Zircon ages of the Bayankhongor ophiolite mélange and associated rocks: Time constraints on Neoproterozoic to Cambrian accretionary and collisional orogenesis in Central Mongolia

Article

Abstract: Central Mongolia is geologically characterized by close juxtaposition of an accreted oceanic terrane

Palabras claves:

Accretion-collision, Central Asian Orogenic Belt, Mongolia, Ophiolite, Syenite porphyry, zircon

Autores:

Alfred Kron̈er, Jian P., Liu D.Y., Miao L., Shi Y., Tomurhuu D., Windley B.F., Zhang F., Zhang W.

Fuentes:

scopus