A new concept of continental construction based on four main terms: (1) crustal growth, (2) crustal formation, (3) continental growth and (4) continental formation is presented here. Each of these terms reflects a certain process responsible for the formation of what we call now "continental crust". This concept is applied to the Central Asian Orogenic Belt (CAOB), which is a global major accretionary orogen formed after the closure of the Paleo-Asian Ocean, and to its actualistic analogues - orogenic belts and accretionary complexes of the Western Pacific. The main focuses of the paper are the state of activities in the study of the CAOB, the theoretical basics of the new concept of continental construction, its challenges, prospects and s...
Despite being the largest accretionary orogen on Earth, the record of crustal growth and reworking o...
This paper attempts to review the descriptions on the genetic series of neotectonic forms in Eurasia...
Accretionary orogens develop at sites of oceanic subduction and they largely contribute to continent...
International audienceA new concept of continental construction based on four main terms: ( 1) crust...
We argue that the production of mantle-derived or juvenile continental crust during the accretionary...
Studies of supercontinental cycle are mainly concentrated on the assembly, breakup and dispersal of ...
The Central Asian Orogenic Belt (CAOB) was the result of long-lived multi-stage tectonic evolution, ...
Continental crust is a unique phenomenon, which distinguishes the Earth from the other planets of th...
The terrain analysis concept envisages primarily a possibility of approximation of fragments / terra...
Continental crust is formed above subduction zones by well-known process of “juvenile crust growth”....
This dissertation research addresses the tectonism of continental crust during ocean basin closure, ...
International audienceUnderstanding the development and evolution of accretionary orogens is crucial...
AbstractThis paper attempts to review the descriptions on the genetic series of neotectonic forms in...
The continental crust is our archive of Earth history, and the store of many natural resources; howe...
In the end of the 20th century folded structures of central Asia were regarded as formed by accretio...
Despite being the largest accretionary orogen on Earth, the record of crustal growth and reworking o...
This paper attempts to review the descriptions on the genetic series of neotectonic forms in Eurasia...
Accretionary orogens develop at sites of oceanic subduction and they largely contribute to continent...
International audienceA new concept of continental construction based on four main terms: ( 1) crust...
We argue that the production of mantle-derived or juvenile continental crust during the accretionary...
Studies of supercontinental cycle are mainly concentrated on the assembly, breakup and dispersal of ...
The Central Asian Orogenic Belt (CAOB) was the result of long-lived multi-stage tectonic evolution, ...
Continental crust is a unique phenomenon, which distinguishes the Earth from the other planets of th...
The terrain analysis concept envisages primarily a possibility of approximation of fragments / terra...
Continental crust is formed above subduction zones by well-known process of “juvenile crust growth”....
This dissertation research addresses the tectonism of continental crust during ocean basin closure, ...
International audienceUnderstanding the development and evolution of accretionary orogens is crucial...
AbstractThis paper attempts to review the descriptions on the genetic series of neotectonic forms in...
The continental crust is our archive of Earth history, and the store of many natural resources; howe...
In the end of the 20th century folded structures of central Asia were regarded as formed by accretio...
Despite being the largest accretionary orogen on Earth, the record of crustal growth and reworking o...
This paper attempts to review the descriptions on the genetic series of neotectonic forms in Eurasia...
Accretionary orogens develop at sites of oceanic subduction and they largely contribute to continent...