A tectonic model reconciling evidence for the collisions between India, Eurasia and intra-oceanic arcs of the central-eastern Tethys

AD Gibbons, S Zahirovic, RD Müller, JM Whittaker… - Gondwana …, 2015 - Elsevier
Despite several decades of investigations, inferences on the timing and nature of collisions
along the Mesozoic–Cenozoic Eurasian margin remain controversial. We assimilate …

Numerical modeling of subduction: State of the art and future directions

T Gerya - Geosphere, 2022 - pubs.geoscienceworld.org
During the past five decades, numerical modeling of subduction, one of the most
challenging and captivating geodynamic processes, remained in the core of geodynamic …

[HTML][HTML] Stagnant lids and mantle overturns: Implications for Archaean tectonics, magmagenesis, crustal growth, mantle evolution, and the start of plate tectonics

JH Bédard - Geoscience Frontiers, 2018 - Elsevier
The lower plate is the dominant agent in modern convergent margins characterized by
active subduction, as negatively buoyant oceanic lithosphere sinks into the asthenosphere …

Deep India meets deep Asia: Lithospheric indentation, delamination and break-off under Pamir and Hindu Kush (Central Asia)

SK Kufner, B Schurr, C Sippl, X Yuan… - Earth and Planetary …, 2016 - Elsevier
Subduction of buoyant continental lithosphere is one of the least understood plate-tectonic
processes. Yet under the Pamir–Hindu Kush, at the northwestern margin of the India–Asia …

The Himalaya in 3D: Slab dynamics controlled mountain building and monsoon intensification

AAG Webb, H Guo, PD Clift, L Husson… - …, 2017 - pubs.geoscienceworld.org
Tectonic models for the Oligocene–Miocene development of the Himalaya mountain range
are largely focused on crustal-scale processes, and developed along orogen-perpendicular …

The shape of the Himalayan “Arc”: An ellipse pinned by syntaxial strike-slip fault tips

L Jiao, P Tapponnier… - Proceedings of the …, 2024 - National Acad Sciences
Trans-Himalayan geodetic data show that, between both syntaxes, India/Asia convergence
is steadily oriented≈ N20° E. However, surface faulting near both syntaxes, along the 2005 …

Driving the upper plate surface deformation by slab rollback and mantle flow

P Sternai, L Jolivet, A Menant, T Gerya - Earth and Planetary Science …, 2014 - Elsevier
The relative contribution of crustal and mantle processes to surface deformation at
convergent plate margins is still controversial. Conflicting models involving either extrusion …

Slab breakoff: A critical appraisal of a geological theory as applied in space and time

E Garzanti, G Radeff, MG Malusà - Earth-Science Reviews, 2018 - Elsevier
The idea that prominent geological phenomena observed in the crust and at the surface may
be caused by the detachment of subducting dense lithosphere has been anticipated by …

Nonlinear viscoplasticity in ASPECT: benchmarking and applications to subduction

A Glerum, C Thieulot, M Fraters, C Blom… - Solid Earth, 2018 - se.copernicus.org
ASPECT (Advanced Solver for Problems in Earth's ConvecTion) is a massively parallel finite
element code originally designed for modeling thermal convection in the mantle with a …

Relict basin closure and crustal shortening budgets during continental collision: An example from Caucasus sediment provenance

E Cowgill, AM Forte, N Niemi, B Avdeev, A Tye… - …, 2016 - Wiley Online Library
Abstract Comparison of plate convergence with the timing and magnitude of upper crustal
shortening in collisional orogens indicates both shortening deficits (200–1700 km) and …