Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Emmanuel A. Njinju"'
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Density perturbations in the subsurface are the main driver of mantle convection and can contribute to lithospheric deformation. However, in many places the density structure in the subsurface is poorly constrained. Most geodynamic models rely on sim
Externí odkaz:
https://doaj.org/article/d77af725eea54255a6f4a16f80451cb6
The force balance that drives and maintains continental rifting to breakup is poorly understood. The East African Rift (EAR) provides an ideal natural laboratory to elucidate the relative role of plate driving forces as only lithospheric buoyancy for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b840ea7d66b2330f861759e4c115996b
https://hdl.handle.net/10919/115435
https://hdl.handle.net/10919/115435
Density perturbations in the subsurface are the main driver of mantle convection and can contribute to lithospheric deformation. However, in many places the density structure in the subsurface is poorly constrained. Most geodynamic models rely on sim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::61952f6561640e4c2a0ddce8144ae158
https://hdl.handle.net/10919/114171
https://hdl.handle.net/10919/114171
Autor:
D. Sarah Stamps, Stewart Fishwick, Emmanuel A. Njinju, Mohamed G. Abdelsalam, Folarin Kolawole, Kevin L. Mickus, Estella A. Atekwana, T. A. Rajaonarison, Eliot A. Atekwana, Victor N. Nyalugwe
Publikováno v:
Tectonics. 38:3835-3853
This project was supported by the National Science Foundation–Continental Dynamics (NSF‐CD) Grant EAR‐1255233 and Office of International and Integrative Activities (OIIA) Grant IIA‐1358150. This project is also supported by the NSF EarthCube
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37363889496da6519d533492f80f674b
https://doi.org/10.1029/2019tc005549
https://doi.org/10.1029/2019tc005549
Autor:
Luelseged Emishaw, J. Salima, Estella A. Atekwana, Mohamed G. Abdelsalam, Emmanuel A. Njinju, Kevin L. Mickus, Victor N. Nyalugwe, Andrew B. Katumwehe
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:12224-12240
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca7c3aa44a72f8964ce0240a42723416
https://doi.org/10.1029/2019jb018430
https://doi.org/10.1029/2019jb018430
ASPECT (Advanced Solver for Problems in Earth's ConvecTion) is an analysis tool that simulates convection in the Earth’s mantle and other planets. The BALTO project has extended the ASPECT software...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0cf151d5e763cb17c795ec7303d813bf
https://doi.org/10.1002/essoar.10503662.1
https://doi.org/10.1002/essoar.10503662.1
The Rungwe Volcanic Province (RVP) is a volcanic center in an anomalous region of magma-assisted rifting positioned within the magma-poor Western Branch of the East African Rift (EAR). The source o...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::51d1f3a7113d044c735cdc276964f953
https://doi.org/10.1002/essoar.10503939.1
https://doi.org/10.1002/essoar.10503939.1
The EarthCube BALTO (Brokered Alignment of Long-Tail Observations) project is aimed at developing new cyberinfrastructures that enables brokered access to diverse geoscience datasets. Towards achie...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc97f1f57196b4cb09519db6591cac82
https://doi.org/10.1002/essoar.10503700.1
https://doi.org/10.1002/essoar.10503700.1
Autor:
D. Sarah Stamps, Daniel R. Fuka, Emmanuel A. Njinju, Nathan Potter, Zachary M. Easton, David Fulker, Anne F. Sheehan, Kodi Neumiller, Scott D. Peckham, James Gallagher, Maria Stoica
The EarthCube BALTO broker (Brokered Alignment of Long-Tail Observations) provides streamlined access to both long-tail and big data using Web Services through several distinct mechanisms. First, w...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e384d2634b3d4fa6e6b65a681edaa119
https://doi.org/10.1002/essoar.10503488.1
https://doi.org/10.1002/essoar.10503488.1
Autor:
Kevin L. Mickus, Estella A. Atekwana, D. Sarah Stamps, Emmanuel A. Njinju, Eliot A. Atekwana, Mohamed G. Abdelsalam, Folarin Kolawole
Publikováno v:
Journal of Volcanology and Geothermal Research. 387:106656
Rift basins show the widest range of heat flow values compared to passive continental margins and intracratonic sag basins. Elevated heat flow is often used to infer asthenospheric upwelling or subsurface magmatic activity for magma-assisted rifts. D
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::30c2ac14a37a3e11abff62e79e5e55a1
https://doi.org/10.1016/j.jvolgeores.2019.07.023
https://doi.org/10.1016/j.jvolgeores.2019.07.023