Xian-Wu Bi

TL;DR: The Ailaoshan Gold Province, China is a series of gold deposits hosted on a 200-km segment of a major normal fault formed during Eocene extension as discussed by the authors, which is well characterised using conventional geochemical and microthermometric techniques, the results of which are consistent with a predominantly high temperature "magmatic" fluid present in the ore minerals.

TL;DR: In this paper, the authors studied the South China low-temperature metallogenic domain (LTMD), which includes an area of ∼500,000 km 2 in the Yangtze Block and is composed of the Chuan-Dian-Qian Pb-Zn, Youjiang Au-As-Sb-Hg and Xiangzhong Sb-Au mines.

TL;DR: In this article, the authors carried out molybdenite Re-Os and phlogopite and muscovite 40Ar/39Ar dating to better understand the timing and genesis of mineralization.

TL;DR: In this paper, He and Ar isotope analyses of four gold and four copper deposits in the Red River-Jinshajiang strike-slip fault zone are presented.

TL;DR: A mantle origin is consistent with the association of the deposits with mafic dikes and the 3He/4He ratios of ore-forming fluids (e.g., 0.10−2.02 Ra for the volcanic-hosted Xiangshan uranium deposit) as discussed by the authors.