us an opportunity to have similar backgrounds and be able to experience and enjoy things together because of the fact that we both have scientific backgrounds." Video Transcript 2: "The petroleum industry has gone through a revolution in the last ten years. The proliferation of PC computing and the declining cost of the hardware and software associate with PC computing has allowed small companies and even independents like myself to compete on a level playing field with the major oil companies. The kind of technology that even just a decade ago you needed a mainframe to really access. Now we have it on our desktops." Video Transcript 3: "I guess that my enthusiasm for working with professional societies is directly related to my desire to give something back to my profession. Geology has been very good to me.
    [Show full text]
  • Petrophysical Modeling of the Tertiary Reservoirs in the Bai Hassan Field, Northern Iraq
    PETROPHYSICAL MODELING OF THE TERTIARY RESERVOIRS IN THE BAI HASSAN FIELD, NORTHERN IRAQ GASHAM ZEYNALOV1, MUHAMMED ISMAIL1 and FAWZI AL-BEYATI2 1 Department of Petroleum Engineering, Khazar University 41 Mehseti street, Baku AZ1096, Azerbaijan 2 Kirkuk Technical University, Baghdad street, Kirkuk 36001, Iraq Introduction The recovery efficiency of reservoir is influenced by its heterogeneities, particularity the distributions of porosity and permeability. Therefore, in order to develop a representative model of the reservoir, should be evaluated porosity, permeability properties and production potential of fields. The main aim of the research is to study the application of reservoir characterization and wireline log analyses to build a new petrophysical model for the Jeribe formation in Bai Hassan oilfield in Northern Iraq. A principal objective for building models at Bai Hassan oil field is to integrate the geological, geophysical and reservoir data collected over several decades in order to visualize and evaluate the interactions between these data using full-field reservoir simulation. Application of the petrophysical study and log analysis on Petrel software to build up static geological model and estimate the best well positions for future drilling depending on the high permeable zone resulted from the petrophysical modeling. The most important phase of a reservoir study is definition of a petrophysical model of the reservoir rock, given both the large number of activities involved, and its impact on the end results. As we are known, the production capacity is depended from geometrical and petrophysical characteristics of the reservoir. The availability of a representative static model is therefore an essential condition for the subsequent dynamic modeling (Lucia Cosentino, 2001).
    [Show full text]
  • Chapter 1: Developing a Philosophy of Exploration
    Chapter 1 Developing a Philosophy of Exploration by Edward A. Beaumont, Norman H. Foster, Richard R. Vincelette, Marlan W. Downey, and James D. Robertson Norman H. Foster Norman H. Foster received a bachelor’s degree (1957) and a master’s degree (1960) in geology at the University of Iowa. In 1963 he completed his Ph.D. in geology at the University of Kansas. His geological career began in 1962, with Sinclair Oil in Casper, Wyoming. When Sinclair merged with Arco in 1969, Foster was offered expanding opportunities to partici- pate in a number of important discoveries, including the giant Irian Jaya field in Indonesia. In 1979, he became an inde- pendent geologist and continued to prospect both in the United States and abroad. In addition to winning AAPG’s Sid- ney Powers Memorial Medal for 1999, the former AAPG president received the Levorsen Award (1980), two Certificate of Merit awards (1987 and 1992), and the Distinguished Service Award (1985). He was a member of the AAPG Foundation and an AAPG Trustee Associate since 1979. His professional activities included GSA, SEG, SPE, SIPES, SEPM, and the National Academy of Sciences. Edward A. Beaumont Edward A. (Ted) Beaumont is an independent petroleum geologist from Tulsa, Oklahoma. He holds a BS in geology from the University of New Mexico and an MS in geology from the University of Kansas. Currently, he is generating drilling prospects in Texas, Oklahoma, and the Rocky Mountains. His previous professional experience was as a sedimentologist in basin analysis with Cities Service Oil Company and as Science Director for AAPG.
    [Show full text]
  • A Petroleum Geologist's Guide to Seismic Reflection William Ashcroft
    To purchase this product, please visit https://www.wiley.com/en-us/9781444332636 A Petroleum Geologist's Guide to Seismic Reflection William Ashcroft E-Book 978-1-444-39786-4 March 2011 $80.00 Paperback 978-1-444-33263-6 May 2011 $99.75 Hardcover 978-1-444-33262-9 May 2011 $183.00 DESCRIPTION This book is written for advanced earth science students, geologists, petroleum engineers and others who want to get quickly ‘up to speed’ on the interpretation of reflection seismic data. It is a development of material given to students on the MSc course in Petroleum Geology at Aberdeen University and takes the form of a course manual rather than a systematic textbook. It can be used as a self-contained course for individual study, or as the basis for a class programme. The book clarifies those aspects of the subject that students tend to find difficult, and provides insights through practical tutorials which aim to reinforce and deepen understanding of key topics and provide the reader with a measure of feedback on progress. Some tutorials may only involve drawing simple diagrams, but many are computer-aided (PC based) with graphics output to give insight into key steps in seismic data processing or into the seismic response of some common geological scenarios. Part I of the book covers basic ideas and it ends with two tutorials in 2-D structural interpretation. Part II concentrates on the current seismic reflection contribution to reservoir studies, based on 3-D data. ABOUT THE AUTHOR After gaining his geology degree, Dr Ashcroft worked with Seismograph Service Ltd on seismic parties in the Middle East and Nigeria, then went on to do research at Birmingham University.
    [Show full text]