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| 1 | The Late Cretaceous source-to-sink system at the eastern margin of the Tibetan Plateau:Insights from the provenance of the Lanping Basin显示文摘The surface uplift of the Tibetan Plateau(TP)and its geomorphology evolution has triggered aridification of Asia's interior and drainage development at the eastern margin of the plateau.However,how the pre-Cenozoic early growth histories of the TP impact the drainage system and climate is poorly constrained.The Late Mesozoic Lacustrine evaporite-bearing basins on the eastern margin of the TP record significant information on the uplift of the source terranes,source-to-sink system development and climate change.In this study,we presented detrital zircon U-Pb ages from the Upper Cretaceous Yunlong Formation in the Lanping Basin,as well as Hf isotopic,petrographic,direct statistical,and multidimensional scaling analyses,and use them to characterize the provenance and reconstruct the drainage system.All of the samples have five major age peaks at 200-290 Ma,400-490 Ma,750-1000 Ma,1750-1950 Ma,and 2400-2600 Ma with mostly negativeε_(Hf)(t)values(81%).We infer the sediments are primarily derived from recycled sediments of the Songpan-Garze terrane,and partly from the Sichuan Basin and the Southern Qiangtang terrane,as well as the exposed magmatic rocks of the Yidun Arc and SongpanGarze terrane.The provenance features of the contemporaneous sediments from the Sichuan,Xichang,Chuxiong,and Simao basins indicate a complex hierarchical drainage pattern on the eastern margin of the TP during the Late Cretaceous.The hierarchical drainage system exhibits a complete gradational cycle of lake-basin types from overfilled freshwater Sichuan Basin through balanced fill saline Xichang Basin and underfilled hypersaline Chuxiong,Lanping,Simao,and Khorat Plateau basins from proximal to distal.The early growth of the TP primarily controlled the drainage and lake-basin evolution by not only causing the uplift and exhumation of the source areas and providing large amounts of clastic material to the proximal sub-drainage areas but also intensifying the aridity and deposition of evaporites. | Licheng Wang Lijian Shen Chenglin Liu Ke Chen Lin Ding Chengshan Wang | 2021 | Geoscience Frontiers2021，12，3： | 2 |
| 2 | Hierarchically Designed SiOx/SiOy Bilayer Nanomembranes as Stable Anodes for Lithium Ion Batteries显示文摘 | Lin Zhang Junwen Deng Lifeng Liu Wenping Si Steffen Oswald Lixia Xi Manab Kundu Guozhi Ma Thomas Gemming Stefan Baunack Fei Ding Chenglin Yan Oliver G. Schmidt | 2014 | Adv Mater2014，，26： | 1 |
| 3 | Evaporation Stage of Paleo-saline Lake in the Sichuan Basin, China: Insight from Fluid inclusions in Halite显示文摘Sichuan Basin is one of the most important marine–salt forming basins in China. The Simian and Triassic have a large number of evaporites. The Triassic strata have found a large amount of polyhalite and potassium-rich brine. However, no soluble potassium salt deposit were found. In this study, the halite in well Changping 3 which is located at the eastern part of the Sichuan basin was studied using the characteristics, hydrogen and oxygen isotopes of the fluid inclusion in halite to reconstruct the paleoenvironment. The salt rocks in well Changping 3 can be divided into two types: grey salt rock and orange salt rock. The result shows that the isotopic composition of the halite fluid inclusion is distinct from the global precipitation line reflecting that the salt formation process is under strong evaporation conditions and the climate is extremely dry. At the same time, compared with the hydrogen and oxygen isotopes of brine in the Sichuan Basin and the hydrous isotope composition of the inclusions in the salt inclusions of other areas in China, it is shown that the evaporation depth of the ancient seawater in the Sichuan Basin was high and reached the precipitation of potassium and magnesium stage. | DING Ting LIU Chenglin GUO Fusheng ZHAO Yanjun WANG Mingquan CHEN Liuqin | 2020 | Acta Geologica Sinica(English Edition)2020，94，3： | 1 |
| 4 | Effects of Mg on the structures and cycling properties of the LaNi 3.8 hydrogen storage alloy for negative electrode in Ni/MH battery显示文摘 | Zhewen Ma Ding Zhu Chaoling Wu Chenglin Zhong Qiannan Wang Wanhai Zhou Linshan Luo Yucheng Wu Yungui Chen | 2015 | Journal of Alloys and Compounds2015，，： | 1 |
| 5 | Mechanical pressing method for making high-quality perovskite single crystals显示文摘Halide perovskites show excellent photovoltaic properties[1−4].However,the preparation of high-quality perovskite crystals remains a great challenge,which limits their applications.Perovskite materials applied to photodetectors mainly include polycrystalline thin films and single crystals.Traditional solution methods are used to prepare polycrystalline thin films,and the films are full of defects such as voids and grain boundaries[5−7].Compared to polycrystalline thin films,perovskite single crystals possess high crystallinity and low defect density[8−10].Photodetectors based on perovskite single crystals exhibit excellent performance[11].However,the size limitation of single crystals hinders their application in photodetectors[12]. | Chenglin Wang Jie Sun Jiangzhao Chen Cong Chen Liming Ding | 2023 | Journal of Semiconductors2023，44，11： | 0 |
| 6 | Alternating current electrolysis:A photoredox catalysis mimic and beyond显示文摘Alternating current electrolysis(ACE)is an emerging powerful synthetic tool,which principally resembles photoredox catalysis strategies.Its periodically alternating polarity feature allows oxidation and reduction processes to take place on the same electrode surface in a well-controlled manner via the fine-tuning of current frequency along with other reaction parameters.Therefore,many challenging transformations in typical direct electrolysis,including constant current electrolysis or constant potential electrolysis,could be achieved via ACE.The recent advances in the organic synthesis using this emerging technology and its advantages over direct electrolysis are highlighted. | Junsong Zhong Chenglin Ding Hyunwoo Kim Terry McCallum Keyin Ye | 2022 | Green Synthesis and Catalysis2022，3，1： | 0 |
| 7 | Genesis of Polyhalite in the Halite in Jialingjiang Formation of Triassic,Eastern Sichuan Basin,China显示文摘Polyhalite generally formed in the early diagenetic stage.It is formed by the brine which rich in K+and Mg2+and adverse reaction with the gypsum,anhydrite,glauberite(Pierre,1985;Peryt et al.,2005;Leitner et al., | ZHAO Yanjun LIU Chenglin WANG Lichen DING Ting WANG Mingquan | 2014 | Acta Geologica Sinica(English Edition)2014，88，S1： | 0 |
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