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Introduction to Geophysics Ali Oncel [email protected] Department of Earth Sciences KFUPM Refraction Interpretation-2 Introduction to Geophysics-KFUPM

Refraction Interpretation-2

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Page 1: Refraction Interpretation-2

Introduction to Geophysics

Ali [email protected]

Department of Earth SciencesKFUPM

Refraction Interpretation-2

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM

Page 2: Refraction Interpretation-2

Previous Lecture

Refraction Seismology ObjectiveInterpretation ModelsQuiz

Page 3: Refraction Interpretation-2

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM Interpretation Models

Figure 4.3 of Lillie

Page 4: Refraction Interpretation-2

Single Horizontal Interface in kmIn

trod

ucti

on t

o Ge

ophy

sics

-KFU

PM

Fig. 4.4 of Lillie

t1 Delayed Time

100-150km <Spread Length< 300-600km

Oceans Continental1

1

2

Vc

Cosht

θ=

CCosh

Vtθ211=

Inversion equations

12

2112 VV

VVhxcr −

+=

Forward equations

Page 5: Refraction Interpretation-2

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM Single Horizontal Interface in meter

Fig. 4.5 of Lillie

11

2

Vc

Cosht

θ=

CCosh

Vtθ211=

Inversion equations

12

2112 VV

VVhxcr −

+=

Forward equations

Page 6: Refraction Interpretation-2

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM Several Horizontal Interfaces

Page 7: Refraction Interpretation-2

Generalized Refraction ModelIn

trod

ucti

on t

o Ge

ophy

sics

-KFU

PM

111

,2

Vni

Cosht

in

in

θ∑

=− =

Fig. 4.7 of Lillie

The above model is valid as long as velocity does not decreased with depth.

Page 8: Refraction Interpretation-2

Refraction: Example from Ocean Basin

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM

Fig. 4.8 of Lillie, modified after Sheriff and Geldart, 1995.

Page 9: Refraction Interpretation-2

Refraction: Oceanic Crust

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM

Where do you know about the well-known examples of Oceanic Crust?

Layer 1: Deep-sea sedimentsLayer 2: Basalt (Volcanics and shallow intrusions)Layer 3: Gabbro (Deeper Intrusions)Layer 4: Peridodite (Uppermost refraction; gives Moho refraction)

Page 10: Refraction Interpretation-2

Mid

-Atla

ntic

R

idge

Eas

t P

acif

ic

Ris

e

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM

Parks and Plates©2005 Robert J. Lillie

Page 11: Refraction Interpretation-2

Formation of Oceanic CrustIn

trod

ucti

on t

o Ge

ophy

sics

-KFU

PM

Parks and Plates©2005 Robert J. Lillie

Page 12: Refraction Interpretation-2

Formation of Oceanic CrustIn

trod

ucti

on t

o Ge

ophy

sics

-KFU

PM

Parks and Plates©2005 Robert J. Lillie

Page 13: Refraction Interpretation-2

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM Formation of Oceanic Crust

Parks and Plates©2005 Robert J. Lillie

Page 14: Refraction Interpretation-2

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM Formation of Oceanic Crust

Parks and Plates©2005 Robert J. Lillie

Page 15: Refraction Interpretation-2

Intr

oduc

tion

to

Geop

hysi

cs-K

FUPM Formation of Oceanic Crust

Parks and Plates©2005 Robert J. Lillie

Page 16: Refraction Interpretation-2

Parks and Plates©2005 Robert J. Lillie

Page 17: Refraction Interpretation-2

Field Trip: KFUPM BEACH

Schedule: March 29 (or 27?) before Mid-Term Break

Leaving from: 12:30 from KFUPM

The purpose: Measurements of Refraction and Gravity

Any questions or suggestions.