supported by the National Key Research and Development Program of China(Grant No.2022YFF0800504);the National Natural Science Foundation of China(Grant Nos.42273057,42076063);the Natural Science Foundation of Shanghai(Grant No.21590712700)。
Sr-Nd isotopes are widely utilized as reliable tracers in sediment provenance studies.In this study,we compiled 304 Sr and 335 Nd isotope data of fine-grained surface sediments collected from major rivers in eastern C...
supported by the National Natural Science Foundation of China(42272129);the Outstanding Youth Science Fund Project of Sichuan Province(23NSFJQ0162);the Department of Natural Resources of Sichuan Province(KJ-2023-011);the Ministry of Science and Higher Education of Russia,State Assignment Project(122041400044-2);the Key R&D Program of Sichuan(Project#2022YFWZ0009);the Everest Scientific Research Program of Chengdu University of Technology.
Paleogeographic reconstructions are of key importance for understanding the history of continental breakups and amalgamations during Earth’s history.A special case is the history of the Asian continent,which,compared...
supported financially by the National Natural Science Foundation of China(No.42272111);the Second Tibetan Plateau Scientific Expedition Program(Nos.2019QZKK0204,2019QZKK0205).
Detrital U-bearing minerals(e.g.,zircon,apatite)U-Pb ages with specific trace-element geochemistry,are frequently used in provenance analyses.In this study,we focus on the Yarlung River drainage in South Tibet,charact...
Detrital geochronology fundamentally involves the quantification of major age ranges and their weights winthin an age distribution.This study presents a streamlined approach,modeling the age distribution of detrital z...
This study focuses on exoscopic analyses of detrital zircon grains of Archean and Paleoproterozoic age, contained in the sediments from the Niamey Neoproterozoic sandstones (Niamey region), with a view to confirming t...
supported by the National Natural Science Foundation of China(Grant Nos.92358301,41873004)。
Potassium isotopes are a novel tracer for continental weathering.Previous K isotope studies on chemical weathering generally targeted weathering profiles under a particular climate region,yet the effects of chemical w...
supported by the IiKSNF and KETEP grant funded by the Korean government MOTIE (No.2021040101003B);YJ acknowledged NRF-2021R1C1C101057011 through the National Research Foundation of Korea (NRF)funded by the Ministry of Science and ICT,Korea;SK acknowledged the 2017R1A6A1A07015374,2019R1A2C1002211;the KBSI R&D program (Project No.C330430);supported by Basic Research Project grant (GP2021-004)from the KIGAM funded by the Ministry of Science,ICT,and Future Planning,Korea.
Detrital zircon geochronology and Hf isotope analysis can be used for inferring provenance characteristics,and to evaluate the tectonic evolution of sedimentary basins and their link with regional orogenesis.The Paleo...
support by the Geoscience Center of the Georg-August-University Göttingen.Y.J.Liu acknowledges the National Key R&D(2022YFF0800400-2);National Natural Science Foundation of China(Grant No.42130305);Taishan Scholars(ts20190918);Qingdao Leading innovation talents(19-3-2-19-zhc);S.Z.Li acknowledges Marine S&T Fund of Shandong Province for Laoshan Laboratory(Qingdao)(No.2022QNLM050302);Taishan Scholars(tspd20210305);study has been performed at the Geoscience Center Göttingen.J.P.Zhou acknowledges China Scholarship Council(2016094678)。
The Cretaceous sedimentary successions in NE China are largely incomplete as the basins are inverted and younger strata are eroded.Except for the Songliao Basin,whose depositional record has remained relatively intact...
Universit a degli Studi di Bari Aldo Moro,Grant IDs:00596609ricat01。
U-Pb spot ages on detrital zircons from turbidite quartzarenites,quartz-feldspathic and volcaniclastic sandstones of the Tufiti di Tusa(TTF),Numidian Flysch(NF),Bifurto(BF),Gorgoglione(GF)and Serra Palazzo(SPF)formati...
the National Natural Science Foundation of China(42172114,41772102 and 41402171);National Science Foundation of the United States(EAR 1620595);the China Scholarship Council(201706455043).
Tectonic transition from a syn-rift stage to subsequent post-rift stage is an important mechanism in the evolution of extensional basins.The sedimentary infill records the crustal response to this process.We have obta...