FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2001361034> ?p ?o ?g. }

• W2001361034 endingPage "170" @default.
• W2001361034 startingPage "153" @default.
• W2001361034 abstract "The 2010 eruption of Merapi is the first large explosive eruption of the volcano that has been instrumentally observed. The main characteristics of the seismic activity during the pre-eruptive period and the crisis are presented and interpreted in this paper. The first seismic precursors were a series of four shallow swarms during the period between 12 and 4 months before the eruption. These swarms are interpreted as the result of perturbations of the hydrothermal system by increasing heat flow. Shorter-term and more continuous precursory seismic activity started about 6 weeks before the initial explosion on 26 October 2010. During this period, the rate of seismicity increased almost constantly yielding a cumulative seismic energy release for volcano-tectonic (VT) and multiphase events (MP) of 7.5 × 1010 J. This value is 3 times the maximum energy release preceding previous effusive eruptions of Merapi. The high level reached and the accelerated behavior of both the deformation of the summit and the seismic activity are distinct features of the 2010 eruption. The hypocenters of VT events in 2010 occur in two clusters at of 2.5 to 5 km and less than 1.5 km depths below the summit. An aseismic zone was detected at 1.5–2.5 km depth, consistent with studies of previous eruptions, and indicating that this is a robust feature of Merapi's subsurface structure. Our analysis suggests that the aseismic zone is a poorly consolidated layer of altered material within the volcano. Deep VT events occurred mainly before 17 October 2010; subsequent to that time shallow activity strongly increased. The deep seismic activity is interpreted as associated with the enlargement of a narrow conduit by an unusually large volume of rapidly ascending magma. The shallow seismicity is interpreted as recording the final magma ascent and the rupture of a summit-dome plug, which triggered the eruption on 26 October 2010. Hindsight forecasting of the occurrence time of the eruption is performed by applying the Material Failure Forecast Method (FFM) using cumulative Real-time Seismic Amplitude (RSAM) calculated both from raw records and on signals classified according to their dominant frequency. Stable estimates of eruption time with errors as small as ± 4 h are obtained within a 6 day lapse time before the eruption. This approach could therefore be useful to support decision making in the case of future large explosive episodes at Merapi." @default.
• W2001361034 created "2016-06-24" @default.
• W2001361034 creator A5004590315 @default.
• W2001361034 creator A5012936761 @default.
• W2001361034 creator A5032682213 @default.
• W2001361034 creator A5050494448 @default.
• W2001361034 creator A5055523481 @default.
• W2001361034 creator A5061715440 @default.
• W2001361034 creator A5073184879 @default.
• W2001361034 creator A5086774902 @default.
• W2001361034 date "2013-07-01" @default.
• W2001361034 modified "2023-09-23" @default.
• W2001361034 title "Analysis of the seismic activity associated with the 2010 eruption of Merapi Volcano, Java" @default.
• W2001361034 cites W1632024656 @default.
• W2001361034 cites W1895969821 @default.
• W2001361034 cites W1956217412 @default.
• W2001361034 cites W1968293803 @default.
• W2001361034 cites W1970776328 @default.
• W2001361034 cites W1974910804 @default.
• W2001361034 cites W1976268687 @default.
• W2001361034 cites W1983443340 @default.
• W2001361034 cites W1987494683 @default.
• W2001361034 cites W1988325392 @default.
• W2001361034 cites W1992124464 @default.
• W2001361034 cites W1993201067 @default.
• W2001361034 cites W1999852801 @default.
• W2001361034 cites W2004289607 @default.
• W2001361034 cites W2006396051 @default.
• W2001361034 cites W2007186363 @default.
• W2001361034 cites W2007824499 @default.
• W2001361034 cites W2010530941 @default.
• W2001361034 cites W2011674844 @default.
• W2001361034 cites W2013450558 @default.
• W2001361034 cites W2015140881 @default.
• W2001361034 cites W2021995044 @default.
• W2001361034 cites W2025878044 @default.
• W2001361034 cites W2027516515 @default.
• W2001361034 cites W2037601751 @default.
• W2001361034 cites W2038431301 @default.
• W2001361034 cites W2039147041 @default.
• W2001361034 cites W2039277967 @default.
• W2001361034 cites W2039657733 @default.
• W2001361034 cites W2044190332 @default.
• W2001361034 cites W2051568115 @default.
• W2001361034 cites W2053594289 @default.
• W2001361034 cites W2055643012 @default.
• W2001361034 cites W2058815834 @default.
• W2001361034 cites W2060050401 @default.
• W2001361034 cites W2066621482 @default.
• W2001361034 cites W2071917711 @default.
• W2001361034 cites W2084616702 @default.
• W2001361034 cites W2087069691 @default.
• W2001361034 cites W2093168377 @default.
• W2001361034 cites W2099243357 @default.
• W2001361034 cites W2100286929 @default.
• W2001361034 cites W2101364243 @default.
• W2001361034 cites W2114993729 @default.
• W2001361034 cites W2115056698 @default.
• W2001361034 cites W2123111622 @default.
• W2001361034 cites W2135372199 @default.
• W2001361034 cites W2138506114 @default.
• W2001361034 cites W2151573464 @default.
• W2001361034 cites W2151909003 @default.
• W2001361034 cites W2152396894 @default.
• W2001361034 cites W2155781583 @default.
• W2001361034 cites W2155913568 @default.
• W2001361034 cites W2169987296 @default.
• W2001361034 cites W2200022943 @default.
• W2001361034 cites W2309700780 @default.
• W2001361034 doi "https://doi.org/10.1016/j.jvolgeores.2013.03.024" @default.
• W2001361034 hasPublicationYear "2013" @default.
• W2001361034 type Work @default.
• W2001361034 sameAs 2001361034 @default.
• W2001361034 citedByCount "82" @default.
• W2001361034 countsByYear W20013610342013 @default.
• W2001361034 countsByYear W20013610342014 @default.
• W2001361034 countsByYear W20013610342015 @default.
• W2001361034 countsByYear W20013610342016 @default.
• W2001361034 countsByYear W20013610342017 @default.
• W2001361034 countsByYear W20013610342018 @default.
• W2001361034 countsByYear W20013610342019 @default.
• W2001361034 countsByYear W20013610342020 @default.
• W2001361034 countsByYear W20013610342021 @default.
• W2001361034 countsByYear W20013610342022 @default.
• W2001361034 countsByYear W20013610342023 @default.
• W2001361034 crossrefType "journal-article" @default.
• W2001361034 hasAuthorship W2001361034A5004590315 @default.
• W2001361034 hasAuthorship W2001361034A5012936761 @default.
• W2001361034 hasAuthorship W2001361034A5032682213 @default.
• W2001361034 hasAuthorship W2001361034A5050494448 @default.
• W2001361034 hasAuthorship W2001361034A5055523481 @default.
• W2001361034 hasAuthorship W2001361034A5061715440 @default.
• W2001361034 hasAuthorship W2001361034A5073184879 @default.
• W2001361034 hasAuthorship W2001361034A5086774902 @default.
• W2001361034 hasBestOaLocation W20013610342 @default.
• W2001361034 hasConcept C120806208 @default.
• W2001361034 hasConcept C121332964 @default.
• W2001361034 hasConcept C127313418 @default.

• next