The Huanglongpu carbonatite-related Mo ore field is located in the Lesser Qinling Orogenic belt in the southern margin of the North China block. The ore field is composed of six deposits, Yuantou, Wengongling, Dashigou, Shijiawan, Taoyuan and Erdaohe, all of which are genetically related to carbonatite dykes except for the Shijiawan deposit which is associated with a granitic porphyry. The Yuantou carbonatite dykes intruded into Archean gneiss and other carbonatites emplaced into Mesoproterozoic volcanic and sediment rocks. The carbonatites are mainly composed of calcite and variable amounts of quartz and K-feldspar and minor molybdenite. Re-Os dating of molybdenite from the Yuantou carbonatite yields a weighted average age of 225.0 +/- 7.6...
The Maoniuping REE deposit is a world-class deposit with 1.2 Mt of REO grading on average 2.89 wt.% ...
Although carbonatites potentially contain a larger concentration of rare earth elements (REEs) than ...
The Donggou Mo deposit in the eastern Qinling area, China, is a giant porphyry system discovered bas...
The Qinling molybdenum belt is a prominent metallogenic structure in central China hosting several s...
Carbonatites, usually occurring within intra-continental rift-related settings, have strong light ra...
The Eastern Qinling, Central China, containing more than 20 Mesozoic porphyry +/- skarn systems, is ...
Carbonatites are commonly related to the accumulation of economically valuable substances such as RE...
The South Qinling orogen in central China hosts carbonatites occurring as stocks associated with sye...
The Hunaglongpu carbonatites, Qinling Mountains, China, are exceptional as they form both an economi...
As a world-class molybdenum province, the Qinling orogenic belt is characterized by voluminous Mesoz...
The Qinling is an important orogenic belt, which formed by the joining of the North China and South ...
The East Qinling region in central China, hosting several tens of Mesozoicmagmatic-hydrothermal Mode...
The 1.85 Ga Longmendian Mo deposit in East Qinling is the oldest Mo system recognized in China. It i...
The Qinling is an important orogenic belt, which formed by the joining of the North China and South ...
The Maoniuping REE deposit is the second largest light rare earth elements deposit (1.45 million ton...
The Maoniuping REE deposit is a world-class deposit with 1.2 Mt of REO grading on average 2.89 wt.% ...
Although carbonatites potentially contain a larger concentration of rare earth elements (REEs) than ...
The Donggou Mo deposit in the eastern Qinling area, China, is a giant porphyry system discovered bas...
The Qinling molybdenum belt is a prominent metallogenic structure in central China hosting several s...
Carbonatites, usually occurring within intra-continental rift-related settings, have strong light ra...
The Eastern Qinling, Central China, containing more than 20 Mesozoic porphyry +/- skarn systems, is ...
Carbonatites are commonly related to the accumulation of economically valuable substances such as RE...
The South Qinling orogen in central China hosts carbonatites occurring as stocks associated with sye...
The Hunaglongpu carbonatites, Qinling Mountains, China, are exceptional as they form both an economi...
As a world-class molybdenum province, the Qinling orogenic belt is characterized by voluminous Mesoz...
The Qinling is an important orogenic belt, which formed by the joining of the North China and South ...
The East Qinling region in central China, hosting several tens of Mesozoicmagmatic-hydrothermal Mode...
The 1.85 Ga Longmendian Mo deposit in East Qinling is the oldest Mo system recognized in China. It i...
The Qinling is an important orogenic belt, which formed by the joining of the North China and South ...
The Maoniuping REE deposit is the second largest light rare earth elements deposit (1.45 million ton...
The Maoniuping REE deposit is a world-class deposit with 1.2 Mt of REO grading on average 2.89 wt.% ...
Although carbonatites potentially contain a larger concentration of rare earth elements (REEs) than ...
The Donggou Mo deposit in the eastern Qinling area, China, is a giant porphyry system discovered bas...