finational supported by the Foundation of Science,Technology and Innovation Funding Authority(STDF)(Award Number:47106;Recipient:Mokhles K K.Azer)。
Leucogranite,pegmatite,and aplite from selected areas in the Wadi El Gemal area in the southern Eastern Desert of Egypt were investigated geochemically for their petrogenesis.These rocks represent a significant episod...
support from Australian Research Council grant FL160100168;supported by the National Institute of Science and Technology for Tectonic Studies(INCT)of Brazil。
The Alto MoxotóTerrane of the Borborema Province presents a wide exposure of Paleoproterozoic crust,but unlike other continental blocks of South America,its orogenic history is strongly obliterated by late Neoprotero...
financially supported by the Qinghai Science and Technology Department(Grant No.2016-ZJ752);Qinghai Salt Lake Industry(Grant No.E050DZ0801)。
The Qilian Block(QB)is a Precambrian micro-continent located in the northeastern Qinghai–Tibet Plateau.Prevalent Lower Paleozoic granitic magmatic rocks crop out in the QB.A new integrated study of zircon U-Pb ages a...
supported by China Geological Survey Development Research Center Program(Grant No.DD2016005234);Geological exploration fund Program of Jiangxi Province(Grant No.20160010);Jiangxi Bureau of Geology&Mineral Exploration Program(Grant No.201698)。
The Pengshan Sn-polymetallic ore field is located in the southeastern part of the Yangtze block,spanning the southeast edge of the MLYDZ and the northern edge of the mid-segment of the Jiangnan Uplift,and on one side ...
The geology,geochemistry of Iroko-granites have been studied and reported in this paper.The study area has been described as of Archaean-Early Proterozoic terrain underlain by migmatite-gneiss-quartzite complex with s...
financially supported by China Geological Survey(grant no.12120113095700,12120101000015001108);the National Science Foundation of China(grant no.41403039);the training program for young and middle aged backbone teachers of Chengdu Universcechnology(grant no.KYGG201502)
Cu–Au mineralization is rare in the Jurassic–Early Tertiary batholiths related to the India–Asia collision. Geochemical analysis and U–Pb isotope chronology was carried out on Shuangbujiere biotite hornblende gran...
Magba granitoids are made up of granites, orthogneiss, migmatites, metagabbro, mafic dykes and mylonites with respectively porphyritic, porphyroblastic, grano-lepido-porphyroblastic, and cataclastic texture. Mafic dyk...
A series of Ni-Cu sulfide deposits hosted in Early Permian mafic-ultramafic complexes occur along the -500 km long linear Huangshan-Jingerquan belt in the East Tianshan at the southern margin of the Central Asian Orog...
supported by the National Natural Science Foundation of China (Nos. 40372094 and 49972067)
The sub-vertical meso-and micro-structures and fabrics developed in coesite-bearing foliated eclogites in the Taohang (桃行) area, southeastern Shandong (山东), China. The diagnostic structures and fabrics, includ...
the National Natural Science Foundation of China (GrantNo.40334037);the Fund for Creative Research Groups (Grant No.40521001)
The Tiefosi granitic pluton is located 5 km northwest of Xinyang City, northern Dabie Orogen, and was emplaced in the Proterozoic Qinling Group. SHRIMP zircon U-Pb dating suggests its crystallization at 436 ± 11 Ma. ...