financially supported by the Ministry of Science and Technology of China(State Key Research Project No.2017YFC0601302);the Chifeng Chaihulanzi Gold Mining Co.Ltd.(Shandong Gold Group)。
The Chaihulanzi area in eastern Inner Mongolia is tectonically situated on the northern margin of the North China Craton(NCC). The main Precambrian lithologies of the area have been referred to the Archean Jianping Gr...
the financial support from the UGC CAS-I & II grant;DSTs New Delhi for financial assistance to MJ. BPD
The chemical and petrological correlation of metamorphic nappes and klippes overlying the Proterozoic sedimentary units in the Kumaun Himalaya is still debated. The Ramgarh and Almora gneisses, not previously distingu...
supported by the National Science Foundation of China(grants No.41272213,41572177,41573023,41502193 and 41272222)
The Qinling Orogenic Belt(QOB)is a composite continental orogenic belt that has experienced many tectonic events.The QOB is subdivided into the following three litho-tectonic units:the North Qinling terrane,the Middle...
financially supported by the National Science Foundation of China(grants No.41430207 and 90914001)
Objective The North China Craton,bounded by the Paleozoic Central Asian Orogenic Belt on the north and by the Qinling–Dabie–Su–Lu Orogenic Belt on the south,is one of the oldest continental nuclei on Earth as a con...
supported by the National Science Foundation of China(grant No.41272223);China Geological Survey(grants No.12120114028001,121201004000150017-28 and 121201004000160901-7);Graduate Innovation Fund of Jilin University
Objective The North China Craton(NCC)is almost continuously widespread TTGs of 3.8–2.5 Ga,and the intrusive peak appears at^2.53 Ga,indicating that the Neoarchean is the most important period of continental growth ...
financially supported by National Natural Science Foundation of China (NO.41390451 and NO.41172101);Science and technology research projects of China Coal Geological Bureau (2013-I-03);basic geological survey project of China Geological Survey (12120114083001)
Qinling orogen is one of the five main repository distribution provinces of large scale graphite resources. Graphite occurrence strata are multitudinous including NeoArchaean group to Neopaleozoic. Mineral deposit typ...
supported by the National Natural Science Foundation of China(41302080,41272220);the China Geological Survey Project(1212011121091,12120114009401);the Fundamental Research Funds for the Central Universities(53200959380);the Key Project of the National Twelve Five Year Research Program of China(2011BAB04B05)
The tectonic evolution of South Qinling, which is a main part of the Qinling orogenic belt, is still in dispute and deformation history of South Qinling is poorly studied. In this paper, detailed structural, microstru...
supported by the China Geological Survey (nos. 1212011120129,1212010811033,and 1212011120152);the National Natural Science Foundation of China (no. 41072053)
The albite rim is present in most felsic gneisses of the Fuping Complex. The presence of the rim indicates the coexistence of plagioclase and K-feldspar in the rock. The rim is formed immediately after the myrmekite, ...
This study was supported by the Ministry of Land and Resources of China Projects“1:250000 Regional Geological Surveyofthe Lianyugang Sheet (150C002004) of P.R.China";"Geological Research for Selecting a Drillhole in the Donghai TargetArea of the Chinese Continental Scientific Drilling Programme”.
Study of micro-area chemical compositions indicates that phengite in albite gneiss from hole ZK2304 of the Donghai region has evident compositional zoning. SiO2 and tetrahedrally coordinated Si contents decrease, and ...
In the gneisses from the drillhole ZK2304 of the Donghai area, there have been preserved high- and ultrahigh-pressure metamorphic mineral assemblages, a series of complicated retrogressive textures and relevant metamo...