L
Lilin Du
Researcher at Chinese Academy of Sciences
Publications - 23
Citations - 2359
Lilin Du is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 19, co-authored 23 publications receiving 2047 citations. Previous affiliations of Lilin Du include Huazhong University of Science and Technology.
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Growth and reworking of the early Precambrian continental crust in the North China Craton: Constraints from zircon Hf isotopes
TL;DR: Zhang et al. as discussed by the authors synthesize more than 2600 Hf isotope data on the Archean-Paleoproterozoic zircons from the North China Craton (NCC).
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SHRIMP U–Pb zircon geochronology and geochemistry of metavolcanic and metasedimentary rocks in Northwestern Fujian, Cathaysia block, China: Tectonic implications and the need to redefine lithostratigraphic units
TL;DR: In this paper, the SHRIMP U-Pb zircon ages presented here indicate that the original lithostratigraphy and the old “Group” and “Formation” terminology should be abandoned.
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Multistage late Neoarchaean crustal evolution of the North China Craton, eastern Hebei
Allen P. Nutman,Yusheng Wan,Lilin Du,Clark R.L. Friend,Chunyan Dong,Hangqiang Xie,Wei Wang,Huiyi Sun,Dunyi Liu +8 more
TL;DR: In this article, the authors show that there is not a single protracted event at the end of the Archaean lasting ∼60 million years, but that from east to west there are several separate events with their own unique character.
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Zircon ages and geochemistry of late Neoarchean syenogranites in the North China Craton: A review
Yusheng Wan,Chunyan Dong,Dunyi Liu,Alfred Kröner,Conghui Yang,Wei Wang,Lilin Du,Hangqian Xie,Mingzhu Ma +8 more
TL;DR: In this paper, two phases of syenogranite magmatism are recognized based on geological relationships, degree of metamorphism, deformation and magmatic zircon ages.
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Evolution of the Yunkai Terrane, South China: Evidence from SHRIMP zircon U–Pb dating, geochemistry and Nd isotope
TL;DR: In this article, four meta-sedimentary rock samples, two each from the Yunkai Group and Gaozhou Complex, together with three granite samples, record metamorphic and magmatic zircon ages of 443-430-Ma (Silurian), with many inherited and detrital zircons with the ages mainly ranging from 1.1 to 0.8.