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Abstract: Detrital Apatite Thermochronology of ODP sediments Reveals Mid-Pleistocene Decrease of Glacial Erosion Rates in the Mid-latitude Patagonian Andes (AGU25)

Detrital Apatite Thermochronology of ODP sediments Reveals Mid-Pleistocene Decrease of Glacial Erosion Rates in the Mid-latitude Patagonian Andes

Hongcheng Guo, Purdue University, Department of Earth, Atmospheric, and Planetary Sciences, West Lafayette, United States, Bethany Remian, Indiana University Bloomington, Department of Earth and Atmospheric Sciences, Bloomington, United States and Marissa M Tremblay, Purdue University, Department of Earth, Atmospheric, and Planetary Sciences, West Lafayette, IN, United States
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