Join the Presentation
Scan to join.
Date & Time: Friday, June 17, 2022 @ 4:00 PM
Location: WERI Room 105 (Conference Room)
Zoom Meeting Link: https://us06web.zoom.us/j/82234297885
Meeting ID: 822 3429 7885
About the Presentation
The Pacific Plate, Earth’s largest tectonic plate, is currently subducting westwards below the Philippine Sea Plate at the Izu-Bonin-Mariana subduction zone. Subduction here started about 52 million years ago. Since about that time, the motion of the Pacific Plate has been towards the northwest, but before this time it was moving towards the north. This has led geologists to suggest that the major change in plate motion of the Pacific Plate was caused by the start of subduction at the Izu-Bonin-Mariana subduction zone. In addition, it is thought that this change in plate motion is related to, or even the cause of, a
change in motion of all major tectonic plates across the globe, also called a global plate reorganization.
To test whether the start of the Izu-Bonin-Mariana subduction zone indeed caused the change in Pacific Plate motion, we need to know the nature and orientation of the Izu-Bonin-Mariana plate boundary before it became a subduction zone. The subduction zone is currently oriented more or less N-S, but some say it was rotated up to 90 degrees clockwise since its formation, while others suggest that is has always been oriented N-S. The aim of the current study is to solve this debate.
To know the orientation of the plate boundary at time of subduction initiation, we use paleomagnetism. In paleomagnetism we measure the ancient magnetic field that is stored in magnetic minerals of rocks and compare it with the current magnetic field. The difference between these two constrains the rotation of a rock. Guam is located right on top of the Izu-Bonin-Mariana subduction zone, and exposes rocks that span its entire existence. Suzanna is now on Guam to sample rocks, with the aim to use paleomagnetism to constrain the rotation of the island through time, and hence the rotation of the subduction zone. This allows for the reconstruction of the plate boundary back to its orientation at the time of subduction
initiation, and thus allows us to reconstruct whether it is possible that the start of subduction caused a change in Pacific Plate motion.
About the Presenter
Suzanna van de Lagemaat is a geologist and PhD student at Utrecht University in the Netherlands. In her PhD, she studies plate tectonics and makes reconstructions of the motion of tectonic plates through time. The most interesting regions for these plate tectonic reconstructions are intensely deformed plate boundary zones, mostly those related to subduction zones. Suzanna’s research is focused on plate tectonic reconstructions of the south and west Pacific. She previously published papers on the tectonic history of the Scotia Sea and the SW Pacific, and did paleomagnetic and geochemical research on the North Island of New Zealand. Now it is time to make a new reconstruction of the West Pacific region, which is the reason why she is on Guam to do geological fieldwork. In this presentation, she will give a brief overview of plate tectonics and why we study it in the first place. Then she will give an explanation of why doing geological fieldwork on Guam might help solve a question that is relevant for global plate tectonics.