Results 231 to 240 of about 8,008,633 (316)
Full waveform tomographic images of the peak ring at the Chicxulub impact crater
J. Morgan +6 more
semanticscholar +1 more source
Fouling in Emulsion Polymerization: Fundamentals and Methods of Investigation
ABSTRACT The current understanding of fouling in emulsion polymerization is summarized from an engineering perspective and from a physical‐chemistry perspective. Emulsion polymerization in semibatch mode offers better control over the number of particles and side reactions than batch mode. Both reaction fouling and particulate fouling are observed, the
Holly A. Huellemeier +5 more
wiley +1 more source
Saturn's moon Mimas may have a vast hidden ocean. [PDF]
Tillman NT.
europepmc +1 more source
Large‐Scale Topographic Changes at Erupting Volcanoes Measured by the TanDEM‐X Digital Change Map
Abstract Volcanic eruptions cause large‐scale topographic changes, through the emplacement of lava flows and lava domes, the formation of craters and calderas, and thick ash and pyroclastic deposits. Here we analyze the TanDEM‐X Digital Change Map (DCM), which compares the DEM produced during 2010–2015 with satellite acquisitions collected in 2016–2022.
Rebecca Edwards, Juliet Biggs
wiley +1 more source
Deposition, exhumation, and paleoclimate of an ancient lake deposit, Gale crater, Mars
J. Grotzinger +46 more
semanticscholar +1 more source
Abstract This study monitors the seismic velocity changes beneath the Izu‐Oshima volcano, central Japan, using ambient seismic noise records from 2003 to 2020. Applying seismic interferometry to the continuous waveform data from 24 seismic stations, we observed significant temporal variations in the seismic velocity structure.
Yohei Yukutake +3 more
wiley +1 more source
Modeling the formation of sedan crater using the FLAG and HOSS codes. [PDF]
Henderson SF +6 more
europepmc +1 more source
Abstract The Mount Sharp group in Gale crater is typically interpreted to record a progressive change (with increasing elevation) from wetter fluvio‐lacustrine environments to dry, eolian environments. This shift has been linked to orbital evidence for a global change in environmental and depositional conditions leading to an overall drying out of Mars.
C. D. O’Connell‐Cooper +14 more
wiley +1 more source
Crater morphology in sandstone targets: The MEMIN impact parameter study
A. Dufresne +6 more
semanticscholar +1 more source

