Sedimentary fill history of the Huicheng Basin in the West Qinling Mountains and associated constraints on Mesozoic intracontinental tectonic evolution

The Qinling Orogenic Belt is divided commonly by the Fengxian-Taibai strike-slip shear zone and the Huicheng Basin into the East and West Qinling mountains, which show significant geological differences after the Indosinian orogeny. The Fengxian-Taibai fault zone and the Meso-Cenozoic Huicheng Basin...

Ausführliche Beschreibung

Gespeichert in:

Bibliographische Detailangaben
Veröffentlicht in:	Science China. Earth sciences 2013-10, Vol.56 (10), p.1639-1653
Hauptverfasser:	Li, Wei, Dong, YunPeng, Guo, AnLin, Liu, XiaoMing, Liu, YiQun, Zha, XianFeng, Zhang, KuaiLe
Format:	Artikel
Sprache:	eng
Schlagworte:	Basins Belts Cenozoic Cretaceous Earth and Environmental Science Earth science Earth Sciences Evolution Fault lines Faults Jurassic Mesozoic Mountains Orogeny Plate tectonics Research Paper Sediment transport Sedimentary basins Sedimentary geology Shear zone Tectonics Triassic 中新生代盆地中生代历史构造演化沉积充填相关约束西秦岭陆内
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!

Schreiben Sie den ersten Kommentar!