Deep Structure of the Northeastern Tibet Collision Zone
Nickname
INDEPTHIV
Format
SEGY
Type
PASSCAL
Start year
2007
End Year
2007
Description
An extension of INDEPTH-III. Testing bypotheses for the uplift of northern Tibet - 1)imbricating of Asian crust while the Asian contiental lithosphere is being detached and "subducted" into the Tibetan mantle; 2)delaminating of a thickened Tibetan lithosphere, and 3) asthenospheric counterflow associated with subduction of Indian contienental lithosphere. Fieldwork to operate concurrently with INDEPTH 4 broadband experiment
EarthScope Consortium operates the NSF National Geophysical Facility (NSF NGF).
Any opinions, findings and conclusions, or recommendations expressed in this
material do not necessarily reflect the views of the U.S. National Science
Foundation.
NSF SAGE Facility has been
certified as a trustworthy data repository
by the CoreTrustSeal Standards and Certification Board
