financially supported by the National Natural Science Foundation of China(NSFC;grant No.41421002,41672188 and 41972200);the MOST Special Funds from the State Key Laboratory of Continental Dynamics。
Objective Rodinia was a supercontinent that comprised nearly all the current existing continents/blocks on Earth to form a coherent large landmass during the Meso-Neoproterozoic. Thus, discovery of Meso-Neoproterozoic...
financially supported by the National Natural Science Foundation of China (No.41872203);China Geological Survey (No.1212011120709);Doctoral Candidate Inter Discipline Fund of Jilin University (No.10183201837)
The paleoposition of North China Craton in Rodinia has long been in controversial. This paper mainly focuses on the U-Pb geochronological studies of detrital zircons obtained from Bayan Obo Group exposed in the Shangd...
financially supported by the Special Fund for the Land and Resources Scientific Research of Public Interest (201511020)
The geodynamic processes for the Neoproterozoic mafic-ultramafic intrusions and dykes in the Kuluketage region,Tarim Craton has also been debated for some time.Some researchers suggested that the Neoproterozoic
The late Archean Dharwar Craton is an important part of the Archean and Proterozoic terrains in Peninsular India.Dharwar Craton consists of Western and Eastern Blocks,separated by the Chitradurga Shear Zone.Eastern
part of the author's PhD project funded by the Australian government and the ministry of higher education of Egypt
Foliation inflexion/intersection axes (FIAs) preserved within porphyroblasts that grew throughout Isan orogenesis reveal significant anticlockwise changes in the direction of bulk horizontal shortening between 1670 ...
supported by National Science Foundation of China(40772123,40721063).
Neoproterozoic rifting-related mafic igneous rocks are widely distributed both in the northern and southern margins of the Tarim Block,NW China.Here we report the geochronology and systematic whole-rock geochemistry o...
supports from the National Natural Science Foundation of China(grants 40172071 and 40211120151 to Yan Quanren);the Ministry of Science and Technology of the People’s Republic of China(grant 2202CB412608 to Wang Zongqi);the China Geological Survey(grant DKD2001002 to Wang Zongqi);the University of Nevada Las Vegas(to Hanson);and the Geological Society of America(to Druschke)are gratefully appreciated.
The Bikou volcanic terrane is predominated by subalkaline tholeiitic lavas. Rock samples display lower initial ratios of Sr and Nd, 0.701248-0.704413 and 0.511080-0.512341 respectively. 207Pb and 208Pb are significant...