Abstract The Chating Cu–Au deposit is a newly discovered porphyry-type deposit within the
Nanling–Xuancheng mining district of the Middle–Lower Yangtze River Metallogenic Belt …

The porosity structures of a permeable rock can have remarkable effects on pore-fluid flow
within the rock. According to the modern mineralization theory, the mineralization pattern in …

The trend surface analysis (TSA) and the spectrum–area (S–A) multifractal model are two
popular methods to identify geochemical anomalies. In this study, the robust principal …

Hydrothermal ore‐forming systems usually involve coupled processes among pore‐fluid
flow, heat transfer, mass transport and chemical reactions in fluid‐saturated porous media …

The formation of the world‐class, high‐grade unconformity‐related uranium deposits in the
Athabasca Basin (Canada) requires circulation of large amounts of fluids, the mechanisms …

The occurrence of either scheelite (CaWO 4) or wolframite ([Fe, Mn] WO 4) in tungsten
deposits is generally explained by the Ca content of the host rocks, but scheelite/wolframite …

Based on the particle simulation method, a thermo-mechanical coupling particle model is
proposed for simulating thermally-induced rock damage. In this model, rock material is …

Various fluid-flow models have been suggested for the formation of unconformity-type
uranium deposits in the Athabasca basin, including fluid flow driven by fluid overpressure …

Finding new, effective predictive variables for 3D mineral prospectivity modeling is both
important and challenging. The 3D ore-forming numerical modeling quantitively …

Abstract The Hutouya Pb-Zn deposit located in Qinghai, China, is a typical skarn-type
polymetallic deposit in the Qimantage metallogenic belt. This belt is characterized by …