Lesson 14 overview

In part two of the exercises for the final two weeks of the course we will combine the thermochronometer age prediction code used last week with an age dataset from the Bhutan Himalaya to quantify the long-term rates of erosion recorded in the thermochronometer data. These results will be presented in detail in your Final paper description.

  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 13 and 14 lecture slides
  5. Exercise 14
  6. Exercise 14 hints
  7. Final paper description

Scientific journal articles