Structural Evolution of a Triclinic‐type Transpressional High Strain Zone and Its Role in Exhuming the Root of the Paleoproterozoic Trans‐North China Orogen

Acta Geologica Sinica- China

doi 10.1111/1755-6724.13976

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May 1, 2019

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Wiley

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Structural Evolution of a Triclinic‐type Transpressional High Strain Zone and Its Role in Exhuming the Root of the Paleoproterozoic Trans‐North China Orogen

Acta Geologica Sinica- China

Full Text

Abstract

Categories

Date

Authors

Publisher

Related search

The Zanhuang Massif, the Second and Eastern Suture Zone of the Paleoproterozoic Trans-North China Orogen

Late Paleoproterozoic (1900–1800Ma) Nappe Stacking and Polyphase Deformation in the Hengshan–Wutaishan Area: Implications for the Understanding of the Trans-North-China Belt, North China Craton

Paleoproterozoic High-Pressure Metamorphism in the Northern North China Craton and Implications for the Nuna Supercontinent

Major Tectonic Units of the North China Craton and Their Paleoproterozoic Assembly

Neoarchean(?) to Paleoproterozoic Metamorphic and Structural Evolution of the Hartville Uplift, Southeastern Wyoming

Comment on “Trans-Hudson Orogen of North America and Himalaya-Karakoram-Tibetan Orogen of Asia: Structural and Thermal Characteristics of the Lower and Upper Plates” by M. R. St-Onge Et Al.

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