The geological terranes on the Indian subcontinent and Tibetan plateau are structurally and chronologically diverse. In this study, a nonlinear inversion is performed to estimate the Moho depths using
The three-dimensional magnetic structure of the Yangtze River basin was determined using three-dimensional oblique magnetization regularization inversion with high-precision total magnetic anomalies.
This data set presents the velocity model interfaces. The velocity models were constrained by traveltime tomography of active-source Ocean Bottom Seismometers data along three profiles from the Easter
This paper presents the results of an extensive structural investigation of the western part of the Sava Depression (SW part of the Pannonian Basin System) and provides insights in the tectonic evolut
