[HTML][HTML] Atlas of the underworld: Slab remnants in the mantle, their sinking history, and a new outlook on lower mantle viscosity

DG Van der Meer, DJJ Van Hinsbergen, W Spakman - Tectonophysics, 2018 - Elsevier
Across the entire mantle we interpret 94 positive seismic wave-speed anomalies as
subducted lithosphere and associate these slabs with their geological record. We document …

A Cenozoic Record of Deep Oceanic Zn Isotopic Composition in Ferromanganese Crusts

M Zhao, N Planavsky, X Wang, Y Zhang… - American Journal of …, 2023 - ajsonline.org
Water plays a critical role in erosion and sediment transport and this relationship is most
evident in the hyperarid Atacama Desert of Northern Chile, a region characterized by …

Ophiolites and their origins

Y Dilek, H Furnes - Elements, 2014 - pubs.geoscienceworld.org
Ophiolites are suites of temporally and spatially associated ultramafic, mafic, and felsic rocks
that are interpreted to be remnants of ancient oceanic crust and upper mantle. Ophiolites …

Zagros orogeny: a subduction-dominated process

P Agard, J Omrani, L Jolivet, H Whitechurch… - Geological …, 2011 - cambridge.org
This paper presents a synthetic view of the geodynamic evolution of the Zagros orogen
within the frame of the Arabia–Eurasia collision. The Zagros orogen and the Iranian plateau …

Forced subduction initiation recorded in the sole and crust of the Semail Ophiolite of Oman

C Guilmette, MA Smit, DJJ van Hinsbergen… - Nature …, 2018 - nature.com
Subduction zones are unique to Earth and fundamental in its evolution, yet we still know little
about the causes and mechanisms of their initiation. Numerical models show that far-field …

Cretaceous–Tertiary convergence and continental collision, Sanandaj–Sirjan zone, western Iran

M Mohajjel, CL Fergusson, MR Sahandi - Journal of Asian Earth Sciences, 2003 - Elsevier
The Sanandaj–Sirjan Zone contains the metamorphic core of the Zagros continental
collision zone in western Iran. The zone has been subdivided into the following from …

Birth, death, and resurrection: The life cycle of suprasubduction zone ophiolites

JW Shervais - Geochemistry, geophysics, geosystems, 2001 - Wiley Online Library
Suprasubduction zone (SSZ) ophiolites display a consistent sequence of events during their
formation and evolution that suggests that they form in response to processes that are …

Structure and geochemistry of Tethyan ophiolites and their petrogenesis in subduction rollback systems

Y Dilek, H Furnes - Lithos, 2009 - Elsevier
Suprasubduction zone (SSZ) ophiolites in orogenic belts represent oceanic crust generation
in subduction rollback cycles during the closing stages of basins prior to terminal continental …

Tectonic setting, origin, and obduction of the Oman ophiolite

M Searle, J Cox - Geological Society of America Bulletin, 1999 - pubs.geoscienceworld.org
The Semail ophiolite in the Oman Mountains is the world's largest and best preserved thrust
sheet of oceanic crust and upper mantle (> 10 000 km2,∼ 550 km long,∼ 150 km wide); it …

Synchronous formation of the metamorphic sole and igneous crust of the Semail ophiolite: New constraints on the tectonic evolution during ophiolite formation from …

M Rioux, J Garber, A Bauer, S Bowring… - Earth and Planetary …, 2016 - Elsevier
Abstract The Semail (Oman–United Arab Emirates) and other Tethyan-type ophiolites are
underlain by a sole consisting of greenschist-to granulite-facies metamorphic rocks. As …