Imaging deep-mantle plumbing beneath La Réunion and Comores hot spots: Vertical plume conduits and horizontal ponding zones
M Dongmo Wamba, JP Montagner, B Romanowicz - Science advances, 2023 - science.org
Whether the two large low–shear velocity provinces (LLSVPs) at the base of Earth's mantle
are wide compact structures extending thousands of kilometers upward or bundles of distinct …
are wide compact structures extending thousands of kilometers upward or bundles of distinct …
Plume-driven recratonization of deep continental lithospheric mantle
Cratons are Earth's ancient continental land masses that remain stable for billions of years.
The mantle roots of cratons are renowned as being long-lived, stable features of Earth's …
The mantle roots of cratons are renowned as being long-lived, stable features of Earth's …
Continental mid‐lithosphere discontinuity: A water collector during craton evolution
Continental mid‐lithosphere discontinuity (MLD) seems to be ubiquitous beneath cratons
around the world with the dominant depth of 70–100 km, and is characterized by a shear …
around the world with the dominant depth of 70–100 km, and is characterized by a shear …
Lithospheric architecture and geodynamics of the Archean Dharwar craton and surrounding terranes: New insights from satellite gravity investigation
A Vasanthi, M Santosh - Gondwana Research, 2021 - Elsevier
The construction and destruction of continents, cratons and supercontinents on the globe
involved multiple events of plume, rifting, subduction-accretion, and collision through the …
involved multiple events of plume, rifting, subduction-accretion, and collision through the …
Multidisciplinary constraints on the abundance of diamond and eclogite in the cratonic lithosphere
Some seismic models derived from tomographic studies indicate elevated shear‐wave
velocities (≥ 4.7 km/s) around 120–150 km depth in cratonic lithospheric mantle. These …
velocities (≥ 4.7 km/s) around 120–150 km depth in cratonic lithospheric mantle. These …
Detailed configuration of the underthrusting Indian lithosphere beneath western Tibet revealed by receiver function images
We analyze the teleseismic waveform data recorded by 42 temporary stations from the Y2
and ANTILOPE‐1 arrays using the P and S receiver function techniques to investigate the …
and ANTILOPE‐1 arrays using the P and S receiver function techniques to investigate the …
Lithosphere structure in the collision zone of the NW Himalayas revealed by alocal earthquake tomography
In this study, we obtained new 3D seismic tomography models of the crust and uppermost
mantle beneath the northwestern Himalayas down to a depth of 120 km. The data were …
mantle beneath the northwestern Himalayas down to a depth of 120 km. The data were …
Influence of inherited Indian basement faults on the evolution of the Himalayan Orogen
L Godin, R Soucy La Roche, L Waffle… - Geological Society …, 2019 - lyellcollection.org
Indian basement faults, which bound three orogen-perpendicular palaeotopographic ridges
of Precambrian Indian basement south of the Himalaya, extend to the base of the Indian …
of Precambrian Indian basement south of the Himalaya, extend to the base of the Indian …
Clinopyroxene and garnet mantle cargo in kimberlites as probes of Dharwar craton architecture and geotherms, with implications for post-1· 1 Ga lithosphere thinning …
Abstract The Wajrakarur Kimberlite Field (WKF) on the Eastern Dharwar Craton in southern
India hosts several occurrences of Mesoproterozoic kimberlites, lamproites and ultramafic …
India hosts several occurrences of Mesoproterozoic kimberlites, lamproites and ultramafic …
Petrogenesis of Neoarchean (2.80–2.75 Ga) Jagannathpur volcanics and the Ghatgaon and Keshargaria dyke swarms, Singhbhum craton, eastern India …
Petrogenesis of Neoarchean dyke swarms and dispersed volcanic successions in the
Singhbhum craton can potentially constrain mantle heterogeneity. Their arc-like trace …
Singhbhum craton can potentially constrain mantle heterogeneity. Their arc-like trace …