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6 FAQs about [Fanshan water storage project]
Where is the Fanshan deposit located?
The Fanshan deposit is located along the east side of the Wenzhou-Zhenhai Fault, in the Fanshan caldera basin, an Early Cretaceous 9 km-long, 6 km-wide elliptic-shaped basin (Fig. 1, Fig. 2 a). Abundant alunite, pyrophyllite, quartz, and minor topaz developed in the Fanshan district, which formed an 8-km 2 lithocap.
Which area is most proximal to the heat source of Fanshan basin?
Pingpengling area is the most proximal area to the heat source of Fanshan basin. The Fanshan alunite deposit, located in Cangnan County, Zhejiang Province, is the largest alunite deposit in China, which developed a lithocap with an extensive advanced argillic alteration.
Are there magmatic-hydrothermal centers in Fanshan lithocaps?
Two types of alunite have been identified by mineral chemistry. Efforts have been made to use the SWIR features and the mineral chemistry of alunite to vector to the possible magmatic-hydrothermal center in Fanshan, which could provide new insights to locating magmatic-hydrothermal centers for other lithocaps elsewhere.
Which Alunite is used to vector heat Center in Fanshan basin?
K-rich and Na-rich alunite have diagnostic Na/K value, Pos1480 and mineralogy. Pos1480 and ratios of Na/K, Rb/Sr*1000, etc. can be used to vector heat center. Pingpengling area is the most proximal area to the heat source of Fanshan basin.
What type of lithocap was developed in Fanshan district?
6. Conclusions The Fanshan district developed a typical lithocap, consisting of advanced argillic alteration. According to the results of SWIR reflectance spectroscopy, eight types of minerals: alunite, pyrophyllite, kaolinite, dickite, illite, phengitic muscovite, chlorite, and topaz —were identified.
Where is the Fanshan alunite deposit located?
Geology of the Fanshan alunite deposit The Fanshan deposit is located along the east side of the Wenzhou-Zhenhai Fault, in the Fanshan caldera basin, an Early Cretaceous 9 km-long, 6 km-wide elliptic-shaped basin (Fig. 1, Fig. 2 a).