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The transition from Palaeo-Asian to marginal Pacific tectonic domain experienced in the Eastern North China Craton: evidence from Late Jurassic sediment provenance in the North Yellow Sea Basin
The North Yellow Sea Basin is located in an important position in the Eastern North China Craton, the sedimentary process of basin has obvious...
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Characteristics and main controlling factors of helium resources in the main petroliferous basins of the North China Craton
At present, the main controlling factors of helium accumulation is one of the key scientific problems restricting the exploration and development of...
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Multistage Formation of Neoarchean Potassic Meta-Granites and Evidence for Crustal Growth on the North Margin of the North China Craton
The North China Craton (NCC) is one of the most complex cratons in the world. It underwent a series of tectonothermal events during the...
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Geochronology and geochemistry of the polyphase mafic rocks in the North Liaohe Group, Jiao-Liao-Ji Belt, North China Craton: implications for petrogenesis and tectonic evolution
The Jiao-Liao-Ji Belt (JLJB) is one of the Paleoproterozoic orogenic belts within the North China Craton (NCC), whose tectonic evolution is still...
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Mineralogical Characteristics and Magmatic Evolution Significance of Garnets in the Late Jurassic Granites in **ngcheng, Eastern North China Craton
AbstractA series of Mesozoic granites related to the subduction of the ancient Pacific plate are widely developed in the eastern part of the North...
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Recycling of Paleo-Asian Ocean carbonates and its influence on the lithospheric composition of the North China Craton
The deep carbon cycle, which plays a critical role in mantle evolution and Earth habitability, is closely linked to the recycling of...
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Zircon U-Pb Geochronology of Baoyintu Group in the Northwestern Margin of the North China Craton and Its Geological Significance
The Baoyintu uplift is located at the northwestern margin of the North China Craton (NCC). The affiliation and evolution history of the uplift have...
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Initiation of the Unazuki Belt, Southwest Japan, during the Carboniferous as an island arc system along the North China Craton
The Unazuki Belt, Southwest Japan, is a part of the Hida Belt, which is characterized as a plutono-metamorphic complex with a continental affinity...
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Druse Calcite Crystals Formed by Mesoproterozoic Paleo-Earthquake Activity in the Northern Margin of the North China Craton
The Meso-neoproterozoic Bayan Obo rift is located along the northern margin of the North China Craton, and was associated with the break-up of the...
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Sedimentation History of the Aldan–Maya Sedimentary Basin (Southeast of the North Asian Craton) Reconstructed from a Seismostratigraphic Section
AbstractThe sedimentation history of the Aldan–Maya sedimentary basin was reconstructed based on a seismostratigraphic section. In total, ten...
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Prolonged Mantle Modification beneath the North China Craton: Evidence from Contrasting Mafic Dykes in Jiaodong Peninsula
The nature of lithosphere mantle beneath North China Craton (NCC) has been changed during the Mesozoic. We investigated the mafic dykes in Jiaodong...
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Destruction of the lower crust beneath the North China Craton recorded by granulite and pyroxenite xenoliths
The lower crust beneath the North China Craton (NCC) was transformed during the craton destruction in the Mesozoic, however, the transformation...
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Critical metal enrichment in Upper Carboniferous karst bauxite of North China Craton
Bauxite is a prominent constituent of the paleoweathering crust that formed during a ~ 150-million-year-long interval between the Ordovician and Late...
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Widespread refertilization of cratonic lithospheric mantle related to circum-craton plate subduction: evidence from peridotite xenoliths from the central North China Craton
Subduction of the Pacific slab has been widely credited for the destruction of the eastern North China Craton (NCC). However, the nature of the...
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Petrogenesis and Tectonic Implications of the Paleoproterozoic A-Type Granites in the **ong’ershan Area along the Southern Margin of the North China Craton
Paleoproterozoic A-type granites are widely distributed in the southern margin of the North China Craton (SNCC), providing important information for...
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A Deep Mantle Source for the Late Neoarchean Metamorphosed Basalts in Eastern Hebei, North China Craton: Insights from Whole-Rock Geochemistry and Sm-Nd Isotopes, and Zircon U-Pb-Hf Isotopes
The basalts within the greenstone belt worldwide serve as an ideal target to decipher the nature of Archean mantle sources and further to extend the...
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Mineral Chemistry of Biotite and Its Petrogenesis Implications in ca. 2.5 Ga Wangjiazhuang Granitic Pluton, North China Craton
The Wangjiazhuang granitic pluton is located in the central Zanhuang Domain, the central part of the North China Craton, which is mainly composed of...
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Periodicity of Endogenic Events of West Transbaikalia and North Mongolia (Eastern Segment of the Central Asian Foldbelt): U–Pb Age of Detrital Zircon from the Present-Day River Sediments
AbstractFive main stages of the formation and reworking of continental crust in the region are recognized on the basis of correlation between the...
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Is there a great unconformity between **amaling and Longshan formations in the North China Craton?
The existence of a 0.3 Ga “great unconformity” between the Mesoproterozoic “Undefined System” **amaling Formation and the “Neoproterozoic” Longshan...
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A Synthesis of Geophysical Data in Southeastern North China Craton: Implications for the Formation of the Arcuate Xuhuai Thrust Belt
The Xuhuai fold thrust belt (XHTB) is a curved structure in the southeastern margin of the North China Craton (NCC) that has attracted great...