Images of possible fossil collision structures beneath the Eastern Ghats belt, India, from P and S receiver functions

The Proterozoic Eastern Ghats belt of India is often believed to be the ancient analogue of the present-day Himalayas. However, geological and geophysical signatures that can be traced and linked to the Eastern Ghats belt orogen due to a Precambrian collisional episode are sparse and evidence of suc...

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Veröffentlicht in:	Lithosphere 2010-04, Vol.2 (2), p.84-92
Hauptverfasser:	Ramesh, D. S, Bianchi, M. B, Das Sharma, S
Format:	Artikel
Sprache:	eng
Schlagworte:	Asia body waves deep-seated structures depth Dharwar Craton Eastern Ghats elastic waves Geophysics Ghats India Indian Peninsula lithosphere P-waves Paleozoic plate collision plate tectonics Precambrian Proterozoic receiver functions S-waves seismic waves solid Earth (tectonophysics) thickness upper Precambrian velocity structure
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