elastic 2d modeling of seismic surveysof seismic surveys · elastic 2d modeling of seismic...

Elastic 2D Modeling of Seismic Surveysof Seismic Surveys

Joe WongJoe Wong Peter Manning

Dave HenleyDave Henley

mFD2D - MATLAB software :

Designed for easy use;Models fairly complex geological structure;f y p g g ;Output data written to SEG-Y files.

Produce realistic-looking synthetic data for :g y f

Reflection RefractionRefraction VSP MicroseismicMicroseismic CrosswellTime LapseTime Lapse

Source Wavelets

Δx = Δz = 2.5 meters Δ 00025 dΔt =.00025 seconds

Vertical Comp.

R di l CRadial Comp.

Non-reflecting Surface

Free SurfaceFree Surface

Dyke –Fault Modely

Anticline Model

Fault-Fold Model

F l b d F l i D hFault bendfold

Fault propagationfold

Detachmentfold

Box foldPop-up

Duplex

STRUCTURES WEO G

Box fold

WANT TO IMAGEAntiformal stack

D. Spratt

Time Lapse Example

Finite Difference 2D Elastic Modeling

BEFORE:TARGET HAS HOSTTARGET HAS HOST ROCK PROPERTIES.

AFTER:10% DROP IN10% DROP IN TARGET PROPERTIES.

Baseline ModelBaseline Model

Monitor ModelMonitor Model

Baseline

Vertical Component

MonitorMonitor

Vertical Component DifferenceVertical Component Difference

Baseline

Radial Component

MonitorMonitor

Radial Component DifferenceRadial Component Difference

Relative Execution SpeedRelative Execution Speed

>> feature jit off>> feature jit off

MATLAB 2009a jit on 49 sec 1MATLAB 2009a jit on 49 sec 1MATLAB 2009a jit off 178 sec 3.6 MATLAB 2010b jit off 120 sec 2 4MATLAB 2010b jit off 120 sec 2.4MATLAB 2010b jit on 525 sec 10.7

Execution Time

Model size : 800 by 400 pixelsTime Steps : 4000No. of Shots : 100Run Time: 15 hours

Multi-processor operation :

Start 3 separate MATLAB windows.In each window run mFD2D from differentIn each window, run mFD2D from different folder names. In each window run same model withIn each window, run same model withinter-leaved shot points, orIn each window run a different modelIn each window, run a different model.

Wish List EnhancementsWish List Enhancements :

CPML d d fl tiCPML - decrease edge reflections ;Attenuation – seismic Q ;V l it A i t VTI/TTIVelocity Anisotropy - VTI/TTI ;Variable grid size ;R ti i ti (???)Reverse-time migration (???).

k l dAcknowledgement

This research was supported by NSERC d h i d i l f CREWSand the industrial sponsors of CREWS.