Japanese WESTPAC Symposium. June 6-7, 1989. Ocean Research Institute, University of Tokyo. 西太平洋におけるマイクロプレートテクトニクスと古環境地図に関する研究会. 1989年6月6日-7日. 東京大学海洋研究所.The eastern part of the Asian continent was intensively deformed in the early Cretaceous time. Deformation has been interpreted to be related to subduction tectonics along the eastern continental margin. We propose an alternative tectonic framwork of collision-extrusion tectonics resulting from collision of the Indosinian block with the Eurasian continent. This event controlled the Jurassic to Cretaceous tectonic history in eastern Asia and evolution of the subduction zone along the eastern margin of the continent
recognition of Phanerozoic subduction systems and two continental fragments of Gondwana-land which e...
International audienceThe Mesozoic geodynamic evolution of Transbaikalia has been largely controlled...
Abstract. The respective tectonic effects of back arc spreading and continental collision in Asia ar...
change in boundary condition along the eastern margin of Asia that allowed the thickened Asian conti...
East Asia is a region of widespread deformation, dominated by normal and strike-slip faults. Deform...
Present-day Asia comprises a heterogeneous collage of continental blocks, derived from the Indian-we...
International audienceStructural studies of three representative objects in eastern Mongolia outline...
Abstract: Continental SE Asia is the site of an extensive Cretaceous–Paleocene regional uncon-formit...
International audienceThe deformation of the eastern Asian lithosphere during the first part of the ...
Several orogenic belts transecting south-eastern Asia are the sites of former convergent plate margi...
Abstract: SE Asia comprises a collage of continental terranes derived directly or indirectly from th...
application/pdfMesozoic through Cenozoic magmatic evolution of East Asia was governed by oceanic pla...
The present paper considers the research of the Cretaceous-Cenozoic rifting for the Eastern margin o...
The belt boundary thrust within the Cretaceous–Neogene accretionary complex of the Shimanto Belt, so...
The India-Asia collision has formed the highest mountains on Earth and is thought to account for ext...
recognition of Phanerozoic subduction systems and two continental fragments of Gondwana-land which e...
International audienceThe Mesozoic geodynamic evolution of Transbaikalia has been largely controlled...
Abstract. The respective tectonic effects of back arc spreading and continental collision in Asia ar...
change in boundary condition along the eastern margin of Asia that allowed the thickened Asian conti...
East Asia is a region of widespread deformation, dominated by normal and strike-slip faults. Deform...
Present-day Asia comprises a heterogeneous collage of continental blocks, derived from the Indian-we...
International audienceStructural studies of three representative objects in eastern Mongolia outline...
Abstract: Continental SE Asia is the site of an extensive Cretaceous–Paleocene regional uncon-formit...
International audienceThe deformation of the eastern Asian lithosphere during the first part of the ...
Several orogenic belts transecting south-eastern Asia are the sites of former convergent plate margi...
Abstract: SE Asia comprises a collage of continental terranes derived directly or indirectly from th...
application/pdfMesozoic through Cenozoic magmatic evolution of East Asia was governed by oceanic pla...
The present paper considers the research of the Cretaceous-Cenozoic rifting for the Eastern margin o...
The belt boundary thrust within the Cretaceous–Neogene accretionary complex of the Shimanto Belt, so...
The India-Asia collision has formed the highest mountains on Earth and is thought to account for ext...
recognition of Phanerozoic subduction systems and two continental fragments of Gondwana-land which e...
International audienceThe Mesozoic geodynamic evolution of Transbaikalia has been largely controlled...
Abstract. The respective tectonic effects of back arc spreading and continental collision in Asia ar...