supported by the UNISINOS-PETROBRAS and UNISINOS-CNODC Cooperation Agreements.
The paleogeographic reconstruction of fragmented and dispersed continents often poses a challenge due to the lack of information regarding the nature of that extend beneath passive margin basins.To define the width of...
the Editorial Advisor Prof.M.Santosh,Associate Editor Dr.S.Glorie,and two anonymous reviewers for their comments.H.G.acknowledges funding from the Khalifa University start-up fund(8474000697/FSU-2024-006);K.W.acknowledges support from the McDonnell Center for the Space Sciences and NASA(Emerging Worlds Program Grant No.#80NSSC21K0379);T.E.J.acknowledges funding from the Australian Government through an Australian Research Council Discovery Project(DP200101104)。
Constraining the processes associated with the formation of new(juvenile)continental crust from mantle-derived(basaltic)sources is key to understanding the origin and evolution of Earth’s landmasses.Here we present h...
financially supported by the State Key Research Development Program of China(Grant No.2022YFF0800903);the National Natural Science Foundation of China(NSFC)(Grant Nos.42261144669 and 42273073)。
High-silica granitoids record the formation and evolution of the continental crust.A new intrusive complex has been recognized among silicic volcanic rocks of the Weixi arc,Southwest China.The intrusions consist of gr...
This work was financially supported by the Natural Science Foundation of China(grant Nos.42072063,41722204);Program for Jilin University Science and Technology Inovative Research Team(2021TD-05);Postgraduate Innovation Research Program of Jilin University(101832020CX199).
Accretionary orogens are sites of extensive continental crustal growth and modification.The mechanism by which mafic crust is transformed into silicic melts(i.e.,maturation of continental crust)is important for unders...
supported by National Natural Science Foundation of China(Nos.42072228,42102060,41902036,41572182);China Postdoctoral Science Foundation(No.2021M692983);the Chinese Ministry of Education(No.BP0719022);the Most Special Fund(Nos.MSFGPMR02-3,MSFGPMR30);Open funds from the State Key Laboratory of Geological Processes and Mineral Resources;China University of Geosciences(Nos.GPMR201703,GPMR201704 and GPMR201903);the Fundamental Research Funds for National University(No.CUG-G1323511572)。
‘Single shot'laser-ablation split-stream(SS-LASS)technique analyzing unpolished zircon grains makes their thin rims tenable for determination,which thus offers great potential in deciphering the timing of multiple an...
financially supported by the National Natural Science Foundation of China(Grant Nos.92162210,42172096 and 41773028).
There are two factors,source composition and magmatic differentiation,potentially controlling W-Sn mineralization.Which one is more important is widely debated and may need to be determined for each individual deposit...
The heat budget of sedimentary basins is determined by heat transfer across the lithosphereasthenosphere boundary and lithospheric heat sources,such that the tectonic evolution of their host continental and oceanic li...
This study was financially supported by National Key Research and Development projects(No.2019YFC0604903,No.2021YFA0716004);by Joint Funds of the National Natural Science Foundation of China(Grant No.U20B6001).
Granites play a crucial role in the Earth's thermal regime and its evolution.Radiogenic heat production(RHP)by the decay of radioactive elements(U,Th,K)in granites is a significant parameter in estimating the thermal ...
The Western Alps provide classic examples of eclogite facies subduction metamorphism widely preserved in Adriaand Europe-derived continental nappes and interposed ophiolitic units derived from the suture of the Piedmo...
financially supported by National Natural Science Foundation of China (42125302, 42073026, 41888101 and42073024);the support from the Xplorer Prize。
We used compiled geochemical data to investigate the mechanisms that control Mg#(molar ratio of Mg/(Mg+Fe_T)) in andesitic arc lavas.We find that andesites from mature continental arcs with crustal thickness of>45 km ...