Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Zhao-Ren Fu"'
Publikováno v:
Resource Geology. 53:89-100
The Liwu Cu-rich sulfide deposit occurs within the Jianglang dome in the eastern margin of the Tibetan plateau. The dome consists of a core, a middle slab and a cover sequence. The main deposit is hosted in the core with minor ore bodies in the middl
Publikováno v:
Journal of Structural Geology. 25:765-779
The Jianglang Tectonic Dome (JTD) lies on the eastern margin of the Tibetan Plateau and consists of three tectono-stratigraphic units separated by two extensional detachment faults: a schist complex, a middle ductile slab and an overlying sedimentary
Publikováno v:
Mineralium Deposita. 37:213-225
The early Tertiary Sanerlin uranium deposit is located near the southwestern margin of the Chaling–Yongxing pull-apart basin defined by the Chaling–Yongxing and Chenxian–Linwu sinistral strike-slip faults in southern China. The uranium ores are
Publikováno v:
Journal of Geodynamics. 32:333-354
The NNE-trending Hunan-Jiangxi strike-slip fault system (HJSFS) of southern China comprises three NNE-trending primary faults (the Anhua-Chengbu fault, the Chalin-Chenxian fault, and the Ganjiang fault) with associated NE- and NW-trending secondary f
Publikováno v:
Science in China Series D. 45:851
South China is the most important uranium producer in the country. Much of the Mesozoic-Cenozoic geology of this area was dominated by NNE-trending intracontinental strike-slip faulting that resulted from oblique subduction of the paleo-Pacific plate
Publikováno v:
BMC Urology; 9/15/2020, Vol. 20 Issue 1, p1-7, 7p
Publikováno v:
Resource Geology; Jun2003, Vol. 53 Issue 2, p89-100, 12p
Publikováno v:
Mineralium Deposita; Mar2002, Vol. 37 Issue 2, p213-225, 13p