syneruptivelyとは 意味・読み方・使い方

副詞

syneruptively (comparative more syneruptively, superlative most syneruptively)

1. (geology) In a syneruptive manner; occurring during the time of a volcanic eruption.
   • 2024 August, Sharon L. Walker, Cornel E. J. de Ronde, “Ongoing Activity at Hunga Submarine Volcano, Tonga: The Case for Better Monitoring of Submarine Volcanoes Worldwide”, in Geochemistry, Geophysics, Geosystems‎, volume 25, number 8, American Geophysical Union, →DOI, archived from the original on 2024-10-05:

     Carbon dioxide is one of the most common magmatic gasses and is often emitted at submarine hydrothermal and eruptive vents (e.g., Chadwick, Cashman, et al., 2008; Lupton et al., 2006). Chadwick et al. (2014) observed CO2 bubbles emerging from the eruptive vents at NW Rota-1 detach from the syneruptively generated sulfur-rich plumes and rise higher in the water column before eventually dissolving. Our observations provide evidence that CO2 appears to behave similarly at Hunga.

   • 2023, “Eruptive history within the vicinity of Al Madīnah in northern Harrat Rahat, Kingdom of Saudi Arabia” (chapter C), in Downs, Drew T., Stelten, Mark E., Champion, Duane E., Dietterich, Hannah R., Hassan, Khalid, Shawali, Jamal, editors, Active volcanism on the Arabian Shield—Geology, volcanology, and geophysics of northern Harrat Rahat and vicinity, Kingdom of Saudi Arabia (USGS Professional Paper; 1862-C)‎, Reston, VA: United States Geological Survey, →DOI, archived from the original on 2024-10-05:

     Despite small individual volumes (less than 1 cubic kilometers dense rock equivalent), each unit represents eruption of a distinct magma batch that was strongly influenced by clinopyroxene, olivine, and plagioclase fractionation. Some of these units are interpreted to have undergone magma mixing pre- and (or) syneruptively.

   • 1986 December, Stephen Blake, Gregory N. Ivey, “Density and viscosity gradients in zoned magma chambers, and their influence withdrawal dynamics”, in Journal of Volcanology and Geothermal Research‎, volume 30, numbers 3–4, Elsevier, →DOI, archived from the original on 2024-10-05, pages 201–230:

     The liquid being sampled from a draining reservoir of density-stratified fluid, such as an erupting zoned magma chamber, is derived from a relatively thin withdrawal layer adjacent to the level of the chamber outlet. This is a consequence of the buoyancy force associated with the density gradient inhibiting vertical motion so that the opportunity for widely separated density levels (compositions) to be tapped and mingled syneruptively is suppressed.

   • 1986 October, V. Lorenz, “On the growth of maars and diatremes and its relevance to the formation of tuff rings”, in Bulletin of Volcanology‎, volume 48, number 5, Springer Science+Business Media, →DOI, archived from the original on 2024-05-06, pages 265–274:

     Fig. 6. A block of feldspar-bearing sandstone which syneruptively subsided in the Rödern diatreme in the Carboniferous-Permian Saar-Nahe Basin, SW Germany (Lorenz 1971).