Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Tai-Yi Luo"'
Publikováno v:
Ore Geology Reviews. 69:403-416
Gejiu is geographically located near Gejiu city, SW China. It is one of the largest tin-polymetallic districts in the world and contains approximately 3 million tons (Mt) of Sn and smaller quantities of Cu, Pb, and Zn. The deposit primarily yields th
Publikováno v:
Economic Geology. 110:1643-1652
The black shale in the Lower Cambrian Niutitang Formation, southwest China, which has been dated to 532.3 ± 0.7 Ma by U-Pb radiometric measurements, hosts a sedimentary layer with abnormally high Ni-Mo-PGE-Au contents. This layer is enriched in Ni (
Autor:
Tai-Yi Luo, Xing-Chun Zhang, Chao Li, Zhilong Huang, Qiuyue Huang, Cheng-Biao Leng, De-Yun Ma, Shou-Xu Wang, Wenbo Li
Publikováno v:
Economic Geology. 110:557-574
The Diyanqinamu porphyry Mo deposit in the southern Greater Khingan Range of the Central Asian orogenic belt contains 800 million metric tons (Mt) of ore with an average grade of 0.097% molybdenum. The deposit is hosted in Late Jurassic volcanic rock
Publikováno v:
Ore Geology Reviews. 63:374-387
Publikováno v:
Ore Geology Reviews. 63:1-8
In the western Yangtze Block, southwest China, there are many hydrothermal native copper ore deposits and Zn–Pb ore deposits. All of these hydrothermal ore deposits are spatially associated with the Permian Emeishan flood basalts (EFBs), although t
Publikováno v:
Ore Geology Reviews. 60:112-125
The Gongchangling BIFs are located in the Anshan–Benxi area, northeastern part of the North China Craton, of which the No. 2 mining area is the largest and most typical high-grade iron ore producing area in China. In this study, the mineralogy, pet
Publikováno v:
Journal of Geochemical Exploration. 136:65-75
The petrography, as well as major and trace element (including rare earth element) compositions of plagioclase amphibolites and schists from the Anshan Group in the Qidashan and Gongchangling iron deposits, the western Liaoning Province, have been in
Publikováno v:
International Geology Review. 45:471-477
The Emeishan flood basalt is a large igneous province (LIP) erupted in southwestern China during the Permian Triassic period. Seismic images of the deep crustal structure beneath the Emeishan large igneous province (ELIP) indicate unusually high seis
Publikováno v:
Economic Geology & the Bulletin of the Society of Economic Geologists; Sep/Oct2015, Vol. 110 Issue 6, p1643-1652, 10p
Autor:
CHENG-BIAO LENG, XING-CHUN ZHANG, ZHI-LONG HUANG, QIU-YUE HUANG, SHOU-XU WANG, DE-YUN MA, TAI-YI LUO, CHAO LI, WEN-BO LI
Publikováno v:
Economic Geology & the Bulletin of the Society of Economic Geologists; Mar/Apr2015, Vol. 110 Issue 2, p557-574, 18p