Results 141 to 150 of about 1,640,713 (238)
Anomalous K-Pg-aged seafloor attributed to impact-induced mid-ocean ridge magmatism. [PDF]
Byrnes JS, Karlstrom L.
europepmc +1 more source
Abstract The Aurora hydrothermal vent field (AVF) is the first confirmed active vent system on the Arctic Ocean seafloor, located at the western end of the ultraslow spreading Gakkel Ridge. It marks a distinctive endmember among ridge‐axis hydrothermal systems, where volcanic construction and ultramafic influence co‐exist.
Matthias Pilot +3 more
wiley +1 more source
Discovery of a Thermostable GH10 Xylanase with Broad Substrate Specificity from the Arctic Mid-Ocean Ridge Vent System. [PDF]
Fredriksen L +6 more
europepmc +1 more source
Abstract The Geomagnetic Polarity Time Scale (GPTS) is essential to date geological events in stratigraphic sequences and to reconstruct plate motions. The first GPTSs were based on the record of magnetic anomalies created by seafloor spreading, calibrated by a few radioisotopic dates.
A. Malinverno, S. R. Meyers
wiley +1 more source
Correction for Worman et al., Abiotic hydrogen (H2) sources and sinks near the Mid-Ocean Ridge (MOR) with implications for the subseafloor biosphere. [PDF]
europepmc +1 more source
Seafloor hydrothermal activity along mid-ocean ridge with strong melt supply: study from segment 27, southwest Indian ridge. [PDF]
Yue X +6 more
europepmc +1 more source
Uncertainty in Precipitation Estimates Warrants Greater Consideration in Debris‐Flow Research
Abstract Quantitative precipitation estimates (QPEs) may provide a valuable data resource for investigations of postfire debris flows. In mountainous regions where debris flows typically occur, gauge coverage can be sparse; gridded QPEs offer remotely sensed and/or physics‐based precipitation estimates where no direct measurement is available. However,
Ann E. Sinclair +4 more
wiley +1 more source
Large melt diversity at a mid-ocean ridge thermal low. [PDF]
Brunelli D +8 more
europepmc +1 more source
Magma plumbing system and seismicity of an active mid-ocean ridge volcano. [PDF]
Schmid F +4 more
europepmc +1 more source
Abstract Whether the Songduo metamorphic belt represents an in situ Paleo‐Tethyan suture within the Lhasa Terrane or far‐traveled allochthonous high‐pressure slices, and how Permian mantle activity along the North Gondwana margin relates to subsequent Tethyan evolution, remain central questions in Tibetan tectonics.
Yuan‐Bo Ma +9 more
wiley +1 more source

