Geoff Plastow talks about geophysical modelling and how to use geological inputs to help to constrain and improve our geophysical models using VOXI.
Overview
Speakers
Geoff Plastow
Senior Geophysicist – Seequent
Duration
12 min
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<v ->Hello, good morning, everyone.</v>
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It’s great to see everyone here at Lyceum 2019.
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My name is Geoff Plastow and I’m a Project Geophysicist
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based here in Vancouver.
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And throughout the course of the day,
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we are going to hold several tips and tricks sessions.
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So I’m excited to kick off our very first session.
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Okay, so this morning,
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I’m going to talk about geophysical modeling
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and how we can use geological inputs
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to help us constrain and improve our geo-physical models.
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This afternoon, my colleague Anna is going to be working
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in Leapfrog Geo,
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and she’s going to show a few tips and tricks
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on how to do quality control
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and how to better manage your drill holes.
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And later at the end of the day, my colleague,
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Sarah is going to be working in Leapfrog edge.
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And she’s going to show you some best practices
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regarding resource estimation.
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So when we were planning this event, we were thinking about,
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it’d be more interesting if we told a more compelling story.
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So throughout the course of the day,
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we are going to be working through what we called
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as mining value chain.
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We were working through exploration to resource evaluation.
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So this morning, my tips and tricks session is based
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in the top left-hand corner,
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where we are talking about prospecting,
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geophysical prospecting.
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We are boots on the ground and we’ve collected
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maybe a few holes.
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We’ve, collected three drill holes,
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and we’re going to look at some geo-physical models
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that we’ve created and ways that we can constrain it.
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Later in the day, my colleagues,
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Anna and Sarah are going to be working in Leapfrog Geo
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and Leapfrog age, Leapfrog edge
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a little further down in a mining chain.
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So this morning I’m going to be working in app.
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So it’s going to be exciting.
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Okay, so the first application I’m working in
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is called Central Browser.
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Central Browser allows you to connect
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to your central server.
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And what that allows you to do is to view and to manage
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the history of your geologic and earth models.
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So we can see on the left-hand side of the screen,
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we have a number of nodes and each one of these nodes
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represents an iteration of your model.
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And it’s great for a geophysicist like myself,
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because I can always go in and I can see how the model
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has evolved and progressed over time.
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And if I want, I can create my own branch
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to kind of keep my geo-physical models
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from interfering with other geological models.
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So if I click on this branch here, I can just pop it open.
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And my colleague Anna was great enough
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to create a little annotation.
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She says, Jeff, can you take a look at this?
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She’s drawn a straight plane through
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this massive sulfide body that started drilling,
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we’ve sunk three drill holes,
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and we’ve intercepted this massive sulfide twice.
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And she’s saying, Jeff,
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is it possible for you to incorporate any of this
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information into your geophysical modeling?
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Well, of course, that would be great.
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So the first thing I’m going to do
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is I’m just going to right click and export this
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export this geological model.
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And I’m just going to select the elements I’m going to export.
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So I’m exporting our MV volcanics, our LMS two,
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which is our sulfide body and the overburden.
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So I’m just going to export that,
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oops, okay.
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So once it’s been exported,
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I’m just going to jump into Oasis montaj.
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Now Oasis montaj is another desktop application
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that’s well known for the integration
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of all types of geoscience information.
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This includes geology, geophysics, geochemistry.
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In this case, we are really going to focus in on the geophysics
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and the geophysical modeling component of Oasis montaj.
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So to start off,
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I’m what we’re looking at is geophysical data
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that we’ve collected over the survey area,
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over the area of interest
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where we’ve already done some drilling,
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the data we’re looking at is magnetic data.
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So what we’ve done is we’ve collected
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total magnetic intensity.
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And what we’re looking at is areas in pink and red
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represent areas that are of high magnetic intensity
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and areas that are cooler in color
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in blue represent areas that have a low magnetic intensity.
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And I’ve just draped this over some topography
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and I’ve imported the drill holes
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that we have already looked at in the Central Browser.
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So the first thing I’m going to do now
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is now I’m just going to import our Leapfrog model.
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And I’m going to assign a projected coordinate system to it,
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just to ensure that everything lines up as it should.
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So the good news is that it imported
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and it looks exactly like it did in Leapfrog Geo,
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and also in the Central Browser.
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So I’m just going to turn off our volcanics
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so we can see our overburden here in this brown or orange.
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And we can see our green sulfide body here penetrated
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by two drill holes.
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Okay, well, this is exciting, what else can we do?
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So I’ve already performed an unconstrained
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geo-physical model.
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And what I’m going to do is I’m just going to visualize that now.
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So what do I mean when I say
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an unconstrained geophysical model,
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what I’ve done initially without any information
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is I’ve created a geo-physical model with no constraints.
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I’ve provided no geologic input.
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I’ve provided no geo-physical input and I’ve just created
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a model as a first pass.
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So let’s see what it looks like.
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So we can see some large pink blobs,
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which represent areas of high magnetic susceptibility.
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And I’m just going to slice through this box, a little bit.
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Okay, great.
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So we can see this large pink geophysical response
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of high magnetic susceptibility,
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more or less correlated with our sulfide mineralization.
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Okay, that’s great news.
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But the reality is we know that this mineralization
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does not extend all the way to the surface
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and the anomaly itself is rather blown out.
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Now, blown out is not a real technical term.
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I’m just saying that it is significantly larger
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and its physical extent is much larger
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than the mineralized body.
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We know that we can do a lot better.
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So why don’t we try to incorporate
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the geological information
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that I’ve just imported into Oasis montaj?
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So I’m going to open Voxler.
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Voxler is the geophysical modeling component
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inside of a Oasis montaj .
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And I have a model space here.
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This is just what we call a model mesh.
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And what I’m going to do now is build a very quick constraint
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from our Leapfrog model to do that.
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I can click constraints, create, build a model.
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So here I have the ability to assign physical rock
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properties to each one of the elements
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of the Leapfrog model.
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In this case, maybe we don’t have a great understanding
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of the magnetic susceptibility.
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So maybe we’re just going to use regional values
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or we’re going to maybe even use textbook values.
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So I’m, I can assign sub magnetic susceptibilities
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to our overburden layer
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and I can assign magnetic susceptibilities to our sulfides.
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I’m going to click, okay.
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Okay, so we’ve created our very first constraint
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from this Leapfrog model.
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We can see here in the blue,
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we see our overburden susceptibility
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and then we can see this susceptibility values
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that we’ve assigned for a massive sulfide body here in pink.
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Okay, great.
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So now we’ve at least provided some physical distribution
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of rock properties that can help us guide our inversion.
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So what I can do now is I can just click this green button
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and run the inversion.
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So the good news is I’ve already run the inversion.
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Voxler runs the inversion in the Cloud.
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It doesn’t use any of your computer resources.
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And in this case it took about an hour.
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So what I’m going to do now is I’m going to visualize
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both the constrained and unconstrained model.
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Okay, so we have our constrained inversion.
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So the model I just created on the right-hand side
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and on the left-hand side,
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we have our original unconstrained inversion.
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So what do we see between these two different earth models?
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So first off, right away, we can see this pink,
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highly susceptible content near surface.
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This is what we expected.
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We told the inversion that we have an overburden
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and we’ve assigned some magnetic susceptibility to it,
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that’s great.
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So now what happens if I spin the model around
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and begin to slice through it?
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So I’m slicing through our constrained inversion
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and we are looking in the area of where we’ve drilled
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and now we see a geo-physical anomaly
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that’s much more constrained.
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It’s much more in line and much more in line
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with our sulfide mineralization.
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The anomaly itself is a little bit larger
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than maybe what we expected,
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but this is pretty good for a first pass.
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So what I’m going to do is I’m just going to spin it around
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again here,
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and I’m just going to clip some of the data values to see,
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how well we recover the overburden and sulfide body.
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So we can see here in pink,
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we see that we’ve recovered more or less what we told it to.
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And we’ve now sort of limited the extent
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of our sulfide mineralization.
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Okay, well, this is great.
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How do I convey these results back to my colleague, Anna,
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who originally sort of created this model?
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I can simply just right click and I have a number of options
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to export and share this model.
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I can upload it to sequent view or I can export to OMF
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OMF stands for open mining format.
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If you want to know more about opening mining format,
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feel free to talk to any of our staff members
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during the solution kiosks.
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So once I export to OMF,
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I can jump back into the Central Browser
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and I can simply send a quick attachment to Anna.
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I can just say, here is a constrained model.
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Hopefully I type that correctly and I can attach to the OMF
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export and I can simply publish this model.
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And next time Anna’s back in the Central Browser,
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she can see that I’ve made an update and she can now begin
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to integrate these updated model into her geologic modeling.
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So to summarize this sort of tips and tricks
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that I’ve talked about this morning.
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The Central Browser is a great location for sharing
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and managing your geoscience data.
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Even geophysicists can go in there and export models.
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We can import these into Oasis montaj and they open
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just like, just like they look just like they do
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in Leapfrog.
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We can use these geologic inputs to constrain
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these geophysical inversions
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and produce much more realistic earth models.
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And then we can share them back with our colleagues
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and geologists and geoscientists
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who are using the Central Browser.
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And we can create a bit of a feedback loop
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and we can constantly update our geologic models
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and geophysical models working together.
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So this concludes my tips and tricks session.
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If you have any questions about anything I mentioned today,
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feel free to just talk to me during one of the breaks.
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Thank you.
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(crowd clapping)