This textbook is a complete rewrite, and expansion of Hugh Rollinson's highly successful
1993 book Using Geochemical Data: Evaluation, Presentation, Interpretation. Rollinson and …

Fluid evolution is an essential subject in the studies of hydrothermal ore-forming processes.
Garnet and scheelite prevail in W-bearing skarn deposits and record plentiful information on …

This contribution presents an application of principal component analysis (PCA) and K-
means clustering as tools for data dimension reduction and grou** of multivariate, whole …

Diverse fluid sources and complex fluid flow paths in skarn systems appear to be well
documented. Nevertheless, in situ microanalysis of oxygen isotopes by secondary ion …

Recent exploration has identified a series of Cu-Mo skarn deposits within the Xuancheng-
Magushan orefield. The orefield forms part of the Nanling-Xuancheng mining district, which …

Fluid-driven contact metamorphism in the Gangdese Arc, resulting from Late Cretaceous
intrusions, led to a diverse range of aureoles in carbonate sequences in southern Tibet …

Lode gold deposits, which are currently the world's major gold supply, have been shown to
be generated mostly by phase separation of metamorphic fluids and/or interaction between …

In response to westward subduction of the Paleo-Pacific, the North China Craton
experienced the uplift of an eastern coastal plateau followed by subsidence in the Early …

Garnet U‐Pb dating by laser ablation‐inductively coupled plasma‐mass spectrometry
requires the development of matrix‐matched reference materials of variable chemistry and U …

Scheelite (CaWO4) is an economically important W mineral in skarns that form when
magmatic fluids exsolved from a granitic intrusion react with carbonate wall rocks. In the …