Seismic-Well Tie Flow-Chart

Slides:



Advertisements
Similar presentations
Well-Seismic Ties Lecture 7 Depth Time Synthetic Trace SLIDE 1
Advertisements

Wedge Modeling HRS-9 Hampson-Russell Software
WAVELET PHASE ESTIMATION WITHOUT ACCURATE TIME-DEPTH CONVERSION JIANGBO YU ADVISOR: DR. JOHN CASTAGNA AGL UPDATE MEETING MAY 2, 2012.
Copyright © NORSAR 2005 Advanced Applications of NORSAR-3D Ray Modelling.
Establishing Well to Seismic Tie
Youli Quan & Jerry M. Harris
REFLECTIONS, ROTATIONS AND TRANSLATIONS. Reflections.
MD + AVO Inversion Jianhua Yu, University of Utah Jianxing Hu GXT.
Seismic is not too complex for geologists - If you can understand convolution, you have it made. Simply stated, when downward traveling waves pass by a.
Geology 5660/6660 Applied Geophysics 24 Feb 2014 © A.R. Lowry 2014 For Wed 26 Feb: Burger (§8.4) Last Time: Industry Seismic Interpretation Well.
Synthetic Seismogram Objectives
Seismic Imaging in GLOBE Claritas
SEISMIC INTERPRETATION
Course 6: Analyzing AVO/AVA Analysis. Use gassman’s equations to predict velocity Objective accurately predict changes in amplitude.
Data QC and filtering Bryce HutchinsonSumit Verma Objective: Consider the frequency range of different seismic features Look for low frequency and high.
Super-virtual Interferometric Diffractions as Guide Stars Wei Dai 1, Tong Fei 2, Yi Luo 2 and Gerard T. Schuster 1 1 KAUST 2 Saudi Aramco Feb 9, 2012.
Info Read SEGY Wavelet estimation New Project Correlate near offset far offset Display Well Tie Elog Strata Geoview Hampson-Russell References Create New.
MD+AVO Inversion: Real Examples University of Utah Jianhua Yu.
Drilling & Measurements (D&M)
Small scale reflection seismology
Applied Geophysics Fall 2016 Umass Lowell
Raw Seismic Data For the explosion we just considered ...
Progradational Internal Configurations
I. Tutorial: ISS imaging
Modeling of free-surface multiples - 2
AVO inversion of multi-component data for P and S impedance
Fang Liu, Arthur B. Weglein, Kristopher A. Innanen, Bogdan G. Nita
Acoustic Structure of the Earth
Sonic (Velocity) Logs Sonic (DT)
Free Surface Multiple Elimination
Seismic Processing Data Processing Stream Field Record (marine)
DHIs: Amplitude Anomalies
Acoustic Reflection 2 (distance) = (velocity) (time) *
Thin beds have almost no impact due to destructive interference
Seismic Interpretation
The Wave Equation Modeled
Objectives of Well-Seismic Ties
Seismic - Units 10s of Meters Thick
The Convolution Method
Purposes for Well-Seismic Ties & Quality
Migration – Correcting for Location
Summary: Lateral Resolution
Thud! Ring! Seismic Response What causes a seismic response?
From Raw Data to an Image
A Predicted Porosity Map
The STRENGTHS of Seismic Data
Comparison of Seismic and Well Data
Well Measurements: Wire-line Logs
Causal (real – no motion before wave arrives) Front loaded
Measurements In Time and In Depth
Typical Vertical Resolution
Local Data - Subsurface
A Prospect A prospect is a location and depth that has been identified as a good place to drill for oil and/or gas For us to find oil or gas, certain conditions.
Passive seismic imaging
Shot Gather For Shot 1 Source Receivers R1 R2 R3 R4 R5 S1
Seismic Facies Mapping Exercise
Raw Data - Marine SLIDE 6 Here is a display of raw seismic data – what would be recorded for one shot/explosion (marine example) The horizontal scale is.
Vertical Resolution Gamma Ray
Modeling the seismic response:
With Correct Velocity, Gather is Flat
Fault Identification: Time Slice View
The Ideal Seismic Response
DHIs: Fluid Contacts Hydrocarbons are lighter than water and tend to form flat events at the gas/oil contact and the oil/water contact. Thicker Reservoir.
Good Migration Enhances Resolution
From Raw Data to an Image
Seismic Reflections Lecture Shot Receiver Seismic Record
АВЛИГАТАЙ ТЭМЦЭХ ҮНДЭСНИЙ ХӨТӨЛБӨР /танилцуулга/
Limited to Mapped Horizons Regular Intervals as Defined by the User
EXPLORATION GEOPHYSICS
Packing of uniform spheres
Presentation transcript:

Seismic-Well Tie Flow-Chart Data Data Processing Real Seismic Trace Estimate Pulse SLIDE 7 Here is a simple flow chart for performing a:well-seismic tie At the top is our seismic data – the raw field data is processed to get us images of the subsurface The processed data gives us a “real” seismic trace at the location of the well we want to tie As part of the data processing, we can get an estimate of the shape of the seismic pulse Near the bottom is the well data, which may need some processing/editing The well data we need come from the sonic log (gives us velocity information) and one of several density logs We may also have check shots from the well – more on check shots on the next slide If we do not have an estimated pulse from the seismic data processing, we can use a standard (external) pulse shape of a user-defined phase and frequency Computer programs combine the sonic and density log data with the estimated or external pulse to generate a “synthetic” or “modeled” seismic trace We then compare the real and synthetic traces and note how well they match If the match is good enough for our purposes, we can then relate one data set to the other – well to seismic OR seismic to well External Pulse Well - Seismic Tie Well - Seismic Tie Well Data Data Processing Seismic Modeling Synthetic Seismic Trace Check Shots/ Time Depth Information Courtesy of ExxonMobil L 7 – Well-Seismic 1