supported by National Natural Science Foundation of China (41702196, 41530208, 41502051 and 41402064);the National Key Research and Development Program of China (2016YFC0601002);Special Fund for Basic Scientific Research of Central Colleges, Chang’an University, China (310827172201)
Reconstruction of pressure-temperature-time(P-T-t)paths and thermal regimes are essential for inferring tectono-metamorphic processes involved in the formation of metamorphic terranes.However,the P-T information,espec...
financially supported by the National Nature Science Foundation of China (41202032, 412111062 and 41311120071)
The first Archean eclogite was announced from the Salma and Gridino complexes of Belomorian Province(Russia)in Fennoscandian Shield(Fig.1a)[1]that has aroused quite a resonance worldwide from all aspects;the debates o...
supported by the Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX2-YW-153);the National Natural Science Foundation of China (40625006);the Fundamental Research Funds for the Central Universities (2011QNA04)
Palaeoproterozoic 全球冻结成冰(2.3 Ga ) 可以是地球历史上的第一个雪球地球事件。诺思中国暴露得好沉积存款这次有最小的 postdepositional 的时期改变。一个冻结成冰事件的沉积证据然而一直在缺乏。这里,我们在 Wutai 山区分析了 P...
supported by the International Cooperation Project of the Ministry of Science and Technology of China (2007DFA21230);the Natural Science Foundation of Hubei Province (2009CDA004);the National Training Foundation of Geological Science Base (J083520);the National Innovation Experiment Program for University Students (1320311009);part of a Higher Education Key Project of Hubei Province (2009108)
The Huashanguan rapakivi pluton in Zhongxiang,Hubei Province,China,is the first discovered Proterozoic rapakivi pluton in the Yangtze block.Based on field and petrographical observations,a typical rapakivi texture was...
supported by the Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China (J0721 and J0907);National Commission on Stratigraphy of China (1212010511702-01);China Geological Survey (1212010611801)
Basalt and basaltic andesite metamorphosed at greenschist facies occurs with conglomerate layers at the bottom of the Paleoproterozoic Hutuo Group in the Wutai Mountains area, North China Craton. Detailed geological s...
Supported by the Key Program of National Natural Science Foundation of China (Grant No. 90814000)
Much attention has been paid in the last two decades to the physical and chemical processes as well as temporal-spatial variations of the lithospheric mantle beneath the North China Craton. In order to provide insight...
Supported by National Natural Science Foundation of China (Grant No. 40873004);Special Funds for National Scientific Research of Commonweal Industries;the Ministry of Land and Resources of China (Grant No. 2008110015);Opening Foun-dation of State Key Laboratory of Continental Dynamics;Northwest University (Grant No. 06LCD12);the Project of Land and Resources Bureau of Zhejiang Province (Grant No. 2004005)
A combined study of zircon LA-ICP-MS U-Pb dating, trace elements and Hf isotope was carried out for gneissic granite from the Sanzhishu area in Jingning, SW Zhejiang Province. Nearly all the zircons separated from the...
Supported by National Natural Science Foundation of China (Grant Nos. 40772042, 90714010 and 40521001);the Ministry of Education of China (Grant Nos. IRT0441, B07039 and NCET-06-0659);Foundation of the State Key Laboratory of Continental Dynamics, Northwest University
Mafic dyke is a sign of regional extension, and thus has important tectonic significance. A great amount of mafic dykes occur in the Kongling terrain of the Yangtze Craton, which have great bearing on the early evolut...
Supported by National Natural Science Foundation of China (Grant Nos. 90714002 and 40772042) ;National Basic Research Program of China (Grant No. 2006CB403502)
Zircon U-Pb age and Hf isotope, and major and trace element compositions were reported for granite at Quanyishang, which intruded into the Kongling complex in Yichang, Hubei Province. The results show that the Quanyis...