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1
Introduction
2
Project Overview
3
Volcanic Record
4
convergent margin
5
Yellowstone plume
6
Time progressive volcanism
7
Types of volcanic rocks being interrupted
8
The 706 line
9
Subduction
10
High Lava Plains
11
Tomographic Results
12
Low Velocity
13
Models
14
Shearwave Splitting
15
Summary
16
Discussion
Description:
Explore the causes of continental intraplate volcanism in this 42-minute AGU Fall Meeting 2008 Bowen Lecture, focusing on the High Lava Plains of Eastern Oregon. Presented by Richard W. Carlson from the Carnegie Institution of Washington's Department of Terrestrial Magnetism, the lecture covers a comprehensive range of topics including the volcanic record, convergent margins, the Yellowstone plume, time-progressive volcanism, and various types of volcanic rocks. Delve into the intricacies of subduction, tomographic results, low velocity models, and shearwave splitting. Gain insights into the complex geological processes shaping the High Lava Plains region through this in-depth examination of volcanic activity and its underlying causes.

On the Causes of Continental Intraplate Volcanism - High Lava Plains of Eastern Oregon

AGU
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