Results 91 to 100 of about 5,526,236 (208)

Assembly, accretion and breakup of the Paleo-mesoproterozoic Columbia supercontinent: Records in the North China Craton

open access: yes, 2003
Established pre-Rodinian connections between cratonic blocks around the world lead to the proposal of a Paleo-Mesoproterozoic supercontinent, named Columbia, which may have contained nearly all of the earth's continental blocks at some time between 1.8 ...
Zhao, G, Sun, M, Wilde, SA, Li, S
core   +1 more source

Geochronology and Hf isotopic characteristics of detrital zircon from the miboshan formation in the eastern hexi corridor: implications for the relationship between the alxa block and the North China craton

open access: yesFrontiers in Earth Science
This study presents U-Pb ages together with newly obtained systematic Hf isotopic data from detrital zircons of the Middle Ordovician Miboshan Formation in the eastern Hexi Corridor (northwestern China), aiming to constrain its provenance characteristics
Hongze Yang   +6 more
doaj   +1 more source

Origin and Evolution of the Ore-Forming Fluids in the Liyuan Gold Deposit, Central North China Craton: Constraints from Fluid Inclusions and H-O-C Isotopic Compositions

open access: yesGeofluids, 2017
The Liyuan gold deposit is hosted within Archean basement metamorphic rocks and controlled by the NNE-trending faults in the central North China Craton. The ore-forming processes can be divided into three stages (early, middle, and late).
Ying Ma   +3 more
doaj   +1 more source

Seismic mapping of the central and southern segments of the Tanlu fault zone using P-wave receiver functions

open access: yesScientific Reports
The central and southern segments of the Tanlu fault zone, located in the collision boundary between the Yangtze Plate and the North China Craton, underwent complex tectonic deformation associated with the Pacific Plate subduction.
Qian Liu, Ziqiang Lü, Jianshe Lei
doaj   +1 more source

A review on the magnetotelluric studies over the Central Asian Orogenic Belt—recent developments and future aspects

open access: yesFrontiers in Earth Science
The Central Asian Orogenic Belt (CAOB) was originated from the subduction, closure, convergence, and post-collisional extension of the Paleo-Asian Ocean located between the North China Craton, Tarim Craton, and the Siberian Craton during the late Permian
Yifan Li   +7 more
doaj   +1 more source

Supporting Information for Rise of oxidation and hydration in Neoarchean continental crust caused by subduction (North China Craton)

open access: yes
Supporting Information for Rise of oxidation and hydration in Neoarchean continental crust caused by subduction (North China ...
Wang, Chao
core   +1 more source

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