Deep mantle melting, global water circulation and its implications for the stability of the ocean mass
Oceans on Earth are present as a result of dynamic equilibrium between degassing and
regassing through the interaction with Earth's interior. We review mineral physics …
regassing through the interaction with Earth's interior. We review mineral physics …
Geomorphic complexity and the case for topographic rejuvenation of the Appalachian Mountains
JA Spotila, PS Prince - Geomorphology, 2022 - Elsevier
Despite vast scientific inquiry, the evolution of Appalachian Mountain topography in eastern
North America has yet to be robustly explained. After a century and a half of investigation …
North America has yet to be robustly explained. After a century and a half of investigation …
MATE: An analysis tool for the interpretation of magnetotelluric models of the mantle
Abstract Interpretation of electrical conductivity anomalies observed in magnetotelluric
models provides an important opportunity to understand the nature of the lithospheric mantle …
models provides an important opportunity to understand the nature of the lithospheric mantle …
Thin lithosphere beneath the central Appalachian Mountains: Constraints from seismic attenuation beneath the MAGIC array
The passive margin of the eastern coast of the United States is known to be geologically
active, with recently rejuvenated topography, intraplate seismicity, and volcanism of Eocene …
active, with recently rejuvenated topography, intraplate seismicity, and volcanism of Eocene …
Evolution, Modification, and Deformation of Continental Lithosphere: Insights from the Eastern Margin of North America
MD Long - Annual Review of Earth and Planetary Sciences, 2024 - annualreviews.org
Continental lithosphere is deformed, destroyed, or otherwise modified in several ways.
Processes that modify the lithosphere include subduction, terrane accretion, orogenesis …
Processes that modify the lithosphere include subduction, terrane accretion, orogenesis …
Evaluating models for lithospheric loss and intraplate volcanism beneath the Central Appalachian Mountains
The eastern margin of North America has been shaped by a series of tectonic events
including the Paleozoic Appalachian Orogeny and the breakup of Pangea during the …
including the Paleozoic Appalachian Orogeny and the breakup of Pangea during the …
The Laramide orogeny: Current understanding of the structural style, timing, and spatial distribution of the classic foreland thick-skinned tectonic system
The Laramide foreland belt comprises a broad region of thick-skinned, contractional
deformation characterized by an anastomosing network of basement-cored arches and …
deformation characterized by an anastomosing network of basement-cored arches and …
Evidence for a lithospheric step and pervasive lithospheric thinning beneath southern New England, northeastern USA
In this study, we use data from the SEISConn seismic experiment to calculate Sp receiver
functions in order to characterize the geometry of upper-mantle structure beneath southern …
functions in order to characterize the geometry of upper-mantle structure beneath southern …
Modification of crust and mantle lithosphere beneath the southern part of the eastern North American passive margin
C Li, H Gao - Geophysical Research Letters, 2021 - Wiley Online Library
Abstract The eastern North American passive margin was modified by Mesozoic rifting.
Seismic data from recent deployment of onshore and offshore stations offer a unique …
Seismic data from recent deployment of onshore and offshore stations offer a unique …
Mantle Structure and Flow Across the Continent‐Ocean Transition of the Eastern North American Margin: Anisotropic S‐Wave Tomography
Little has been seismically imaged through the lithosphere and mantle at rifted margins
across the continent‐ocean transition. A 2014–2015 community seismic experiment …
across the continent‐ocean transition. A 2014–2015 community seismic experiment …