Triassic southeastward subduction of North China Block to South China Block: Insights from new geological, geophysical and geochemical data

S Li, B Jahn, S Zhao, L Dai, X Li, Y Suo, L Guo… - Earth-Science …, 2017 - Elsevier
Lithospheric subduction prior to the assembly of the South China and North China blocks is
traditionally considered to be directed northward. However, some critical geological and …

The Dabie–Sulu continental collision zone: a comprehensive review

RY Zhang, JG Liou, WG Ernst - Gondwana Research, 2009 - Elsevier
The Dabie–Sulu Triassic orogen in central-eastern China was created by northward
subduction of the Yangtze cratonal plate beneath the Sino-Korean craton. Eclogites, garnet …

[HTML][HTML] On ultrahigh temperature crustal metamorphism: Phase equilibria, trace element thermometry, bulk composition, heat sources, timescales and tectonic …

DE Kelsey, M Hand - Geoscience Frontiers, 2015 - Elsevier
Ultrahigh temperature (UHT) metamorphism is the most thermally extreme form of regional
crustal metamorphism, with temperatures exceeding 900° C. UHT crustal metamorphism is …

Tectonic evolution of the North China Block: from orogen to craton to orogen

TM Kusky, BF Windley, MG Zhai - Geological Society, London …, 2007 - lyellcollection.org
Abstract The North China Craton contains one of the longest, most complex records of
magmatism, sedimentation, and deformation on Earth, with deformation spanning the …

Neoproterozoic (~ 900 Ma) Sariwon sills in North Korea: Geochronology, geochemistry and implications for the evolution of the south-eastern margin of the North …

P Peng, MG Zhai, Q Li, F Wu, Q Hou, Z Li, T Li… - Gondwana …, 2011 - Elsevier
The Sariwon sills are distributed in the Pyongnam basin at the center of the Korean
peninsula, eastern part of the North China Craton. These sills are up to 150m in thickness …

Evidence for Permo-Triassic collision in far east Asia: the Korean collisional orogen

S Kwon, K Sajeev, G Mitra, Y Park, SW Kim… - Earth and Planetary …, 2009 - Elsevier
Eclogites from paragneiss in the Korean Peninsula are characterized by a peak pressure
assemblage of garnet+ omphacite+ quartz+ rutile, that is overprinted by multiphase …

Early Mesozoic magmatism and tectonic evolution of the Qinling Orogen: Implications for oblique continental collision

F Hu, S Liu, MN Ducea, JB Chapman, F Wu… - Gondwana Research, 2020 - Elsevier
Abstract The Qinling Orogenic Belt in Central China is formed by an oblique continental
collision between the North China and South China Blocks. In this review, we summarize the …

Pan-African metamorphic and magmatic rocks of the Khanka Massif, NE China: further evidence regarding their affinity

JB Zhou, SA Wilde, GC Zhao, XZ Zhang… - Geological …, 2010 - cambridge.org
The Khanka Massif is a crustal block located along the eastern margin of the Central Asian
Orogenic Belt (CAOB) and bordered to the east by Late Jurassic–Early Cretaceous circum …

The geology of North Korea: an overview

M Zhai, XH Zhang, YB Zhang, FY Wu, P Peng… - Earth-Science …, 2019 - Elsevier
Abstract The Korean Peninsula (KP) occupies a junction area of three big tectonic domains
that are the Paleo-Central Asian Orogenic Belt, Paleo-Tethyan Orogenic Belt and the …

Two-stage Triassic exhumation of HP–UHP terranes in the western Dabie orogen of China: constraints from structural geology

S Li, TM Kusky, G Zhao, X Liu, G Zhang, H Kopp… - Tectonophysics, 2010 - Elsevier
Abundant exposures of widely-distributed HP–UHP metamorphic rocks in the western part of
the Dabie orogen enable us to study the tectonic evolution of HP–UHP terranes associated …