Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Xingzhu Fan"'
Autor:
Depeng Yang, Yajing Zhang, Shahzad Bakht, Xingzhu Fan, Lu Yu, Fengyue Sun, Dongqian Wu, Liang Huo, Chenghan Xu, Yinqiang Sun
Publikováno v:
Canadian Journal of Earth Sciences. 59:135-155
The widespread Early Cretaceous plutons intruding along the southern Great Xing’an Range (SGXR) provide evidence for tectonic evolution of the region. Petrological, geochemical, zircon U–Pb geochronology, and zircon Hf isotopic studies are conduc
Publikováno v:
International Geology Review. 65:61-88
Publikováno v:
International Geology Review. 64:1270-1293
The volcanic rocks of the Elashan Formation provide important evidence for the Late Triassic post-collisional magmatism in the East Kunlun Orogenic Belt. This study focused on the geochronology, ge...
Publikováno v:
Resource Geology. 71:177-201
Autor:
Lu Yu, Fengyue Sun, Christoph Beier, Dongqian Wu, Liang Li, Li Wang, Guobiao Huang, Xingzhu Fan, Chenghan Xu
The Heihaibei gold deposit is a newly discovered gold deposit in the southern part of the Eastern Kunlun Orogenic Belt. Its most distinctive features are that the gold mineralization is hosted in monzogranite, and that the presence of pre-ore (possib
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ae5cf74d8467bb2eda4bb55617b4284c
http://hdl.handle.net/10138/343448
http://hdl.handle.net/10138/343448
Publikováno v:
International Journal of Earth Sciences. 109:1439-1461
Petrology, whole-rock geochemistry, in situ zircon U–Pb ages, and Lu–Hf isotopic data are reported for granodiorite and monzonitic granite samples from the Harizha Region in the eastern section of the East Kunlun Orogenic Belt. The results of the
Publikováno v:
Precambrian Research. 345:105761
Granitic magmatism related to the collisional orogenic belt provides important information for the evolution of continental crust. We performed petrological, geochemical and zircon U-Pb-Hf isotopic studies on four granitoid samples from the Guyang Ch
Publikováno v:
Lithos. :105159
Mafic–intermediate igneous rocks can provide important insights into the geodynamic evolution of orogenic belts. Here, we investigate the petrogenesis of mafic–intermediate intrusive igneous rocks in the East Kunlun Orogenic Belt (EKOB) to constr