Accessibility Skip to Global Navigation Skip to Local Navigation Skip to Content Skip to Search Skip to Site Map Menu

GEOL274 Metamorphism and Metamorphic Mineralisation

Concepts and controls of metamorphism; chemical equilibrium and graphical portrayal of mineral assemblages; metamorphic grade and metamorphic facies; relationship between metamorphism and tectonics; New Zealand metamorphic rocks; metamorphic mineralisation.

This paper covers a spectrum of metamorphic types, including contact, regional and some of the metamorphic extremes, such as ultra-high-pressure and ultra-high-temperature. All types are discussed with reference to examples from around the world, although the focus is on the spectacular New Zealand geology. We will examine metamorphic reactions that take place in the shallow crust (e.g., in the zeolite facies) through to those that occur in the deep crust (e.g. in the eclogite facies), as well as those that occur in the largest metamorphic complex on Earth: the mantle. For metamorphic mineralisation, we will examine the formation of mesothermal gold deposits, massive sulphide deposits, skarns and diamond occurrences.

Paper title Metamorphism and Metamorphic Mineralisation
Paper code GEOL274
Subject Geology
EFTS 0.1500
Points 18 points
Teaching period Not offered in 2018, expected to be offered in 2019
Domestic Tuition Fees (NZD) $1,038.45
International Tuition Fees (NZD) $4,492.80

^ Top of page

GEOL 251
GEOL 374
Schedule C
GEOL 274 is for students in their second year of a geology or equivalent degree. GEOL 374 is for students in their third year of a geology or equivalent degree.
Teaching Arrangements
Two lectures and one 3-hour laboratory per week.
Fieldwork: 1 day field excursion to the Haast Schist occurring south of Dunedin.
Course outline
GEOL274-374-Metamorphism-syllabus-2015.pdf (latest syllabus indicative of content next time the paper is taught)
Teaching staff
Coordinator: Dr James Scott
Dr Steven Smith
Paper Structure
The paper is structured so that the lectures and labs are integrated.
The first two weeks are on contact metamorphism and skarns. This is followed by a section on regional metamorphism and then fault zone deformation and recrystallisation. The course progresses into geothermobarometry, and then into high pressure metamorphism in the crust and mantle. Assessment 40 % internal component, made up of a take home assignment and a practical test, with a 60 % final written exam. Assessments for GEOL374 are set and graded differently to GEOL274 to reflect greater background knowledge and higher expectations of students taking the paper at 300-level.
Text books are not required for this paper.
Graduate Attributes Emphasised
Global perspective, Interdisciplinary perspective, Lifelong learning, Critical thinking, Research, Self-motivation.
View more information about Otago's graduate attributes.
Learning Outcomes
To be able to reconstruct the metamorphic history of a rock, from the field to microscopic scale.

^ Top of page


Not offered in 2018, expected to be offered in 2019

Teaching method
This paper is taught On Campus
Learning management system