Central China orogenic belt and amalgamation of East Asian continents
Abstract The Central China Orogenic Belt (CCOB) comprises, from the east to the west, the
Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important …
Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important …
Multiple Tethyan ocean basins and orogenic belts in Asia
I Metcalfe - Gondwana Research, 2021 - Elsevier
Four Tethyan ocean basins are recognised in Asia, the Proto-Tethys (Late Proterozoic-
Silurian), Palaeo-Tethys (Middle Devonian-Late Triassic), Meso-Tethys (Middle Permian …
Silurian), Palaeo-Tethys (Middle Devonian-Late Triassic), Meso-Tethys (Middle Permian …
Exploring a lost ocean in the Tibetan Plateau: Birth, growth, and demise of the Bangong-Nujiang Ocean
The vast eastern-Tethyan oceanic domain that throughout the Mesozoic extended between
Gondwana and Eurasia was a puzzle of larger and smaller microcontinents separated by …
Gondwana and Eurasia was a puzzle of larger and smaller microcontinents separated by …
Active seismotectonics of the East Anatolian fault
SUMMARY The East Anatolian Fault (EAF) is a 700-km-long left-lateral transform fault
located between the Anatolian and Arabian plates. The proximity of the Euler Pole to the …
located between the Anatolian and Arabian plates. The proximity of the Euler Pole to the …
Subduction and accretionary tectonics of the East Kunlun orogen, western segment of the Central China Orogenic System
Y Dong, D He, S Sun, X Liu, X Zhou, F Zhang… - Earth-Science …, 2018 - Elsevier
Abstract The Kunlun Orogen is generally divided into the East Kunlun Orogenic Belt (E-KOB)
and the West Kunlun Orogenic Belt (W-KOB) by the Altyn Tagh fault. The E-KOB forms part …
and the West Kunlun Orogenic Belt (W-KOB) by the Altyn Tagh fault. The E-KOB forms part …
Tectonic evolution and geodynamics of the Neo-Tethys Ocean
Abstract The Neo-Tethys Ocean was an eastward-ga** triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …
Active fault database of Turkey
We have updated the active fault map of Turkey and built its database within GIS
environment. In the study, four distinct active fault types, classified according to …
environment. In the study, four distinct active fault types, classified according to …
Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction
Integration of lithostratigraphic, magmatic, and metamorphic data from the Lhasa–Qiangtang
collision zone in central Tibet (including the Bangong suture zone and adjacent regions of …
collision zone in central Tibet (including the Bangong suture zone and adjacent regions of …
Closure of the East Paleotethyan Ocean and amalgamation of the Eastern Cimmerian and Southeast Asia continental fragments
Abstract The Phanerozoic record of Southeast Asia preserves the history of opening and
subsequent consumption of the Paleotethyan Ocean and the assembly of continental …
subsequent consumption of the Paleotethyan Ocean and the assembly of continental …
Tectonic units of the Alpine collision zone between Eastern Alps and western Turkey
We present a map that correlates tectonic units between Alps and western Turkey
accompanied by a text providing access to literature data, explaining the concepts used for …
accompanied by a text providing access to literature data, explaining the concepts used for …