The subduction plate interface: Rock record and mechanical coupling (from long to short timescales)

P Agard, A Plunder, S Angiboust, G Bonnet, J Ruh - Lithos, 2018 - Elsevier
Short-and long-term processes at or close to the subduction plate interface (eg, mineral
transformations, fluid release, seismicity and more generally deformation) might be more …

Boron isotopes as a tracer of subduction zone processes

JCM De Hoog, IP Savov - Boron isotopes: The fifth element, 2018 - Springer
This chapter reviews recycling of boron (B) and its isotopes in subduction zones. It discusses
the profound changes in B concentrations and B isotope ratios of various materials involved …

The water and fluid-mobile element cycles during serpentinite subduction. A review

M Scambelluri, E Cannaò… - European Journal of …, 2019 - pubs.geoscienceworld.org
The key role of serpentinites in the global cycles of volatiles, halogens and fluid-mobile
elements in oceans and in subduction zones is now ascertained by many studies …

Mafic slab melt contributions to Proterozoic massif-type anorthosites

DS Keller, CTA Lee, WH Peck, BD Monteleone… - Science …, 2024 - science.org
Massif-type anorthosites, enormous and enigmatic plagioclase-rich cumulate intrusions
emplaced into Earth's crust, formed in large numbers only between 1 and 2 billion years …

Fluid-mobile elements in serpentinites: Constraints on serpentinisation environments and element cycling in subduction zones

D Peters, A Bretscher, T John, M Scambelluri, T Pettke - Chemical geology, 2017 - Elsevier
Fluid-mobile element (FME) systematics in serpentinites are key to unravel the environments
of mantle rock hydration, dehydration, and element recycling in subduction zones. Here we …

[HTML][HTML] Fluid-mediated element cycling in subducted oceanic lithosphere: The orogenic serpentinite perspective

T Pettke, A Bretscher - Earth-Science Reviews, 2022 - Elsevier
Serpentinites are central to water (re) cycling in subduction zones and thus effect fluid-
mediated element transfer between the hydrosphere and the Earth's mantle and back into …

Complexity of graphite formation in response to metamorphic methane generation and transformation in an orogenic ultramafic body

A Boutier, I Martinez, O Sissmann, S Agostini… - … et Cosmochimica Acta, 2024 - Elsevier
The fate of carbon in subduction is explored by considering fluid-rock interactions in a body
of metamorphosed ultramafic rocks from the Appalachian belt as potential proxies for …

Carbonate transfer during the onset of slab devolatilization: New insights from Fe and Zn stable isotopes

B Debret, P Bouilhol, ML Pons, H Williams - Journal of Petrology, 2018 - academic.oup.com
Long-term carbon cycling is a subject of recent controversy as new mass balance
calculations suggest that most carbon is transferred from the slab to the mantle wedge by …

Aqueous fluids are effective oxidizing agents of the mantle in subduction zones

K Iacovino, MR Guild, CB Till - Contributions to Mineralogy and Petrology, 2020 - Springer
Aqueous fluids produced by dehydration of the downgoing slab facilitate chemical exchange
in subduction zones, but the efficiency of fluid-mediated redox transfer as a mechanism to …

Geochemical constraints on the origin and tectonic setting of the serpentinized peridotites from the Paleoproterozoic Nyong series, Eseka area, SW Cameroon

P Nga Essomba Tsoungui, S Ganno… - Acta Geochimica, 2020 - Springer
Serpentinized rocks closely associated with Paleoproterozoic eclogitic metabasites were
recently discovered at Eseka area in the northwestern edge of the Congo craton in southern …