National Natural Science Foundation of China(NSFC grant numbers 41973029,41272070)to Zou.
Young zircons from crystal-poor volcanic rocks provide the best samples for the investigations of pre-eruption magmatic processes and for testing a possible relationship between zircon Eu anomalies and crustal thickne...
the Curtin Research Office for providing support to LS。
The Beshta-Kamenistaya intrusions are located in the Main Range structural zone of the Greater Caucasus.They are composed of tonalitic gneisses that genetically resemble granites of the tholeiitic series of the ophiol...
financially supported by the Major Research Project of National Natural Science Foundation of China(NSFC Project;Grant Nos.92162215 and 92155305);National Key Basic Research Development Program of China(973 Program;Grant Nos.2015CB452602 and 2015CB452606);111 Plan under the Ministry of Education of China and the State Administration of Foreign Experts Affairs,China(Grant No.B07011)。
Magmatic-hydrothermal Sn deposits are commonly associated with high silica magmas,but why most global high silica granites do not bear economic Sn ore grades remains unclear.Two crucial factors controlling magmatic-hy...
supported by the National Natural Science Foundation of China(Nos.41973013,41730211);the Natural Science Foundation of Hubei Province(No.2020CFA045);the Most Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences(Nos.MSFGPMR04 and MSFGPMR08)。
This work evaluates the use of femtosecond laser ablation multiple collector inductively coupled plasma mass spectrometry(fs-LA-MC-ICP-MS) for Zr isotopic analysis in zircons. The mass fractionation caused by instrume...
supported by the National Natural Science Foundation of China(No.41973034);the Postdoctoral Initiation Fund of Northwestern University(No.208521)。
The origin of lowδ^(18)O signals in zircons from the Early Cretaceous A-type granites in eastern China has long been disputed.It is uncertain whether the^(18)O-depleted features were inherited from high-temperature h...
financially supported by National Science Foundation of China(Grant Nos.41303026);the funded project of Hubei Key Laboratory of Paleontology and Geological Environment Evolution(Grant No.PEL-202010);China Geological Survey(Grant No.DD20190050)。
Objective Geological records of Earth history in the Hadean(>4.0 Ga)are critical for understanding the earliest evolution of the planet’s continental crust.Unfortunately,investigation of such proto-continental crust,...
financially supported by the Inner Mongolia Autonomous Region Geological and Mineral Exploration Fund(Grant Nos.2017-YS01,2020-YS01)。
This study focuses on the geology,geochemistry,zircon U-Pb geochronology and tectonic settings of the three types of seamount basalts from the Xingshuwa subduction accretionary complex in the Xar Moron area,eastern ma...
supported by the National Natural Science Foundation of China(Grant Nos.40739903 and 41872137)。
The in situ zircon U-Pb-Lu-Hf isotope records from end-Permian volcanic interlayers in southwest China,integrated with previous studies,restructure the evolutionary history of the Yangtze Craton from Precambrian to La...
The Ekomedion two-mica granite,southwestern Cameroon,has potential for uranium and molybdenum mineralization.Here,we present LA-ICP-MS U-Pb ages,Lu-Hf isotope characteristics,trace element concentrations and Ti-geothe...
supported by the National Natural Science Foundation of China (Grant Nos. 41603053);the National Key R & D Program of China (No. 2018YFC0604206)
Detailed studies on U-Pb ages and Hf isotope have been carried out in zircons from a carbonatite dyke associated with the Bayan Obo giant REE-Nb-Fe deposit,northern margin of the North China Craton(NCC),which provide ...