A model of the crust and mantle structure down to 700km depth beneath the lhasa to golmud transect across the tibetan plateau as derived from seismological data

Tectonophysics

Volumn 606, Issue , 2013, Pages 187-197

  Mechie, J ^a   Kind, R ^a  

^a GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

Author keywords

Crustal structure; Mantle structure; Mantle transition zone; Tibet

Indexed keywords

CRUSTAL STRUCTURE; ISO-STATIC SUPPORTS; LITHOSPHERIC MANTLE; MANTLE STRUCTURE; MANTLE TRANSITION ZONE; SEISMIC VELOCITIES; SEISMOLOGICAL DATA; TIBET;

SEISMIC WAVES; TECTONICS; VELOCITY;

STRUCTURAL GEOLOGY;

CRUSTAL STRUCTURE; CRUSTAL THICKNESS; DISCONTINUITY; LOWER CRUST; MANTLE STRUCTURE; MOHO; SEISMIC VELOCITY; SEISMOLOGY; TERRANE; TRANSITION ZONE; UPPER MANTLE;

CHINA; GOLMUD; KUNLUN MOUNTAINS; LHASA; QAIDAM BASIN; QINGHAI; QINGHAI-XIZANG PLATEAU; XIZANG;

EID: 84885310772     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2013.04.030     Document Type: Article

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