SEG Near-Surface Geophysics Technical Section Annual Meeting

Total Page:16

File Type:pdf, Size:1020Kb

SEG Near-Surface Geophysics Technical Section Annual Meeting The 2018 SEG Near-Surface Geophysics Technical Section Proposed Technical Sessions (Please note, the identified session topics here are not inclusive of all possible near-surface geophysics technical sessions, but have been identified at this point.) Session topic/title Session description and objective Coupled above and below-ground Description: There have been significant advances in a variety of geophysical techniques in the past decades to characterize near- monitoring using geophysics, UAV, surface critical zone heterogeneity, including hydrological and biogeochemical properties, as well as near-surface spatiotemporal and remote sensing dynamics such as temperature, soil moisture and geochemical changes. At the same time, above-ground characterization is evolving significantly – particularly in airborne platforms and unmanned aerial vehicles (UAV) – to capture the spatiotemporal dynamics in microtopography, vegetation and others. The critical link between near-surface and surface properties has been recognized, since surface processes dictates the evolution of near-surface environments evolve (e.g., topography influences surface/subsurface flow, affecting bedrock weathering), while near-surface properties (such as soil texture) control vegetation and topography. Now that geophysics and airborne technologies can capture both surface and near-surface spatiotemporal dynamics at high resolution in a spatially extensive manner, there is a great opportunity to advance the understanding of this coupled surface and near-surface system. This session calls for a variety of contributions on this topic, including coupled above/below-ground sensing technologies, new geophysical techniques to characterize the interactions between near-surface and surface environments. Near-surface modeling using Description: The first few meters of the subsurface is of paramount importance to the engineering and environmental industry. tomography Accurate estimations of physical properties are challenging in these areas because of the unconsolidated nature of the material. This even makes lab testing for strength, compaction and porosity very difficult without inducing any disturbances. Using tomography on geophysical data in general, due to their non-intrusive nature and sensitivity to the state of soil/rock consolidation can be a promising tool for investigating the physical properties of this zone. Objectives: 1. To have a common session on tomographic application in near-surface modeling 2. To be able to compare and contrast different tomographic analysis in shallow subsurface characterization, and their pros and cons Petrophysical relationship - link Description: Geophysical tools show the promise to provide spatiotemporal information of subsurface hydrogeological properties in a hydrologic parameters with minimal invasive way. Accurate characterization of subsurface using geophysical tools is challenging due to incomplete understanding geophysical signals of how the highly coupled physical, biological, and geochemical processes occurring spatiotemporally change the geophysical responses. The link between the geophysical signals with subsurface parameters of interests requires understanding of petrophysical relationships and coupled fluid flow and biogeochemical processes. Several petrophysical relationships have been established and most of them are empirical and database dependent. Recently new theoretical or empirical models have been significantly explored to provide mechanical explanation of geophysical responses and/or simulate the effective properties of porous media. This workshop will provide the opportunities for experts in rock physics and anyone who is interested in petrophysical relationships with applications to both hydrogeological investigations. The topics include theoretical developments, laboratory experiments, and field demonstration. Developments and Applications of Description: Active and passive (ambient vibration) surface wave techniques, including the multi-channel analysis of surface Active and Passive Source Surface waves(MASW), spectral analysis of surface waves (SASW), array microtremor, H/V spectral ratio methods have become increasingly Wave Methods popular over the past 15 years. Surface wave measurements may involve acquisition of Rayleigh wave data, Love wave data, or both. Surface wave techniques are often used for site characterization as part of earthquake hazard assessment. Other applications include (Special Session) mapping bedrock and fault zones, compaction control for the pads of critical structures, pavement assessment, levee assessment, geologic site characterization, void mapping, etc. Objectives: In this session, we welcome presentations on new developments in data acquisition, data reduction and modeling/inversion strategies. Case studies with practical applications of surface wave methods are also welcome. Coastal Zone geophysics Description: The Coastal Zone is one of the most important environments on earth where major cities are heavily populated, and ports and harbors and coastlines include substantial infrastructure necessary for society to survive and enjoy. Because the Coastal Zone spans the region from land to water, there are special requirements for obtaining subsurface information needed to identify and map potential environmental hazards. Site surveys are needed to plan routes for pipelines and other coastal infrastructure, and to locate obstacles for planned construction. Major coastal infrastructure includes energy, transportation, water supply, hydrocarbon production, processing and storage, waste management, and critical defense installations. Due to the difficult data acquisition within the transition zone – where water meets land – the Coastal Zone may be considered the biggest data gap in earth sciences. Consequently, a session to examine numerous examples of data acquisition, processing and interpretation to understand this critical environment and provide important lessons for continued research and commercial projects within the Coastal Zone. Southern California is a natural place to focus attention on Coastal Zone geophysics which are important around the world including all areas where water and land meet – oceans, lakes and rivers. Objective: The proposed session will provide numerous examples of near surface (and deeper) geophysics used to solve important societal problems including environment, natural hazards, coastal infrastructure, and national defense. Some examples may include coastal energy systems such as offshore wind farms, ocean thermal energy, hydrocarbon production, processing, and storage, water supply (desalination and seawater intrusion), waste treatment and disposal (e.g., CO2 sequestration, sewage, waste water from hydrocarbon production), earthquake, tsunami, storm surge, sea level rise, riverine flooding and water-related hazards to harbors, ports, bridges and other coastal infrastructure, and coastal populations. In addition, the numerous government regulations regarding geophysical work in the sensitive coastal environment need to be addressed and reviewed to help provide a coordinated planning and data acquisition framework for continued successful development and enjoyment of the Coastal Zone. Noise attenuation techniques in Description: Near surface seismic surveys are typically acquired under economic constraints that do not allow for anything approaching near-surface seismic surveys an optimal survey design. In the case of near surface reflection seismic surveys, the observation is frequently made that there is little or no visible signal. The observation could also be made that there is just too much noise. In either case, reducing/attenuating noise in the acquired seismic data is critical in generating interpretable seismic products. The proposed technical session seeks to merge talks that describe acquisition strategies for improving signal-to-noise in the recorded seismic data with talks that describe processing algorithms and/or strategies for attenuating noise in the processed seismic data. Objective: The goal of the session will be to highlight the interplay between these aspects of data acquisition and data processing in near surface reflection surveys. The session seeks to have an even distribution of acquisition and processing presentations. Acquisition strategies should be illustrated through case studies. Description: Airborne geophysics uses aircraft, helicopter, or UAV to tow geophysical instruments to do geophysical survey, including Airborne geophysics airborne gravity, magnetics, EM and radiometry. Due to its moving platform, airborne geophysics has been widely used in mountains, deserts, lakes and swamps, and forest-covered areas for mineral exploration, oil & gas, environmental and engineering, groundwater, and ocean investigation, etc. This technology has special usage in NSG due to its high resolution near the Earth’s surface. However, the forward modeling and inversion theory, the instrumentation and the data processing and interpretation are still underdeveloped and have much room for improvement. To set up the session on airborne geophysics in this meeting will certainly help speed up largely the development of this technology. Near-surface geophysics applied to Description: The search and characterization of earthen archaeological features is an important topic in geophysical prospecting for archaeological research archaeology due to the large temporal and spatial distribution of such type of cultural heritage. Earthen
Recommended publications
  • Preprint Arxiv:1806.10939, 2018
    Solid Earth Discuss., https://doi.org/10.5194/se-2019-4 Manuscript under review for journal Solid Earth Discussion started: 15 January 2019 c Author(s) 2019. CC BY 4.0 License. Bayesian geological and geophysical data fusion for the construction and uncertainty quantification of 3D geological models Hugo K. H. Olierook1, Richard Scalzo2, David Kohn3, Rohitash Chandra2,4, Ehsan Farahbakhsh2,4, Gregory Houseman3, Chris Clark1, Steven M. Reddy1, R. Dietmar Müller4 5 1School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA 6845, Australia 2Centre for Translational Data Science, University of Sydney, NSW 2006 Sydney, Australia 3Sydney Informatics Hub, University of Sydney, NSW 2006 Sydney, Australia 4EarthByte Group, School of Geosciences, University of Sydney, NSW 2006 Sydney, Australia Correspondence to: Hugo K. H. Olierook ([email protected]) 10 Abstract. Traditional approaches to develop 3D geological models employ a mix of quantitative and qualitative scientific techniques, which do not fully provide quantification of uncertainty in the constructed models and fail to optimally weight geological field observations against constraints from geophysical data. Here, we demonstrate a Bayesian methodology to fuse geological field observations with aeromagnetic and gravity data to build robust 3D models in a 13.5 × 13.5 km region of the Gascoyne Province, Western Australia. Our approach is validated by comparing model results to independently-constrained 15 geological maps and cross-sections produced by the Geological Survey of Western Australia. By fusing geological field data with magnetics and gravity surveys, we show that at 89% of the modelled region has >95% certainty. The boundaries between geological units are characterized by narrow regions with <95% certainty, which are typically 400–1000 m wide at the Earth’s surface and 500–2000 m wide at depth.
    [Show full text]
  • Geophysics (3 Credits) Spring 2018
    GEO 3010 – Geophysics (3 credits) Spring 2018 Lecture: FASB 250, 10:45-11:35 am, M & W Lab: FASB 250, 2:00-5:00 pm, M or W Instructor: Fan-Chi Lin (Assistant Professor, Dept. of Geology & Geophysics) Office: FASB 271 Phone: 801-581-4373 Email: [email protected] Office Hours: M, W 11:45 am - 1:00 pm. Please feel free to email me if you would like to make an appointment to meet at a different time. Teaching Assistants: Elizabeth Berg ([email protected]) FASB 288 Yadong Wang ([email protected]) FASB 288 Office Hours: T, H 1:00-3:00 pm Website: http://noise.earth.utah.edu/GEO3010/ Course Description: Prerequisite: MATH 1220 (Calculus II). Co-requisite: GEO 3080 (Earth Materials I). Recommended Prerequisite: PHYS 2220 (Phycs For Scien. & Eng. II). Fulfills Quantitative Intensive BS. Applications of physical principles to solid-earth dynamics and solid-earth structure, at both the scale of global tectonics and the smaller scale of subsurface exploration. Acquisition, modeling, and interpretation of seismic, gravity, magnetic, and electrical data in the context of exploration, geological engineering, and environmental problems. Two lectures, one lab weekly. 1. Policies Grades: Final grades are based on following weights: • Homework (25 %) • Labs (25 %) • Exam 1-3 (10% each) • Final (20 %) Homework: There will be approximately 6 homework sets. Homework must be turned in by 5 pm of the day they are due. 10 % will be marked off for each day they are late. Homework will not be accepted 3 days after the due day. Geophysics – GEO 3010 1 Labs: Do not miss labs! In general you will not have a chance to make up missed labs.
    [Show full text]
  • SOP14 Geophysical Survey
    SSFL Use Only SSFL SOP 14 Geophysical Survey Revision: 0 Date: April 2012 Prepared: C. Werden Technical Review: J. Plevniak Approved and QA Review: J. Oxford Issued: 4/6/2012 Signature/Date 1.0 Objective The purpose of this technical standard operating procedure (SOP) is to introduce the procedures for non-invasive geophysical investigations in areas suspected of being used for disposal of debris or where landfill operations may have been conducted. Specifics of the geophysical surveys will be discussed in the Geophysical Survey Field Sampling Plan Addendum. Geophysical methods that will be used to accurately locate and record buried geophysical anomalies are: . Total Field Magnetometry (TFM) . Frequency Domain Electromagnetic Method (FDEM) . Ground Penetrating Radar (GPR) TFM and FDEM will be applied to all areas of interest while GPR will be applied only to areas of interest that require further and/or higher resolution of geophysical anomaly. The geophysical investigation (survey) will be conducted by geophysical subcontractor personnel trained, experienced, and qualified in shallow subsurface geophysics necessary to successfully perform any of the above geophysical methods. CDM Smith will provide oversight of the geophysical contractor. 2.0 Background 2.1 Discussion This SOP is based on geophysical methods employed by US Environmental Protection Agency’s (EPA) subcontractor Hydrogeologic Inc. (HGL) while conducted geophysical surveys of portions of Area IV during 2010 and 2011. The Data Gap Investigation conducted as part of Phase 3 identified additional locations of suspected buried materials not surveyed by HGL. To be consistent with the recently collected subsurface information, HGL procedures are being adopted. The areas of interest and survey limits will be determined prior to field mobilization.
    [Show full text]
  • Geophysical Investigations of Well Fields to Characterize Fractured-Bedrock Aquifers in Southern New Hampshire
    In Cooperation with the NEW HAMPSHIRE DEPARTMENT OF ENVIRONMENTAL SERVICES o Geophysical Investigations of Well Fields to Characterize Fractured-Bedrock Aquifers in Southern New Hampshire Water-Resources Investigations Report 01-4183 U.S. Department of the Interior / U.S. Geological Survey The base map on the front cover shows geophysical survey locations overlaying a geologic map of U.S. Geological Survey, Windham, New Hampshire, 1:24,000-scale quadrangle. Geology is by G.S. Walsh and S.F. Clark, Jr. (1999) and lineaments are from Ferguson and others (1997) and R.B. Moore and Garrick Marcoux, 1998. The photographs and graphics overlying the base map are showing, counterclockwise from the left, a USGS scientist using a resistivity meter and surveying equipment (background) to survey the bedrock beneath the surface using a geophysical method called azimuthal square-array direct- current resistivity. In the lower left, this cross section is showing the results of a survey along line 3 in Windham, N.H., using another method called two-dimensional direct-current resistivity. In the lower right, the photograph is showing a bedrock outcrop located between red lines 3 and 4 (on base map) at Windham, in which the fractures and parting parallel to foliation have the same strike as the azimuthal square-array direct-current resistivity survey results, and remotely sensed lineaments (purple and green lines on base map). The upper right graphic shows a polar plot of the results of an azimuthal square-array direct-current resistivity survey at Windham for array 1 (red circle on base map). U.S. Department of the Interior U.S.
    [Show full text]
  • An Introduction to Geophysical Exploration, 3E
    An Introduction to Geophysical Exploration Philip Kearey Department of Earth Sciences University of Bristol Michael Brooks Ty Newydd, City Near Cowbridge Vale of Glamorgan Ian Hill Department of Geology University of Leicester THIRD EDITION AN INTRODUCTION TO GEOPHYSICAL EXPLORATION An Introduction to Geophysical Exploration Philip Kearey Department of Earth Sciences University of Bristol Michael Brooks Ty Newydd, City Near Cowbridge Vale of Glamorgan Ian Hill Department of Geology University of Leicester THIRD EDITION © 2002 by The right of the Authors to be distributors Blackwell Science Ltd identified as the Authors of this Work Marston Book Services Ltd Editorial Offices: has been asserted in accordance PO Box 269 Osney Mead, Oxford OX2 0EL with the Copyright, Designs and Abingdon, Oxon OX14 4YN 25 John Street, London WC1N 2BS Patents Act 1988. (Orders: Tel: 01235 465500 23 Ainslie Place, Edinburgh EH3 6AJ Fax: 01235 465555) 350 Main Street, Malden All rights reserved. No part of MA 02148-5018, USA this publication may be reproduced, The Americas 54 University Street, Carlton stored in a retrieval system, or Blackwell Publishing Victoria 3053,Australia transmitted, in any form or by any c/o AIDC 10, rue Casimir Delavigne means, electronic, mechanical, PO Box 20 75006 Paris, France photocopying, recording or otherwise, 50 Winter Sport Lane except as permitted by the UK Williston,VT 05495-0020 Other Editorial Offices: Copyright, Designs and Patents Act (Orders: Tel: 800 216 2522 Blackwell Wissenschafts-Verlag GmbH 1988, without the prior
    [Show full text]
  • Geophysical Methods Commonly Employed for Geotechnical Site Characterization TRANSPORTATION RESEARCH BOARD 2008 EXECUTIVE COMMITTEE OFFICERS
    TRANSPORTATION RESEARCH Number E-C130 October 2008 Geophysical Methods Commonly Employed for Geotechnical Site Characterization TRANSPORTATION RESEARCH BOARD 2008 EXECUTIVE COMMITTEE OFFICERS Chair: Debra L. Miller, Secretary, Kansas Department of Transportation, Topeka Vice Chair: Adib K. Kanafani, Cahill Professor of Civil Engineering, University of California, Berkeley Division Chair for NRC Oversight: C. Michael Walton, Ernest H. Cockrell Centennial Chair in Engineering, University of Texas, Austin Executive Director: Robert E. Skinner, Jr., Transportation Research Board TRANSPORTATION RESEARCH BOARD 2008–2009 TECHNICAL ACTIVITIES COUNCIL Chair: Robert C. Johns, Director, Center for Transportation Studies, University of Minnesota, Minneapolis Technical Activities Director: Mark R. Norman, Transportation Research Board Paul H. Bingham, Principal, Global Insight, Inc., Washington, D.C., Freight Systems Group Chair Shelly R. Brown, Principal, Shelly Brown Associates, Seattle, Washington, Legal Resources Group Chair Cindy J. Burbank, National Planning and Environment Practice Leader, PB, Washington, D.C., Policy and Organization Group Chair James M. Crites, Executive Vice President, Operations, Dallas–Fort Worth International Airport, Texas, Aviation Group Chair Leanna Depue, Director, Highway Safety Division, Missouri Department of Transportation, Jefferson City, System Users Group Chair Arlene L. Dietz, A&C Dietz and Associates, LLC, Salem, Oregon, Marine Group Chair Robert M. Dorer, Acting Director, Office of Surface Transportation Programs, Volpe National Transportation Systems Center, Research and Innovative Technology Administration, Cambridge, Massachusetts, Rail Group Chair Karla H. Karash, Vice President, TranSystems Corporation, Medford, Massachusetts, Public Transportation Group Chair Mary Lou Ralls, Principal, Ralls Newman, LLC, Austin, Texas, Design and Construction Group Chair Katherine F. Turnbull, Associate Director, Texas Transportation Institute, Texas A&M University, College Station, Planning and Environment Group Chair Daniel S.
    [Show full text]
  • Geophysical Field Mapping
    Presented at Short Course IX on Exploration for Geothermal Resources, organized by UNU-GTP, GDC and KenGen, at Lake Bogoria and Lake Naivasha, Kenya, Nov. 2-23, 2014. Kenya Electricity Generating Co., Ltd. GEOPHYSICAL FIELD MAPPING Anastasia W. Wanjohi, Kenya Electricity Generating Company Ltd. Olkaria Geothermal Project P.O. Box 785-20117, Naivasha KENYA [email protected] or [email protected] ABSTRACT Geophysics is the study of the earth by the quantitative observation of its physical properties. In geothermal geophysics, we measure the various parameters connected to geological structure and properties of geothermal systems. Geophysical field mapping is the process of selecting an area of interest and identifying all the geophysical aspects of the area with the purpose of preparing a detailed geophysical report. The objective of geophysical field work is to understand all physical parameters of a geothermal field and be able to relate them with geological phenomenons and come up with plausible inferences about the system. Four phases are involved and include planning/desktop studies, reconnaissance, actual data aquisition and report writing. Equipments must be prepared and calibrated well. Geophysical results should be processed, analysed and presented in the appropriate form. A detailed geophysical report should be compiled. This paper presents the reader with an overview of how to carry out geophysical mapping in a geothermal field. 1. INTRODUCTION Geophysics is the study of the earth by the quantitative observation of its physical properties. In geothermal geophysics, we measure the various parameters connected to geological structure and properties of geothermal systems. In lay man’s language, geophysics is all about x-raying the earth and involves sending signals into the earth and monitoring the outcome or monitoring natural signals from the earth.
    [Show full text]
  • A Continuous Plate-Tectonic Model Using Geophysical Data to Estimate
    GEOPHYSICAL JOURNAL INTERNATIONAL, 133, 379–389, 1998 1 A continuous plate-tectonic model using geophysical data to estimate plate margin widths, with a seismicity based example Caroline Dumoulin1, David Bercovici2, Pal˚ Wessel Department of Geology & Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, 96822, USA Summary A continuous kinematic model of present day plate motions is developed which 1) provides more realistic models of plate shapes than employed in the original work of Bercovici & Wessel [1994]; and 2) provides a means whereby geophysical data on intraplate deformation is used to estimate plate margin widths for all plates. A given plate’s shape function (which is unity within the plate, zero outside the plate) can be represented by analytic functions so long as the distance from a point inside the plate to the plate’s boundary can be expressed as a single valued function of azimuth (i.e., a single-valued polar function). To allow sufficient realism to the plate boundaries, without the excessive smoothing used by Bercovici and Wessel, the plates are divided along pseudoboundaries; the boundaries of plate sections are then simple enough to be modelled as single-valued polar functions. Moreover, the pseudoboundaries have little or no effect on the final results. The plate shape function for each plate also includes a plate margin function which can be constrained by geophysical data on intraplate deformation. We demonstrate how this margin function can be determined by using, as an example data set, the global seismicity distribution for shallow (depths less than 29km) earthquakes of magnitude greater than 4.
    [Show full text]
  • The Reunification of Seismology and Geophysics Brad Artman Exploration Geophysics – a Brief History
    The Reunification of Seismology and Geophysics Brad Artman Exploration geophysics – a brief history J.C. Karcher patents the reflection seismic method, focused the exploration geophysicist for the next century Beno Guttenberg becomes a professor of seismology Gas research institute, Teledyne Geotech, & Sandia National Labs develop equipment and techniques for microseismic monitoring to illuminate hydraulic fracturing 1920 1930 1940 1950 1960 1970 1980 1990 2000 2010 2013 Rapid advances in computational capabilities allow processing of ever-larger data volumes with more complete physics Exploration geophysics begins (re) learning earthquake seismology to commercialize microseismic monitoring Today, we have the opportunity to capitalize on the strengths of 100 yrs of development in both communities © Spectraseis Inc. 2013 2 Strength comparison To extract the full Seismology Geophysics potential from these Better sensors More sensors measurements, Better physics More compute horsepower we must capture the best of both Bigger events Smaller domain knowledge bases. Seismologists use cheap computers (grad. students) to do very thorough analysis on small numbers of traces. Geophysicists use cheap computers (clusters) to do good- enough approximations on very large numbers of traces. The merger of these fields is an historic opportunity to do exciting and valuable work © Spectraseis Inc. 2013 3 Agenda Sensor selection Survey design Processing algorithms and computer requirements Conclusions © Spectraseis Inc. 2013 4 Fracture mechanisms Compensated Linear Isotropic Double Couple Vector Dipole (explosion) (DC) (CLVD) P-waves only P- and S-waves P- and S-waves All fractures can be decomposed into these three mechanisms © Spectraseis Inc. 2013 5 DC radiation and particle motion Particle motion of P waves is compressional and in the same direction direction to the traveling wavefront.
    [Show full text]
  • Equivalence of Current–Carrying Coils and Magnets; Magnetic Dipoles; - Law of Attraction and Repulsion, Definition of the Ampere
    GEOPHYSICS (08/430/0012) THE EARTH'S MAGNETIC FIELD OUTLINE Magnetism Magnetic forces: - equivalence of current–carrying coils and magnets; magnetic dipoles; - law of attraction and repulsion, definition of the ampere. Magnetic fields: - magnetic fields from electrical currents and magnets; magnetic induction B and lines of magnetic induction. The geomagnetic field The magnetic elements: (N, E, V) vector components; declination (azimuth) and inclination (dip). The external field: diurnal variations, ionospheric currents, magnetic storms, sunspot activity. The internal field: the dipole and non–dipole fields, secular variations, the geocentric axial dipole hypothesis, geomagnetic reversals, seabed magnetic anomalies, The dynamo model Reasons against an origin in the crust or mantle and reasons suggesting an origin in the fluid outer core. Magnetohydrodynamic dynamo models: motion and eddy currents in the fluid core, mechanical analogues. Background reading: Fowler §3.1 & 7.9.2, Lowrie §5.2 & 5.4 GEOPHYSICS (08/430/0012) MAGNETIC FORCES Magnetic forces are forces associated with the motion of electric charges, either as electric currents in conductors or, in the case of magnetic materials, as the orbital and spin motions of electrons in atoms. Although the concept of a magnetic pole is sometimes useful, it is diácult to relate precisely to observation; for example, all attempts to find a magnetic monopole have failed, and the model of permanent magnets as magnetic dipoles with north and south poles is not particularly accurate. Consequently moving charges are normally regarded as fundamental in magnetism. Basic observations 1. Permanent magnets A magnet attracts iron and steel, the attraction being most marked close to its ends.
    [Show full text]
  • Geophysical Abstracts 136-139 January-December 1949 (Numbers 10737-11678)
    Geophysical Abstracts 136-139 January-December 1949 (Numbers 10737-11678) Abstracts of world literature t contained in periodicals, books, and patents OHIO GEOLOGICAL SURVEY UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director \ « For sale by the Superintendent of Documents, U. S._ Government Printing Office Washington 25, D. C. - Price 5 cents (paper cover) CONTENTS [The letters in parentheses are those used]to designate the chapters for separate publication] Page <A) Geophysical Abstracts 136, January-March 1949 (nos. 10737-11001). 1 <B) Geophysical Abstracts 137, April-June 1949 (nos. 11002-11201__ 95 <C) Geophysical Abstracts 138, July-September 1949 (nos. 11202-11441). 167 (D) Geophysical Abstracts 139, October-December, 1949 (nos. 11442- 11678....._________________________________________________ 253 Under Departmental orders, Geophysical Abstracts have been published at different times by the Bureau of Mines or the Geological Survey as noted below: 1-86, May 1929-June 1936, Bureau of Mines, Information Circulars. [Mimeo­ graphed.] 87, July-December 1937, Geological Survey, Bulletin 887. 88-91, January-December 1937, Geological Survey, Bulletin 895. 92-95, January-December 1938, Geological Survey Bulletin 909. 96-99, January-December 1939, Geological Survey, Bulletin 915. 100-103, January-December 1940, Geological Survey, Bulletin 925. 104-107, January-December 1941, Geological Survey, Bulletin 932. 108-111, January-December 1942, Geological Survey, Bulletin 939. 112-127, January 1943-December 1946, Bureau of Mines, Information Circulars. [Mimeographed.] 128-131, January-December 1947, Geological Survey, Bulletin 957. 132-135, January-December 1948, Geological Survey, Bulletin 959. in Geophysical Abstracts 136 January-March 1949 (Numbers 10737-11001) By V.
    [Show full text]
  • Geophysical Investigation Report Bennett's Dump Site
    EPA Region 5 Records Ctr. 248323 GEOPHYSICAL INVESTIGATION REPORT BENNETT'S DUMP SITE BLOOMINGTON PROJECT Bloomington, Indiana CBS Corporation 11 Stanwix Street Pittsburgh, PA 15222-1384 February 22,1999 TABLE OF CONTENTS Section Title Page 1.0 Introduction 1 2.0 Summary of Field Activities 2 2.1 Site Preparation 2 2.2 Geophysical Survey 3 3.0 Summary of Findings 6 3.1 Electromagnetic and Magnetometer Results 6 3.2 Seismic Refraction Study Results 7 4.0 Conclusions 11 List of Figures 1 Site Location Map 2 Site Layout Map 3 Geophysical Sample Location Map 4 Generalized Electromagnetic Anomaly Map 5 Lithologic Profiles 6 Bedrock Contour Map 7 Top of Clay Layer Contour Map Appendices A Geosphere Inc. Report B Soil Boring Logs 1.0 INTRODUCTION Previous investigations led by the U.S. Environmental Protection Agency (USEPA) at the Bennett's Dump site have identified various electromagnetic anomalies. Since the primary method of site cleanup will involve excavation of portions of the site, a refined understanding of the subsurface conditions was required to aid in planning of future delineation studies. A geophysical survey, including an electromagnetic survey, a magnetometer survey, and a seismic refraction study, were performed at the Bennett's Dump site during the week of December 14,1998. This report summarizes the geophysical survey, presents the geophysicist's findings, and, based on data gathered herein as well as from previous boring projects, provides a summary of the local geology. The complete report of the geophysical results provided by the geophysics contractor is included in Appendix A. The seismic investigation was conducted to provide an understanding of the subsurface structures in areas most likely to contain large amounts of fill.
    [Show full text]