The Role of Vertical Seismic Profiles in Core, Log, Seismic Integration Ralph Stephen, WHOI CLSI Workshop, Tokyo October 3-4, 2005 Ralph Stephen, WHOI.

Slides:



Advertisements
Similar presentations
Types of Data Lecture 3 Mega-Regional Local Present Circulation
Advertisements

Time-Lapse Monitoring of CO2 Injection with Vertical Seismic Profiles (VSP) at the Frio Project T.M. Daley, L.R. Myer*, G.M. Hoversten and E.L. Majer.
Designer Seismic VSP Ernie Majer (LBNL) J. Queen ( Hi –Q Geophysics) T. Dalely (LBNL) Roy Long ( DOE)
8. Ocean Crustal Structure and Seismic Reflection William Wilcock (via Michelle W.) OCEAN/ESS 410.
The sea floor. seafloor water covers 70% of Earth’s surface.
March 25, 2002EarthScope CSIT Workshop Data Archiving and IT Issues for PBO Douglas Neuhauser UC Berkeley Seismological Lab Northern California Earthquake.
Seismological Crust Models for KamLAND Experiment Nozomu Takeuchi (University of Tokyo)
Geology of the Lithosphere 2. Evidence for the Structure of the Crust & Upper Mantle What is the lithosphere and what is the structure of the lithosphere?
IODP Town Hall Meeting 2004 Fall AGU Meeting San Francisco, CA 14 December 2004 IODP Town Hall Meeting 2004 Fall AGU Meeting San Francisco, CA 14 December.
Mid-Ocean Ridges: A Connected System Hydrothermal circulation links ocean, seafloor, and crust, including vent communities How is fluid circulation controlled.
What is a reflector? There are many reflectors on a seismic section. Major changes in properties usually produce strong, continuous reflectors as shown.
Lab 2 Seismogram Interpretation
Three Worlds to Explore Look Up? (Astronomy) Look Down? (Geophysics) Look at Surface? (Geology)
Applied Geophysics An Introduction
EARTHQUAKES.
  The word comes from the Greek word seismic, for shaking.  It is the branch of Geology which has provided the most comprehensive interpretation of.
Head Waves, Diving Waves and Interface Waves at the Seafloor Ralph Stephen, WHOI ASA Fall Meeting, Minneapolis October 19, 2005 Ralph Stephen, WHOI ASA.
GG 450 April 15, 2008 Refraction Applications. While refraction is used for engineering studies such as depth to basement and depth to the water table,
SEEING FROM HEARING VISUALIZING CRUSTAL THICKNESS FROM ACTIVE- SOURCE SEISMOLOGY..
Faults and Earthquakes
Lecture items - Logging Up? - Wireline Log Services. - What Logs can measure? - The role of the Well Log Analyst - Creating the Well Log “Logging Operation”
Overview of NanTroSEIZE: The Nankai Trough Seismogenic Zone Experiment
Eagle Mountain – Woodfibre Gas Pipeline Project Geotechnical and geophysical tests James Lota, FortisBC September 25, 2014.
Understanding Earth Fifth Edition Chapter 14: EXPLORING EARTH’S INTERIOR Copyright © 2007 by W. H. Freeman and Company Grotzinger Jordan Press Siever.
John N. Dougherty, PG Lisa Campbell, PG EPA Region 2, New York City
Geology 5660/6660 Applied Geophysics 17 Jan 2014 © A.R. Lowry 2014 Read for Wed 22 Jan: Burger (Ch 2.2–2.6) Last time: The Wave Equation; The Seismometer.
An Earth science program to explore the 4D structure of the North American continent Kaye Shedlock EarthScope Program Director.
Plus an Introduction to the: Institute of Earth Science & Engineering RESOURCE INDEX MAPPING: Getting the Right Data for the Right Model.
Seismic Hazard Map EPOS European Plate Observing System RESEARCH INFRASTRUCTURE AND E-SCIENCE FOR DATA AND OBSERVATORIES ON EARTHQUAKES, VOLCANOES, SURFACE.
5. Seismology William Wilcock OCEAN/ESS 410. A. Earthquake Seismology.
SOES6002: Modelling in Environmental and Earth System Science CSEM Lecture 1 Martin Sinha School of Ocean & Earth Science University of Southampton.
Basic research needs workshop for Materials Under Extreme Environments Plenary Closing Session June 13, 2007 BREAKOUT SESSION 2: DEEP CARBON FLUXES What.
Geology 5660/6660 Applied Geophysics 19 Feb 2014 © A.R. Lowry 2014 For Fri 21 Feb: Burger (§ ) Last Time: Reflection Data Processing Step.
Marine Resistivity: a Tool for Characterizing Sediment Zones.
Geology 5660/6660 Applied Geophysics 23 Apr 2014 © A.R. Lowry 2014 Last Time: Wireline Logging Wireline Logging is the practice of lowering a geophysical.
© 2005 Paulsson Geophysical Characterization of the San Andreas Fault at Parkfield Using a Massive 3D VSP J. Andres Chavarria, Alex Goertz, Martin Karrenbach,
The main instrument used is called the sonde. A basic sonde consists of a source and two receivers one-foot apart. The sonde is lowered down the borehole.
Of EgyptSeismicity BadawyAhmed National Research Institute of Astronomy and Geophysics, Cairo, EGYPTHelwan Abstract. Spatial distribution of earthquake.
Warm-Up Write a paragraph describing what it is like to be in an earthquake. If you have never been in one, MAKE IT UP! Write about what you THINK it would.
STRESS – The amount of force exerted on a material.
Analyzing pressure responses to Earth tides for monitoring CO 2 migration Kozo Sato Geosystem Engineering The University of Tokyo.
The Structure of the Earth and Plate Tectonics. Structure of the Earth The Earth is made up of 3 main layers: –Core –Mantle –Crust Inner core Outer core.
Geology 5660/6660 Applied Geophysics 20 Jan 2016
Geology 5660/6660 Applied Geophysics 22 Jan 2016 © A.R. Lowry 2016 For Mon 25 Jan: Burger (Ch 2.2.2–2.6) Last time: The Seismometer A seismometer.
Geology 5660/6660 Applied Geophysics 20 Apr 2016
1 Introduction to Applied Geophysics & Geophysical Exploration Prof Jeannot Trampert (coordinator) Dr Fred Beekman
CodeClass 1 Course Title Interpretation of Reflection data & petroleum Exploration Credit Lecturer Kim, Ki Young Rm NS3-303 Office Hour By appointment.
Data Integration Challenges Building 3-D models of earth structure via integration of geological and geophysical data - schemes, data models, and work.
A Fiber-Optic Borehole Seismic
Erno Takacs 1, Zoltan Hajnal 1, Bhaskar Pandit 1 1 Department of Geological Sciences, U of S ______________________________________________________ Joint.
Introduction to Seismology
Bellringer Explain in complete sentences what are pros and cons of coal energy use.
Geology 5660/6660 Applied Geophysics 18 Apr 2016 © A.R. Lowry 2016 Last Time: Magnetotellurics (MT) Some (minor but growing) applications in oil & mining;
Seismic Methods Geoph 465/565 Vertical Seismic Profiling– Nov 2, 2015
January 24, Earthquake Engineering GE / CEE - 479/679 Lecture 2. Plate Tectonics January 24, 2008 John G. Anderson Professor of Geophysics.
ON THE GEOTHERMAL REGIME OF THE FORELAND OF THE EASTERN CARPATHIANS BEND C. Demetrescu 1, H. Wilhelm 2, M. Andreescu 1, V. Dobrica 1, D.Z. Serban 1, A.
EXPLORING EARTH’S INTERIOR
INSTRUCTOR © 2017, John R. Fanchi
Argo’s Role in Climate Science
Wyoming Blair Wallis Fractured Rock Hydrology Research
Session 4: GOCE for Solid Earth
Geology 5660/6660 Applied Geophysics 22 Apr 2016
Marine Reflection Seismology - Geometry
Geophysical exploration in and around CTD
Elements of 3D Seismology: Introduction to Interpretation
Detection of Mobile Fluids
Overview of current and upcoming field projects
Comparison of Seismic and Well Data
Geophysics/Tectonics
Packing of uniform spheres
Presentation transcript:

The Role of Vertical Seismic Profiles in Core, Log, Seismic Integration Ralph Stephen, WHOI CLSI Workshop, Tokyo October 3-4, 2005 Ralph Stephen, WHOI CLSI Workshop, Tokyo October 3-4, 2005

The first application of borehole seismology on DSDP - the Oblique Seismic Experiment - was to correlate core and logging observations with surface seismic refraction observations of crustal structure.

Head Waves versus Diving Waves (Horizontal Component) Observed data Thick layer model of oceanic crust based on head waves. Gradient layer model of oceanic crust based on diving waves.

Correlation of lithology from cores, resistivity and sonic logging, with offset VSP results from 504B.

Correlation of core-derived lithology with surface seismic reflection data using normal incidence VSP data (Argo Abyssal Plain).

Correlation of Chlorine concentration (salinity), CaCO2 concentration from logging, normal incidence VSP profiles and surface seismic reflection for gas hydrate drilling on the Blake Ridge (ODP Leg 164).

SeisCORK Concept - for time lapse VSPs and offset VSPs - for monitoring micro- earthquake activity

Three basic styles of borehole geophysical measurements: 1) conventional well logging, 2) two-ship borehole experiments (such as offset VSP's that require the drill ship to be on site) 3) long-term borehole experiments (CORK's, strain installations, ION broadband seismometers, micro-earthquake monitoring, etc) acquiring data either autonomously or over cable networks (eg ORION).

Scientific Justification for Borehole Seismology Validating Surface Seismic - Scales of Observation Validating Surface Seismic - Interference and Multi-path Effects Extrapolating the Geological Structure Away from the Well Monitoring Cracking Fronts and Fluid Flow by Micro- and Nano- Earthquake Activity Monitoring Time-Dependent Effects

Some Typical and Proposed Borehole Seismic Experiments 1)Conventional Well-Logging and Normal Incidence VSP's 2)Two-ship Experiments and Offset VSP's 3)Time-lapse VSP's 4)Long-term Borehole Experiments and "Spin-off"Projects a) Monitoring and locating micro- and nano-earthquakes b) Cross-well tomography c) Broadband Seismometer Installations (ION)