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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
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Cape Verde Islands (1)
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Central Africa
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Lake Kivu (1)
-
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East Africa
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Afar Depression (1)
-
Ethiopia (2)
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Ethiopian Rift (2)
-
Kenya (1)
-
Tanzania (2)
-
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East African Lakes
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Lake Kivu (1)
-
-
East African Rift (2)
-
Madagascar (1)
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Mozambique Belt (1)
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North Africa
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Algeria
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Constantine Algeria (1)
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Guelma Algeria (1)
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Atlas Mountains
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Moroccan Atlas Mountains
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Middle Atlas (1)
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Egypt (2)
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Morocco
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Moroccan Atlas Mountains
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Middle Atlas (1)
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Nubian Shield (1)
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Southern Africa
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Kaapvaal Craton (2)
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Namaqualand (1)
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South Africa
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KwaZulu-Natal South Africa (1)
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West Africa (2)
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West African Craton (1)
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Zimbabwe Craton (1)
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Altiplano (2)
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Mediterranean region
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Mexico
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Old Faithful Geyser (1)
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Pacific Ocean
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North Pacific
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South Pacific
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Southern Ocean
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upper Cenozoic (1)
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Paleozoic
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lower Paleozoic (1)
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upper Precambrian
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Proterozoic
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igneous rocks
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metamorphic rocks
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Primary terms
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Africa
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East Africa
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Ethiopian Rift (2)
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Kenya (1)
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Tanzania (2)
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East African Lakes
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Lake Kivu (1)
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East African Rift (2)
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Madagascar (1)
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North Africa
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Atlas Mountains
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Egypt (2)
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Nubian Shield (1)
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Asia
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Ghats
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Gujarat India
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Dhanbad India (1)
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receiver functions
INSIGHTS INTO THE MOHO DEPTH AND CRUSTAL CHARACTERISTICS IN THE GUELMA–CONSTANTINE BASIN: A SHORT-PERIOD SEISMIC-RECEIVER-FUNCTION PERSPECTIVE ( northeastern Algeria )
Imaging Complex Structures of the Los Angeles Basin via Adjoint‐State Travel‐Time Tomography
Seismic Electromagnetic Radiation Simulation Using Finite‐Element Time‐Domain Method
Proximal Observations of Epicentral Infrasound Generated by Shallow Low‐Magnitude Earthquakes in the Permian Basin, West Texas
Hydrous Melting and its Seismic Signature
A translithospheric magmatic system revealed beneath Changbaishan volcano
Assessing the Predictive Power of GPS‐Based Ground Deformation Data for Aftershock Forecasting
Deep Learning–Based Denoising Improves Receiver Function Imaging Using Dense Short‐Period Teleseismic Data
Uncertainty Quantification in Radial Anisotropy Models Based on Transdimensional Bayesian Inversion of Receiver Functions and Surface‐Wave Dispersion: Case Study Sri Lanka
Fault–Dike–Magma Interactions Inferred from Transcrustal Conical Structures under Akutan Volcano
Single‐Station Back‐Azimuth Determination with the Receiver Function Rotation Technique Validated by the Locations of Earthquakes, Impacts, and Explosions
Multitimescale Template Matching: Discovering Eruption Precursors across Diverse Volcanic Settings
A Seismic Nodal Deployment to Understand Magmatic Structure in the Vicinity of the Pāhala Earthquake Swarm
Crustal Imaging with Noisy Teleseismic Receiver Functions Using Sparse Radon Transforms
Characterization of anisotropy in basin-scale subsurface using teleseismic receiver function analysis
Exploring the Moho beneath the Northern Canadian Cordillera, with seismically constrained gravity inversion
Continents never forget: seismological record of lithospheric deformation 1 billion years ago
Abstract A seismic array extended from the Grenville Province into the Abitibi and Opatica subprovinces of the Superior Province, Canada. We use P-to-S converted waves in seismograms of distant earthquakes to probe boundaries in seismic properties, and demonstrate the presence of a prominent seismic feature that dips NNW into the mantle beneath the Grenville Front. We use two variants of receiver function (RF) analysis, a common conversion-point (CCP) imaging that combines seismic signals from multiple paths connecting sources and receivers, and harmonic decomposition of RF data that separates signals according to their direction in the cone of paths from which the signals have come. CCP images show the crust beneath the Grenville Province to be thicker than beneath the Superior Province, and identify a NNW-dipping boundary beneath the Grenville Front. Harmonic RF analysis shows that this feature is associated with seismic anisotropy in upper-mantle peridotite, and that this anisotropic feature extends to depths of at least 70 km. We interpret the feature as the result of a NNW-dipping shear zone formed within the mantle lithosphere during the Grenvillian continental collision. It could have accommodated internal deformation within Laurentian lithosphere or, more speculatively, mark the contact with the impacting Amazonian lithosphere.