Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
Abstract
Over the Earth’s evolutionary history, the style of plate subduction has evolved through time due to the secular cooling of the mantle. While continuous subduction is a typical feature of modern plate tectonics, a stagnant-lid tectonic regime with localized episodic subduction likely characterized the early Earth. The timing of the transition between these two subduction styles bears important insights into Earth’s cooling history. Here we apply...
Paper Details
Title
Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
Published Date
Jul 30, 2019
Journal
Volume
10
Issue
1
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