Three-dimensional Moho topography beneath the Tibetan Plateau determined by Γxy, Γxz and Γyz of GOCE gravity gradients

Author:

Xu Chuang,Jian Guangyu,Cui Lilu

Funder

Natural Science Foundation of Guangdong Province

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference39 articles.

1. On the computations of the effect of the attraction of the mountain masses as disturbing the apparent astronomical latitude of stations in geodetic surveys;Airy;Trans. Royal Society (London), Series B,1855

2. Gravity inversion in Qinghai-Tibet Plateau;Braitenberg;Phys. Chem. Earth (A),2000

3. The gravity and isostatic Moho undulations in Qinghai-Tibet plateau;Braitenberg;J. Geodyn.,2000

4. Topographic ooze: Building the eastern margin of Tibet by lower crustal flow;Clark;Geology,2000

5. An approach to Moho discontinuity recovery from on-orbit GOCE data with application over Indo-Pak region;Eshagh;Tectonophysics,2016

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