Roger Taylor Boeken

This text concentrates upon field observations concerning leached cappings and gossans, occurring as oxidised surface expressions of underlying ore zones. Although the advent of modern multielement geochemical sampling and easier mechanical excavation assist considerably in subsurface interpretation, there are still many occasions where the first observation and recognition are made by the lone field geologist. New exposures continue to be found in remote and often difficult terrains, where “on the spot” skills are of prime importance. In general terms the text has been arranged from the broad scale to the specific, and it should be realised that all scales provide valuable input for final interpretation. The topics covered include: • Theoretical perspectives • Initial recognition • General field observations • Detailed field observations (secondary minerals, boxworks) • Porphyry copper leached cappings

This text reflects forty years of the author's journey to understand ore textures, beginning with a lack of preparation after leaving academia. The learning process has been gradual and remains ongoing. Initial confusion arose from the challenge of interpreting mineralizing processes through field observations. Enlightenment came through several key experiences: working as a mine and exploration geologist, visiting various ore deposit styles as both an academic and consultant, addressing questions from generations of students, conducting research, and collaborating with esteemed economic geologists. Professor Willard C. Lacy played a pivotal role by demonstrating the importance of fundamental principles regarding fluid channelways and the careful observation of textures. Despite rapid technological advancements, these skills are essential for both exploration geologists and academic researchers focused on ore-forming processes. Over eleven years, five volumes were compiled, each designed to guide observers through the principles of recognition related to infill, alteration, overprinting, and ore-related breccias.

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