Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Derek Neuharth"'
Autor:
Ameha Muluneh, Sascha Brune, Carolina Pagli, Alessandro La Rosa, Derek Keir, Derek Neuharth, Giacomo Corti
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 12, Pp n/a-n/a (2024)
Abstract Central Afar is shaped by the interaction between the Red Sea (RS) and Gulf of Aden (GoA) rifts. While there have been several studies conducted in the region, we know surprisingly little about the mechanism of connection between these two r
Externí odkaz:
https://doaj.org/article/8d1fcdae0cfc45fb82cb1aebbea97c77
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 4, Pp n/a-n/a (2021)
Abstract Continental microplates are enigmatic plate boundary features, which can occur in extensional and compressional regimes. Here we focus on microplate formation and their temporal evolution in continental rift settings. To this aim, we employ
Externí odkaz:
https://doaj.org/article/5e2c5f32aa76479db5b90044bd8cd493
Autor:
Derek Neuharth, Eric Mittelstaedt
Publikováno v:
Geophysical Journal International
SUMMARY Along age-progressive hotspot volcano chains, the emplacement rate of igneous material varies through time. Time-series analysis of changing emplacement rates at a range of hotspots finds that these rates vary regularly at periods of a few to
Cenozoic rifting in the South China Sea developed after a Mesozoic Andean-type orogeny (i.e., Yanshanian orogen) which led to structural, compositional, and thermal inheritance.These inherited lithospheric weaknesses can control the inception and evo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8305a30799a8a3b193fc9c4f3d9ec84
https://doi.org/10.5194/egusphere-egu23-7518
https://doi.org/10.5194/egusphere-egu23-7518
Because subduction zones can extend thousands of kilometers along-strike, many previous studies have used 2D subduction models which inherently assume homogeneity along-strike. However, in nature we see that subduction zones are often heterogeneous a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1085f920e6905a3af2d9e0a2b89422e3
https://doi.org/10.5194/egusphere-egu23-11688
https://doi.org/10.5194/egusphere-egu23-11688
Understanding how normal fault networks initiate and evolve is important for quantifying plate boundary deformation, assessing seismic hazard and finding natural resources. In recent years, 3D numerical models have been developed that can simulate th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::913a1bfff57879a23c2221b9e41e6a94
https://doi.org/10.5194/egusphere-egu23-11050
https://doi.org/10.5194/egusphere-egu23-11050
The region around the Dead Sea Transform represents a unique example of the structures that form around restraining and releasing bends in a strike-slip environment. With our 3D numerical models, we aim to understand the processes that shaped the reg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9d1b1243078720d500923f177e353b77
https://doi.org/10.5194/egusphere-egu22-5427
https://doi.org/10.5194/egusphere-egu22-5427
During the formation of rifted continental margins, a rift evolves through a number of stages that produce major sedimentary basins and distinct rifted margin domains. While these domains have been classified based on the resulting structures and cru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::51c3475e6fcfd0ac4e200bb30dc0ba87
https://doi.org/10.5194/egusphere-egu22-5758
https://doi.org/10.5194/egusphere-egu22-5758
The nature of the shortening of the Central Andes has been a matter of debate. The South American plate is advancing westwards forcing the subducting Nazca plate to roll back and the trench to retreat. But as the trench slowed its retreat the Andean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8825c4798d58a5b393ebfcd1c4597dc6
https://doi.org/10.5194/egusphere-egu22-5284
https://doi.org/10.5194/egusphere-egu22-5284
Quantifying the spatial and temporal evolution of fault systems is crucial in understanding plate boundary deformation and the associated seismic hazard, as well as to help georesources exploration in sedimentary basins. During the last decade, 3D li
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1de56cba5e5f2eead80566b770e98e4c
https://doi.org/10.5194/egusphere-egu22-6294
https://doi.org/10.5194/egusphere-egu22-6294