All abstracts by Debin Yang in conference series: Goldschmidt
(2020) Sedimentary Response to the Tectonic Evolution of the Southern North China Craton during the Late Paleozoic and MesozoicYang D, Yang H, Xu W & Wang F
(2013) Petrogenesis of Early Cretaceous Intrusive Rocks from Southern Margin of the North China Craton: Constraints from Zircon U-Pb Ages and Sr-Nd-Pb-Hf Isotopes
Yang D, Xu W, Wang F & Pei F
(2012) Petrogenesis of the Mesozoic Intermediate Intrusive Rocks in the Central North China Craton: Constraints from Zircon U – Pb Chronology and Geochemistry
Yang D-B, Xu W-L, Pei F-P & Wang D-Y
(2011) Chronology of Detrital Zircons from Jurassic Sandstones in Western Shandong Province, China: Constraints on the Nature of the Tan–Lu Fault Zone
Yang D, Xu W, Xu Y & Pei F
(2011) Recycling of Lower Continental Crust in an Intracontinental Setting: Mineral Chemistry and Oxygen Isotope Insights from Websterite Xenoliths in the North China Craton
Xu W, Zhou Q, Pei F, Yang D, Gao S, Wang W & Feng H
(2010) Spatial Extent of Influence of Deeply Subducted Continental Crust to Adjacent Lithosphere: Constraints from Sr-Nd-Pb Isotopic Compositions of Mesozoic Gabbros and High-Mg Diorites in Western Shandong, China
Yang D, Xu W, Yang C & Pei F
(2010) Multiplicity of the North China Craton Destruction: Constraints from Metasomatic Types and Zircon U-Pb Ages from Peridotite Xenoliths Entrained by Mesozoic High-Mg# Diorites
Xu W, Yang D, Gao S, Pei F & Wang W
(2010) Heterogeneity of the Lower Continental Crust beneath Southern Jilin Province, NE China: Evidence from Geochemical and Sr–Nd–Pb Isotopic Compositions of Early Cretaceous Granitoids
Pei F, Xu W, Yang D, Lu S & Feng H
(2009) Recycled Lower Continental Crust: Re-Os Isotopic Evidence from Peridotite Xenoliths Entrained by Mesozoic High-Mg Diorites in the Eastern North China Craton
Xu W-L, Gao S, Yang D-B, Yuan H-L, Rudnick RL & Walker RJ
(2008) Mesozoic Lithospheric Mantle of the Central North China Craton: Evidence from Peridotite Xenoliths
Xu W-L, Yang D-B, Gao S, Yu Y & Pei F-P