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Iron isotope constraints on the genesis of giant Beiya Au-base

The Beiya Au-base metal deposit in southwest China is characterised by a huge amount of iron associated with gold mineralization. The formation of the Beiya deposit is

Why is geophysical imaging of the Beiya conductor important?

Thus, further high-resolution geophysical imaging of the shallow structures surrounding the Beiya conductor is needed. The Beiya porphyritic polymetallic deposit is an important gold deposit in the Jinshajiang-Ailaoshan metallogenic belt.

Energy storage techniques, applications, and recent trends: A

Energy storage provides a cost-efficient solution to boost total energy efficiency by modulating the timing and location of electric energy generation and consumption. The

What pore space is required to produce the resistivity of Beiya conductor?

The corresponding pore space required to produce the resistivity of the Beiya conductor (1–3 Ωm) is 1–3 vol% (Figure 6 ). Possible explanations for the low resistivity of the Beiya conductor are discussed above.

What is the mineralization pattern at the Beiya deposit?

The mineralization at the Beiya deposit shows a zoned pattern that changes from the center of the porphyries to country rocks, that is, from Cu-Mo-Au-porphyry mineralization to skarn Au-Cu-Fe mineralization to epithermal Au-Cu and Pb-Zn-Ag mineralization (W. C. Li et al., 2016 ).

Could a cooled Beiya magma chamber provide radioactive heat?

The cooled Beiya magma chamber could provide radioactive heat for the geothermal observations. Magma chambers in active magmatic events should be highly conductive because of partial melts and high temperature (Cordell et al., 2018 ).

Heterogeneous effects of battery storage deployment strategies

Battery storage is critical for integrating variable renewable generation, yet how the location, scale, and timing of storage deployment affect system costs and carbon dioxide

Does the Beiya deposit have a magma chamber?

Previous studies suggested the presence of a magma chamber during the formation of the Beiya deposit, which include: (a) It was demonstrated that the ore-forming fluids of the Beiya deposit was a supercritical fluid exsolved from a magma chamber (He et al., 2017 ).

Nature and evolution of fluid inclusions in the Cenozoic Beiya gold

The Beiya Au deposit in the Sanjiang metallogenic belt, Southwest China, is one of the largest Au deposits in China. It has proven reserves of more than 370 tons (t) of Au with

Is the Beiya deposit dominated by a hydrothermal magmatic system?

However, the latest volcanism in the study area was dated as 3.7 Ma (He et al., 2013) and melts are likely no longer present in the crust. Nevertheless, the formation of the Beiya deposit was dominated by a hydrothermal magmatic system.

About Beiya kunhou energy storage

About Beiya kunhou energy storage

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