Deep Crustal Structure of the Eastern Central Asian Orogenic Belt Revealed by Integrated Magnetic-Gravity Imaging
The Central Asian Orogenic Belt (CAOB) is a globally magnificent accretionary orogenic belt that has been formed since the Phanerozoic as a result of the Paleozoic closing of the Paleo-Asian Ocean (PAO). The transition zone between the North China Craton (NCC) and the Siberia Plate is located in the...
Main Authors: | Chang Chang, Haiyan Wang, Rui Gao, Hua Guo, Song Han, Yangang Wu |
---|---|
Format: | Article |
Language: | English |
Published: |
Frontiers Media S.A.
2022-03-01
|
Series: | Frontiers in Earth Science |
Subjects: | |
Online Access: | https://www.frontiersin.org/articles/10.3389/feart.2022.843499/full |
Similar Items
-
Paleozoic tectonic evolution of the eastern Central Asian Orogenic Belt in NE China
by: Yong-fei Ma, et al.
Published: (2022-10-01) -
Permian tectonic evolution and continental accretion in the eastern Central Asian Orogenic Belt: A perspective from the intrusive rocks
by: Anzong Fu, et al.
Published: (2024-03-01) -
Permian tectonic switch of the southern Central Asian Orogenic Belt: Constraints from magmatism in the southern Alxa region, NW China
by: Wang Erteng, et al.
Published: (2024-03-01) -
Source-to-sink of Late carboniferous Ordos Basin: Constraints on crustal accretion margins converting to orogenic belts bounding the North China Block
by: Anqing Chen, et al.
Published: (2020-11-01) -
Two-Stage Orogenic Cycle of the Eastern Paleo-Asian Ocean from Early Palaeozoic to Early Triassic: Constraints from Magmatic Rocks of the Southeastern Central Asian Orogenic Belt
by: Jinlei Sun, et al.
Published: (2022-08-01)