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Statements

Subject Item
n2:RIV%2F67985530%3A_____%2F13%3A00389366%21RIV14-MSM-67985530
rdf:type
n3:Vysledek skos:Concept
dcterms:description
Internal structure and recent tectonics of the geologically complex Banda Arc region (latitude 1–9 S, longitude 124–135 E) have been studied by means of the analysis of global seismological data. Relocated hypocentral determinations of the International Seismological Center (EHB data) and fault plane solutions of the Global Centroid Moment Tensor Project have been used together with previously published information on regional geology and dynamics. The analysis considered earthquakes in the lithospheric wedges above subducting slabs and earthquakes in the uppermost portions of the Wadati–Benioff zones (focal depth < 100 km); we avoided intermediate-depth and deep earthquakes that are clearly separated from shallow ones by distinct discontinuities in the Wadati–Benioff zones. Such a selection best reflects present manifestations of tectonic processes. We delimitated 11 domains of earthquakes, each of them spatially distinct and with similar earthquake focal mechanisms. The number of events that did not fit in any domain was negligible. Internal structure and recent tectonics of the geologically complex Banda Arc region (latitude 1–9 S, longitude 124–135 E) have been studied by means of the analysis of global seismological data. Relocated hypocentral determinations of the International Seismological Center (EHB data) and fault plane solutions of the Global Centroid Moment Tensor Project have been used together with previously published information on regional geology and dynamics. The analysis considered earthquakes in the lithospheric wedges above subducting slabs and earthquakes in the uppermost portions of the Wadati–Benioff zones (focal depth < 100 km); we avoided intermediate-depth and deep earthquakes that are clearly separated from shallow ones by distinct discontinuities in the Wadati–Benioff zones. Such a selection best reflects present manifestations of tectonic processes. We delimitated 11 domains of earthquakes, each of them spatially distinct and with similar earthquake focal mechanisms. The number of events that did not fit in any domain was negligible.
dcterms:title
Seismic response to recent tectonic processes in the Banda Arc region Seismic response to recent tectonic processes in the Banda Arc region
skos:prefLabel
Seismic response to recent tectonic processes in the Banda Arc region Seismic response to recent tectonic processes in the Banda Arc region
skos:notation
RIV/67985530:_____/13:00389366!RIV14-MSM-67985530
n3:predkladatel
n4:ico%3A67985530
n5:aktivita
n16:I n16:P
n5:aktivity
I, P(ME09011)
n5:cisloPeriodika
5 March
n5:dodaniDat
n11:2014
n5:domaciTvurceVysledku
n7:7241798 n7:4369211 n7:6083064
n5:druhVysledku
n15:J
n5:duvernostUdaju
n12:S
n5:entitaPredkladatele
n17:predkladatel
n5:idSjednocenehoVysledku
104437
n5:idVysledku
RIV/67985530:_____/13:00389366
n5:jazykVysledku
n19:eng
n5:klicovaSlova
Banda Arc; subduction; Wadati-Benioff zone; collision; calc-alkaline volcanism
n5:klicoveSlovo
n10:collision n10:Wadati-Benioff%20zone n10:calc-alkaline%20volcanism n10:subduction n10:Banda%20Arc
n5:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n5:kontrolniKodProRIV
[D29BB6D76A8D]
n5:nazevZdroje
Journal of Asian Earth Sciences
n5:obor
n9:DC
n5:pocetDomacichTvurcuVysledku
3
n5:pocetTvurcuVysledku
3
n5:projekt
n6:ME09011
n5:rokUplatneniVysledku
n11:2013
n5:svazekPeriodika
64
n5:tvurceVysledku
Špičák, Aleš Matějková, Radka Vaněk, Jiří
n5:wos
000316706500001
s:issn
1367-9120
s:numberOfPages
13
n18:doi
10.1016/j.jseaes.2012.11.014