Lithotectonic elements and geological events in the Hengshan-Wutai-Fuping belt: A synthesis and implications for the evolution of the Trans-North China Orogen

Article

Abstract: The Hengshan-Wutai-Fuping belt is located in the middle segment of the Trans-North China Orogen, a P

Palabras claves:

Archaean, Collision, Hengshan-Wutai-Fuping belt, Magmatic arc, Palaeoproterozoic, Subduction, Trans-North China Orogen

Autores:

Alfred Kron̈er, He Y., Li S., Li X., Sun M., WILDE S.A., Xia X., Zhang J., Zhao G.C.

Fuentes:

scopus