National Natural Science Foundation of China(Grant No.52202282);Opening Project of the State Key Laboratory of High-Performance Ceramics and Superfine Microstructure(Grant No.SKL202209SIC);Natural Science Foundation of Tianjin City(Grant No.22JCYBJC00040).
Developing high-capacity and high-rate anodes is significant to engineering sodium-ion batteries with high energy density and high power density.Layered Na_(2)Ti_(3)O_(7)(NTO),with an open crystal structure,large theo...
financial support from the Academic-Industry Cooperation Project(grant HE1913);National Natural Science Foundation of China(41972094).
The Haoyaoerhudong gold deposit,located in the northwestern part of the North China craton(NCC),has produced over 120 metric tonnes(t)of gold since 2007.It has a total reserve of>240 t at average gold grade of 0.62 g/...
supported by the National Natural Science Foundation of China(Grants Nos.42103011,42073034;42288201);the B-type Strategic Priority Program of the Chinese Academy of Sciences(Grants No.XDB41000000)。
In-situ dating of the zircons, titanites, and apatites in the rock fragments of approximately 1 cm2in size from the Acasta Gneiss Complex was performed using secondary ion mass spectrometry or laser ablation inductive...
supported by funds from the National Natural Science Foundation of China(Grant Nos.42172067,41972064,U1906207);the SDUST Research Fund。
Gneisses with anatectic characteristics from the Liansan island in the Sulu UHPM(ultra-high pressure metamorphic)belt were studied for petrography,titanite U-Pb dating and mineral geochemistry.Three origins of garnets...
acknowledge the DST-SERB grant Project No.CRG/2020/002635,DST-INSPIRE fellowship No.IF210186.
The Ghansura Rhyolite Dome of Bathani vol-cano-sedimentary sequence,eastern India,represents a subvolcanic felsic magma chamber that was invaded by crystal-rich mafic magma during its cooling phase to form an assortme...
supported by ARC Linkage Project LP160100578(JLP and MH);the Mineral Exploration Cooperative Research Centre whose activities are funded by the Australian Government’s Cooperative Research Centre Program;support of an Australian Government Research Training Program Stipend and LJM acknowledges the support of ARC DECRA Fellowship DE210101126.
Tectonic reconstructions of Proterozoic Australia commonly place the Peake and Denison Domain of the northeastern Gawler Craton at the interface between the North and South Australian cratons prior to the reconfigurat...
funded in part by the Ministère des Ressources naturelles du Québec contribution no.8449–2021-2022–04 under the supervision of A;Moukhsil and partially funded by an NSERC-Discovery grant RGPIN-2014-04593 hosted by F.Gervais.
In this contribution,we analyzed a pair of mafic samples collected from a recently identified shear zone and its proximal footwall from the Manicouagan Imbricate Zone(MIZ)of the central Grenville Province,Québec,Cana...
financially supported by the National Natural Science Foundation of China(Grant No.42130814)。
The West Qinling orogen in central China,formed from continental collision between the North China and Yangtze cratons in the Late Triassic,hosts numerous gold deposits with a total Au endowment of about 2000 t.Most d...
supported by the National Science Foundation of China(Grant Nos.92055202);the Second Tibetan Plateau Scientific Expedition and Research(Grant No.2019QZKK0702);the China Geological Survey(Grant Nos.DD20221817 and DD20221630)。
The formation of titanite coronae after rutile is common in retrograde high-to ultrahigh-pressure meta-mafic rocks,which provides a good opportunity to address the geochemical behavior of HFSE in crustal environments....
financial support from the National Centre of Excellence in Geology, University of Peshawar, Pakistan。
The putative Jambil meta-carbonatites of Swat,northern Pakistan,occur as discrete intrusions into the Proterozoic Manglaur Formation,which are difficult to be distinguished from nearby calc-silicate marble because bot...