Subduction zone metamorphic pathway for deep carbon cycling: I. Evidence from HP/UHP metasedimentary rocks, Italian Alps

Volume: 386, Pages: 31 - 48
Published: Oct 29, 2014
Abstract
null null Metamorphosed Jurassic oceanic sediment in the Italian Alps experienced peak null P – T null conditions (1.5–3.0 GPa; 330–550 °C) similar to those experienced by sediments subducting through forearcs in most modern subduction zones. Integrated field, petrologic, and geochemical study of the devolatilization history of these rocks provides evidence regarding the extents of loss and mobility of oxidized and reduced C during subduction of...
Paper Details
Title
Subduction zone metamorphic pathway for deep carbon cycling: I. Evidence from HP/UHP metasedimentary rocks, Italian Alps
Published Date
Oct 29, 2014
Volume
386
Pages
31 - 48
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