Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications

Constraints on the paleogeographic evolution of the North China Craton during the Late Triassic–Jurassic

“…4c; Zheng et al, 2004;Tian et al, 2007;Zhang et al, 2007bZhang et al, , 2007cZhang et al, , 2007dZhang et al, , 2009cZhang et al, , 2009dShi et al, 2010;Yang and Li, 2008;Ma and Zheng, 2009). The NQO is characterized by the Ordovician-Silurian and early Mesozoic magmatic rocks .…”

Thrusting and exhumation of the southern Mongolian Plateau: Joint thermochronological constraints from the Langshan Mountains, western Inner Mongolia, China

“…The CAOB is a major Phanerozoic accretionary orogen seated between the European Craton (EC) to the west, the Siberian Craton (SC) to the east, and the NCC to the south (e.g., Windley et al, 2007;Xiao et al, 2009). The accretion process of the CAOB is related to the tectonic evolution of the Paleo-Asian Ocean (e.g., Tang et al, 1990;Han et al, 2011;Xu et al, 2013) and the final closure of the Paleo-Asian Ocean resulted in the amalgamation of the NCC and CAOB during the Late Permian to Triassic (e.g., Xiao et al, 2003, Zhang et al, 2007a, 2009a, 2009bMiao et al, 2008;Jian et al, 2010). In the CABO, the closure of the Mongol-Okhotsk orogen shows a youngering trend from the Permian-Jurassic in the west to Late Jurassic-Early Cretaceous in the east (Zonenshain et al, 1990;Cogné et al, 2005;Tomurtogoo et al, 2005).…”

Fluid Inclusion and Oxygen Isotope Constraints on the Origin and Hydrothermal Evolution of the Haisugou Porphyry Mo Deposit in the Northern Xilamulun District, NE China

“…In Paleozoic, due to the southward subduction of the Paleo-Asian oceanic plate beneath the northern margin of the North China Craton, extensive subduction-related intrusions have been recognized in the region, forming a typical Andean-type continental margin [24,25]. In Triassic, NE China went into a postcollisional intraplate evolution stage, as indicated by the occurrence of many alkaline rocks including ultramafic-syenite complexes, lamprophyres, and A-type granites [24][25][26][27][28].…”

“…In Triassic, NE China went into a postcollisional intraplate evolution stage, as indicated by the occurrence of many alkaline rocks including ultramafic-syenite complexes, lamprophyres, and A-type granites [24][25][26][27][28]. Since Jurassic, NE China has been reactivated as a result of the westward subduction of the PaleoPacific oceanic plate [23,29].…”