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Gravity Anomaly - Seismology - Lecture Slides, Slides of Geology

In these Lecture Slides, the Lecturer has tried to illustrate the following key points : Gravity, Rocks, Gravity’S Effects, Downward Acceleration, Change With Location, Experience, Gravitational Forces, Information, Gravity Surveying, Projectiles

Typology: Slides

2012/2013

Uploaded on 07/19/2013

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Gravity Anomaly Due to Buried Sphere
The gravity anomaly due to a buried sphere is straightforward
We’ll start by assuming the sphere is a point source
x = 0 x
θ
2
z
m
Gg
vert
=
δ
θδ
cos
2
r
m
Gg
vert
=
Directly over the sphere (r = z) all of
the additional acceleration is vertical
and given by the relationship derived
earlier.
At some location, x, away from the sphere,
only part of the acceleration is vertical and
the vertical component is found by
trigonometry.
vertnet
gg
δδ
=
net
g
δ
vert
g
δ
z = r zr
horiz
g
δ
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Gravity Anomaly Due to Buried Sphere

  • The gravity anomaly due to a buried sphere is straightforward
  • We’ll start by assuming the sphere is a point source

x = 0

x

θ

2 z

m g (^) vert G

δ = δ^2 cos^ θ

r

m g (^) vert G

Directly over the sphere (r = z) all of

the additional acceleration is vertical

and given by the relationship derived

earlier.

At some location, x, away from the sphere,

only part of the acceleration is vertical and

the vertical component is found by

trigonometry.

δ gnet = δ g vert

δ gnet

z = r z r δ g vert

δ g horiz

Gravity Anomaly Due to Buried Sphere

  • Now lets put the equation into a more useful form…

It is not convenient to calculate θ, so

we can reformulate the equation in

terms that are more convenient.

r

z

cosθ = ( )

2 2 1 /^2 r = x + z

x

z r^ θ

Now plug these back into the previous

equation…

δ cos θ

2 r

m g (^) vert G

3 r

mz g (^) vert G

δ =

Subs in cos θ…

Subs in r = …

2 2 3 /^2 x z

mz g (^) vert G

δ =

But this is based on a mass change of a

point source. Sub in the mass change of

a sphere with radius = R and density

contrast Δρ

2 2 3 /^2

3

3

x z

G R z

g (^) sphere

∆ m =^ ( Vol^ )(^ ∆ρ)

Other Gravity Anomalies

  • Spherical targets :: diapirs and/or plutons
  • Cylindrical targets :: tunnels/caves
    • Note that all anomalies lack a sharp edge
    • Subsurface geometry is non-unique

Other Gravity Anomalies

  • Sheets :: dikes, veins
  • Anomaly shape

depends on

  • Density contrast
  • Depth
  • Length of sheet
  • Dip of the sheet