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Evolution and structure of the Upper Rhine Graben — quantitative insights from numerical modelling approaches
(11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)The Upper Rhine Graben forms the major segment of the Cenozoic Rift system of Western Europe. Although the rift was the target of many seismic and geological investigations, the style of lithospheric extension below the ... -
Evolution of (Bio‐)Geochemical Processes and Diagenetic Alteration of Sediments Along the Tectonic Migration of Ocean Floor in the Shikoku Basin off Japan
; ; ; ; ; ; ; ; ; ; (Geochemistry, Geophysics, Geosystems, 2021-08-03)
Biogeochemical processes in subseafloor sediments are closely coupled to global element cycles. To improve the understanding of changes in biogeochemical conditions on geological timescales, we investigate sediment cores ... -
Evolution of a hydrothermal ore-forming system recorded by sulfide mineral chemistry: a case study from the Plaka Pb–Zn–Ag Deposit, Lavrion, Greece
; ; ; ; ; (Mineralium Deposita, 2021-08-28)
Laser ablation-inductively coupled plasma-mass spectrometry and electron-probe microanalysis were used to investigate the trace-element contents of sphalerite, chalcopyrite and pyrite from the Plaka Pb–Zn–Ag deposit. Using ... -
Evolution of an Atmospheric Kármán Vortex Street From High-Resolution Satellite Winds: Guadalupe Island Case Study
; ; ; ; ; ; ; ; ; (Journal of Geophysical Research: Atmospheres, 2020)
Vortex streets formed in the stratocumulus-capped wake of mountainous islands are the atmospheric analogues of the classic Kármán vortex street observed in laboratory flows past bluff bodies. The quantitative analysis of ... -
Evolution of convective characteristics during tropical cyclogenesis
(Quarterly Journal of the Royal Meteorological Society, 2021-04-05)
Four idealized, high‐resolution (500 m horizontal grid spacing), numerical simulations are used to investigate the evolution of convective structures during tropical cyclogenesis. The simulations all begin with a weak ... -
Evolution of diagenetic conditions and burial history in Buntsandstein Gp. fractured sandstones (Upper Rhine Graben) from in-situ δ18O of quartz and 40Ar/39Ar geochronology of K-feldspar overgrowths
; ; ; ; ; ; ; (International Journal of Earth Sciences, 2021-07-09)
In-situ δ18O measured in the quartz overgrowths help identify temperature and fluid origin variations responsible for cementation of the pore network (matrix and fracture) in the Buntsandstein Gp. sandstone reservoirs ... -
Evolution of Global Ocean Tide Levels Since the Last Glacial Maximum
; ; ; ; ; ; (Paleoceanography and Paleoclimatology, 2023-05-10)
Abstract This study addresses the evolution of global tidal dynamics since the Last Glacial Maximum ...
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Evolution of Lamayuru palaeolake in the Trans Himalaya: Palaeoecological implications
(E&G – Quaternary Science Journal; Vol.48, No. 1)Vor etwa 35 000-40 000 Jahren schuf eine Episode neotektonischer Aktivität an der Indus-Sutur bei Lamayuru (Ladakh) einen See, von dem eine über 105 m mächtige Abfolge fluviolakustriner Ablagerungen erhalten ist. Die ... -
Evolution of Magmatism in the New Hebrides Island Arc and in Initial Back-Arc Rifting, SW Pacific
; ; Lima, S. M.; ; ; Romer, R. L.; Bellon, H. (Geochemistry, Geophysics, Geosystems, 2020)
We present new geochemical and isotopic data for rock samples from two island arc volcanoes, Erromango and Vulcan Seamount, and from a 500 m thick stratigraphic profile of lava flows exposed on the SW flank of Vate Trough ... -
Evolution of Rift Systems and Their Fault Networks in Response to Surface Processes
; ; ; ; ; (Tectonics, 2022-02-24)
Continental rifting is responsible for the generation of major sedimentary basins, both during rift inception and during the formation of rifted continental margins. Geophysical and field studies revealed that rifts feature ... -
Evolution of Sea Surface Hydrology Along the Western Australian Margin Over the Past 450 kyr
; ; ; ; ; ; ; (Paleoceanography and Paleoclimatology, 2021-11-05)
We collected a suite of core top samples during R/V Sonne Cruise SO257 in May 2017 along the southwestern front of the Indo‐Pacific Warm Pool (IPWP) to monitor the variability of Southern Hemisphere tropical and subtropical ... -
Evolution of the Geomagnetic Daily Variation at Tatuoca, Brazil, From 1957 to 2019: A Transition From Sq to EEJ
; ; ; ; ; ; ; (Journal of Geophysical Research: Space Physics, 2020)
The magnetic equator in the Brazilian region has moved over 1,100 km northward since 1957, passing the geomagnetic observatory Tatuoca (TTB), in northern Brazil, around 2013. We recovered and processed TTB hourly mean ... -
Evolution of the Lower Permian Rochlitz volcanic system, Eastern Germany: reconstruction of an intra-continental supereruption
; ; ; ; ; ; (International Journal of Earth Sciences, 2021-07-14)
Extensional tectonics in the Late Paleozoic Central Europe was accompanied by rift magmatism that triggered voluminous intracontinental caldera-forming eruptions. Among these, the Lower Permian Rochlitz Volcanic System ... -
Evolution of the Tamtsag Basin / NE-Mongolia — part I: basin fill
(11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)The Tamtsag Basin in NE Mongolia is part of a widespread basin system which formed during Late Jurassic and Cretaceous times (Graham et al. 2001, Qing-Ren et al. 2003). It is filled with continental sediments and volcanics ... -
Evolution of the Tamtsag Basin / NE-Mongolia — part II: structure and hydrocarbon potential
(11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)The Tamtsag basin in NE Mongolia is part of a widespread basin system which formed during Late Jurassic and Cretaceous times (Graham et al. 2001, Qing-Ren et al. 2003). It is filled with continental sediments and volcanics which ... -
Evolution of the tRNALeu (UAA) Intron and Congruence of Genetic Markers in Lichen-Symbiotic Nostoc.
(PloS one, 2015)The group I intron interrupting the tRNALeu UAA gene (trnL) is present in most cyanobacterial genomes as well as in the plastids of many eukaryotic algae and all green plants. In lichen symbiotic Nostoc, the P6b stem-loop ... -
Evolution of the West Andean Escarpment at 18°S (N. Chile) during the last 25 Ma: uplift, erosion and collapse through time
; Uhlig, Dieter; Kohler, Ingrid; Seyfried, Hartmut (Tectonophysics, 2002)
The geological record of the Western Andean Escarpment (WARP) reveals episodes of uplift, erosion, volcanism and sedimentation. The lithological sequence at 18°S comprises a thick pile of Azapa Conglomerates (25–19 Ma), ... -
Evolution of Thrace Macula on Europa: Strike‐Slip Tectonic Control and Identification of the Youngest Terrains
; ; ; ; (Journal of Geophysical Research: Planets, 2023-08-11)
Abstract Chaos terrains are geologically young and extensively disrupted surface features of ...
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Evolution und Struktur des Oberrheingrabens - quantitative Einblicke mit Hilfe dreidimensionaler thermomechanischer Modellrechnungen
(Univ. Freiburg (Breisgau), 2006)In der Modellstudie wurde ein numerisches Modell für ein kontinentales Riftsystem erstellt, welches durch präexistierende Störungen sowohl entlang in seinem Streichen als auch quer dazu vorgeƯzeichnet war. Das Modell ... -
Evolving temperature field in a fossil subduction channel during the transition from subduction to collision (Tauern Window, Eastern Alps)
; Pleuger, Jan; ; Germer, Marisa; (Journal of Metamorphic Geology, 2020-10-12)
We investigate the evolution of the three‐dimensional thermal structure of a palaeo‐subduction channel exposed in the Penninic units of the central Tauern Window (Eastern Alps). Structural and petrological observations ...
