Docsity
Docsity

Prepare for your exams
Prepare for your exams

Study with the several resources on Docsity


Earn points to download
Earn points to download

Earn points by helping other students or get them with a premium plan


Guidelines and tips
Guidelines and tips

Interpretation of geological features, Lecture notes of Engineering Geology

Seismic is the best techniques for oil and gas exploration.

Typology: Lecture notes

2018/2019

Uploaded on 10/28/2019

vivek-aryan
vivek-aryan 🇮🇳

1 document

1 / 52

Toggle sidebar

This page cannot be seen from the preview

Don't miss anything!

bg1
Seismology and the Earth’s Deep Interior Seismogram Interpretation
Seismogram Interpretation
Seismogram Interpretation
Travel times in the Earth
Ray paths, phases and their name
Wavefields in the Earth: SH waves, P-SV waves
Seismic Tomography
Receiver Functions
pf3
pf4
pf5
pf8
pf9
pfa
pfd
pfe
pff
pf12
pf13
pf14
pf15
pf16
pf17
pf18
pf19
pf1a
pf1b
pf1c
pf1d
pf1e
pf1f
pf20
pf21
pf22
pf23
pf24
pf25
pf26
pf27
pf28
pf29
pf2a
pf2b
pf2c
pf2d
pf2e
pf2f
pf30
pf31
pf32
pf33
pf34

Partial preview of the text

Download Interpretation of geological features and more Lecture notes Engineering Geology in PDF only on Docsity!

Seismogram Interpretation Seismogram Interpretation

• Travel times in the Earth

• Ray paths, phases and their name

• Wavefields in the Earth: SH waves, P-SV waves

• Seismic Tomography

• Receiver Functions

Seismogram Example Seismogram Example

4400s

Long-period transverse

displacement for an

earthquake at 600km

depth recorded at 130o

(synthetic).

How can we extract

information from

seismograms on Earth

structure?

-> identify phases

-> pick travel times

-> collect travel times

as

a function of distance

History of Travel-Times History of Travel-Times

  • (^) Harrold Jeffreys and Keith Bullen (1940), (J-B) Remarkable accuracy for teleseismic travel times (below 1%)!
  • Herrin et al. (1968), with well located earthquakes.
  • (^) Dziewonski and Anderson (1981), Preliminary Reference Earth Model (PREM)
  • (^) Kennett and Engdahl (1991), most accurate radially symmetric model (iasp91)
  • (^) (2000), The first 3-D reference model with travel times?

Ray Paths in the Earth (1) Ray Paths in the Earth (1)

Particular phases at teleseismic distances are named after the wave types (P or S), regions they pass along their path, and emergence angle at the source (upwards or downwards).

Ray Paths in the Earth - Names Ray Paths in the Earth - Names

P P waves

S S waves

small p depth phases (P)

small s depth phases (S)

c Reflection from CMB

K wave inside core

i Reflection from Inner core

boundary

I wave through inner core

diff diffractions at CMB

Examples:

PcP, pPcS, SKS, PKKKP, PKiKP, PKIKP, sSS, pSSS,

sPcS, etc.

Wavefields in the Earth: SH waves Wavefields in the Earth: SH waves

Red and yellow

color denote

positive and

negative

displacement,

respectively.

Wavefield for

earthquake at

600km depth.

Wavefields in the Earth: SH waves Wavefields in the Earth: SH waves

Red and yellow

color denote

positive and

negative

displacement,

respectively.

Wavefield for

earthquake at

600km depth.

Wavefields in the Earth: SH waves Wavefields in the Earth: SH waves

Red and yellow

color denote

positive and

negative

displacement,

respectively.

Wavefield for

earthquake at

600km depth.

Wavefields in the Earth: P-SV waves Wavefields in the Earth: P-SV waves

Red and yellow color denote positive and negative vertical displacement, respectively. Left: homogeneous mantle, right: realistic spherically symmetric model (Preliminary Reference Earth Model, PREM ) Wavefield for explosion at 600km depth.

Wavefields in the Earth: P-SV waves Wavefields in the Earth: P-SV waves

Red and yellow color denote positive and negative vertical displacement, respectively. Left: homogeneous mantle, right: realistic spherically symmetric model (Preliminary Reference Earth Model, PREM ) Wavefield for explosion at 600km depth.

Wavefields in the whole Earth: P waves Wavefields in the whole Earth: P waves

Red and blue colors denote positive and negative vertical displacement, respectively. Spherically symmetric model (Preliminary Reference Earth Model, PREM ) Wavefield for explosion at surface. Time: 150s

Wavefields in the whole Earth: P waves Wavefields in the whole Earth: P waves

Red and blue colors denote positive and negative vertical displacement, respectively. Spherically symmetric model (Preliminary Reference Earth Model, PREM ) Wavefield for explosion at surface. Time: 450s

Wavefields in the whole Earth: P waves Wavefields in the whole Earth: P waves

Red and blue colors denote positive and negative vertical displacement, respectively. Spherically symmetric model (Preliminary Reference Earth Model, PREM ) Wavefield for explosion at surface. Time: 1050s

Wavefields in the whole Earth: P waves Wavefields in the whole Earth: P waves

Red and blue colors denote positive and negative vertical displacement, respectively. Spherically symmetric model (Preliminary Reference Earth Model, PREM ) Wavefield for explosion at surface. Time: 1350s