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Imaging	with	sca-ered	teleseismic	waves:		
data,	method	and	applica7on	to		
the	Hellenic	subduc7on	zone		
F.D.	Pearce1	and	S.	Rondenay1	
1	Dept.	of	Earth,	Atmospheric,	
and	Planetary	Sciences,	MIT	
Frederick	D.	Pearce	 Modified	aKer	Project	MEDUSA	proposal
Subducted	
Crust	
Surface	
Seismics	
Seismic	images	of	lithosphere	and	upper-mantle	structure	
provide	key	constraints	on	large-scale	tectonic	processes	
Travel7me	
Tomography	
Mo7va7on	
Moho	
Teleseismic	
Migra7on	
40	km	
Frederick	D.	Pearce
Bostock	et	al.,	JGR	2001	
Teleseismic	migra7on	of	sca-ered	waves	
Objec7ve	
Frederick	D.	Pearce
Data	
Northern	Line	(NL)	
	*	71	events	
Southern	Line	(SL)	
	*	51	events	
SS	
NS	
CTF	
Frederick	D.	Pearce
Method	
Rondenay,	Survey	Geophysics	2009	
I)	Isolate	sca-ered	teleseismic	body	waves	
0	
50	
0	
50	
0	
50	
0	
50	
0	
50	
Time	[sec]	
1)	Align	wavefields	
2)	Isolate	incident	P	
3)	Isolate	sca-ered	
				P,	SV,	and	SH	
Frederick	D.	Pearce
Method	
II)	Apply	teleseismic	migra7on	algorithm	
P	
*	Propaga7on	within	a	1D	background	model	
*	2D	Generalized	Radon	transform	inversion	Frederick	D.	Pearce	
Rondenay,	Survey	Geophysics	2009
XSL	[km]	
Depth	[km]	
SL	Imaging*	
Δβ = +/- 5% 	Δα = +/- 10% 	
XSL	[km]	
Frederick	D.	Pearce	 *	Early	version	of	images,	see	final	in	Pearce	et	al.,	JGR	2012
XSL	[km]	
Depth	[km]	
SL	Imaging*	
P	S	
XSL	[km]	
P	P	S	
P	S	Sv	 P	S	Sh	
Frederick	D.	Pearce	 *	Early	version	of	images,	see	final	in	Pearce	et	al.,	JGR	2012
SL	Lateral	Varia7ons*	
Depth	[km]	
1T	
3T	
2T	
2T	
XSL	[km]	
Frederick	D.	Pearce	 *	Early	version	of	images,	see	final	in	Pearce	et	al.,	JGR	2012
XSL	[km]	
Depth	[km]	
SL	Imaging*	
Subducted	
Crust	
Con3nental	
Moho	
Eclogi3za3on	
Oceanic	
Moho	
Δβ	from	-5%	(red)	to	5%	(blue)	
Frederick	D.	Pearce	 *	Early	version	of	image,	see	final	in	Pearce	et	al.,	JGR	2012
NL	Imaging*	
XNL	[km]	
Depth	[km]	
Δβ	from	-5%	(red)	to	5%	(blue)	
Subducted	
Crust	
Con3nental	
Moho	
Frederick	D.	Pearce	 *	Early	version	of	image,	see	final	in	Pearce	et	al.,	JGR	2012
Results:	NL	vs.	SL*	
Moho	Contour	Map	
CROP	Project	
Finee,	2005	
XST	
Frederick	D.	Pearce	 *	Early	version	of	schema7c,	see	final	in	Pearce	et	al.,	JGR	2012
Conclusions	
Teleseismic	migra7on	provides	high-resolu7on	images		
of	lithosphere	and	upper-mantle	structure	
Images	from	the	western	Hellenic	subduc7on	zone	show	
	*	oceanic	crust	beneath	southern	segment	
	*	con3nental	crust	beneath	northern	segment	
	*	differen7al	rollback	between	SS	and	NS	
Frederick	D.	Pearce

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