NOM DE FICHIER: Geodynamic Evolution of Sedimentary Basins. International Symposium, Moscow, May 18-23, 1992.pdf
DATE DE PUBLICATION: 1996-Jan-01
TAILLE DU FICHIER: 8,34 MB
The intracontinental weakness of Asia's interior has caused deformation in the Tian Shan Range after the collision of India into Asia. However, the Tian Shan was uplifted prior to the Cenozoic Indo-Asia collision. Paleozoic. The Tian Shan contains two late Paleozoic sutures. The older, southern suture marks the collision of a passive margin at the north of the Tarim block and an active ...
how and where sedimentary strata have been deposited and preserved during Earth history. The formation of sedimentary basins is ultimately controlled by topography that defines the surface depressions that receive the sediments, the elevated regions that provide sediment sources, and the topographic and bathymetric gradients that transport sediments from source to basin.