Wenjiao Xiao
Chinese Academy of Sciences
Publications 393
#1Xiaoliang Jia (CAS: Chinese Academy of Sciences)H-Index: 2
#2ZHAIMingguo (CAS: Chinese Academy of Sciences)H-Index: 59
Last.Yin Liu (CAS: Chinese Academy of Sciences)H-Index: 1
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Abstract The Taihua Complex is exposed mostly in the central-western part along the southern margin of the North China Craton (NCC). In this study, field geological, geochemical, LA-ICP-MS zircon U-Pb age dating and Lu-Hf isotopic analysis are applied to the orthorgneisses, felsic leucosomes, and granites of the Taihua Complex, in order to provide constraints on its crustal evolution from the Mesoarchean to Paleoproterozoic (ca. 2.9-1.8 Ga). The ca. 2.90-2.73 Ga magmatism was an important episod...
#1R.T. Ratheesh-Kumar (CUSAT: Cochin University of Science and Technology)
#2B.F. Windley (University of Leicester)H-Index: 24
Last.F.K. Zeba-Nezrin (CUSAT: Cochin University of Science and Technology)
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Abstract This study provides a new perspective into the Archean accretionary tectonic evolution of the Dharwar Craton and the adjacent high-grade granulite blocks of southern India. The necessary constraints for this tectonic assembly were derived using new petrochemical and zircon U-Pb age data from the granulite facies Biligiri Rangan Block (BRB), which occupies a central key position in the Archean collage of southern India. The BRB, composed largely of charnockites and mafic granulites, is a...
#1Rongguo ZhengH-Index: 4
#2Jin ZhangH-Index: 1
Last.Wenjiao Xiao (CAS: Chinese Academy of Sciences)H-Index: 60
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Abstract The Permian magmatism in the Alxa region provides critical geological evidence to constrain the geodynamic processes in the southern Central Asian Orogenic Belt. The Shouji batholith is located in the southern Langshan, eastern Alxa region, and contains monzogranites, K-feldspar granites, and gabbros. New zircon U Pb age data show that the Shouji batholith formed at 282–268 Ma. The Shouji granites have high (Na2O + K2O), Nb, and Zr contents, and high 10000*Ga/Al, FeOT/(FeOT + MgO), Yb/N...
Abstract Mafic dikes preserve a considerable amount of geological information about crustal evolution. Yanshanian granitoids and granitites are widespread in the southern margin of the North China Craton (NCC) and northern Qinling Orogenic Belt (NQOB), respectively. However, further study is required to resolve the many contrasting hypotheses relating to the mechanisms of petrogenesis and origins. The present study therefore reports on geochemical, geochronological, and Sr-Nd-Pb isotopic data fo...
#1Chunming HanH-Index: 33
#2Wenjiao Xiao (CAS: Chinese Academy of Sciences)H-Index: 60
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