The lithospheric structure in Central Asia features large blocks such as the Indian plate, the Afghan block, the Turan plate, and the Tarim block. This geologically and tectonically complicated area is also one of the most seismically active regions in the world. We developed P- and S-wave velocity structures of Central Asia in the crust using th
Ample geologic and geophysical data provide the basis for distinguishing the 102–104° E geodivider i...
The Central Eurasia region hosts wide deforming areas, with diffused or localized deformation occurr...
In this study, we explore the neotectonic deformation in the whole Central Eurasia, including both t...
north Eurasian lithosphere plate separated from neighboring plates by some transit zones. These zone...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1981.M...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1979.M...
The article describes the history, the staff, researches and scientific activities of the Laboratory...
Altaids in the Central Asian Orogenic Belt (CAOB) is one of the world’s largest orogenic belts conta...
The Paleozoic mosaic-block structure of the Central Asia folded area is formed by isometrically outl...
has produced a vast system of folds and faults, many of which are active today, as evidenced by such...
Altaids in the Central Asian Orogenic Belt (CAOB) is one of the world’s largest orogenic belts conta...
Altaids in the Central Asian Orogenic Belt (CAOB) is one of the world’s largest orogenic belts conta...
Three seismic activity maps, the A-value map, the b-value map and the return-period map for earthqua...
The Tien Shan in central Asia is the world’s largest and most active intracontinental orogen, with a...
We introduce a new hypothesis to explain the unusual pattern of intermediate-depth earthquakes in th...
Ample geologic and geophysical data provide the basis for distinguishing the 102–104° E geodivider i...
The Central Eurasia region hosts wide deforming areas, with diffused or localized deformation occurr...
In this study, we explore the neotectonic deformation in the whole Central Eurasia, including both t...
north Eurasian lithosphere plate separated from neighboring plates by some transit zones. These zone...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1981.M...
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1979.M...
The article describes the history, the staff, researches and scientific activities of the Laboratory...
Altaids in the Central Asian Orogenic Belt (CAOB) is one of the world’s largest orogenic belts conta...
The Paleozoic mosaic-block structure of the Central Asia folded area is formed by isometrically outl...
has produced a vast system of folds and faults, many of which are active today, as evidenced by such...
Altaids in the Central Asian Orogenic Belt (CAOB) is one of the world’s largest orogenic belts conta...
Altaids in the Central Asian Orogenic Belt (CAOB) is one of the world’s largest orogenic belts conta...
Three seismic activity maps, the A-value map, the b-value map and the return-period map for earthqua...
The Tien Shan in central Asia is the world’s largest and most active intracontinental orogen, with a...
We introduce a new hypothesis to explain the unusual pattern of intermediate-depth earthquakes in th...
Ample geologic and geophysical data provide the basis for distinguishing the 102–104° E geodivider i...
The Central Eurasia region hosts wide deforming areas, with diffused or localized deformation occurr...
In this study, we explore the neotectonic deformation in the whole Central Eurasia, including both t...