David R. Lentz

TL;DR: In this paper, the authors present a new synthesis of the geological history of Greece as revealed by the varied igneous rocks, based on more than 30 years of fi eld and laboratory studies by the authors together with a synthesis of widely scattered published literature that has been written in many different languagues.

TL;DR: In this paper, empirical geochemical links between felsic volcanism, geotectonic environment, and extensional geodynamics have not been adequately documented so as to distill the fundamental relationships between these features and formation of volcanic-hosted massive sulphide (VHMS) mineralization.

TL;DR: In this paper, textural and compositional data of magnetite from the Chengchao iron deposit, Daye district, China to provide a better understanding in the formation mechanism and genesis of the deposit and shed light on analytical protocols for in-situ chemical analysis of hydrothermal magnetite.

TL;DR: In this paper, the halogen fugacity ratio contour lines are transected by the measured values of biotite composition; this suggests the fluid composition, fO2 and fS2 of the fluids, and reaction between wall rock and hydrothermal fluids play a key role in the resultant halogene fugacities recorded in biotites that are critical to interpreting metal complexing behaviour during magmatic-hydrothermal evolution.

TL;DR: Agua Rica is a world-class Cu (Mo-Au) deposit located in Catamarca, Argentina, in which the porphyry and high sulfidation epithermal stages are juxtaposed due to the telescoping of the mineralizing system as mentioned in this paper.