Warning: This document is for an old version of IntroQG. The main version is master.

Lesson 6 overview

This week we will be introduced to the geochronological dating method called thermochronology. Thermochronology can be used to determine the time since rocks at the surface were at a given temperature in the Earth, and combines several of the equations we have already seen earlier in the course. This will be the topic of the final two weeks of the course, as well as the final paper you will write.

  1. Basic concepts of thermochronology lecture slides
  2. Low-temperature thermochronology lecture slides (not presented in class)
  3. Quantifying erosion with thermochronology lecture slides (not presented in class)
  4. Overview of Exercises 6 and 7 lecture slides
  5. Exercise 6
  6. Final paper description

Scientific journal articles

Lesson video

Lesson 6 - Thermochronology I

Dave Whipp, University of Helsinki @ Quantitative Geology channel on Youtube.