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Statements

Subject Item
n2:RIV%2F00216208%3A11310%2F14%3A10282973%21RIV15-MSM-11310___
rdf:type
n7:Vysledek skos:Concept
rdfs:seeAlso
http://dx.doi.org/10.1111/ter.12103
dcterms:description
Fault-bounded coherent belts alternating with belts of melanges are common in accretionary wedges and are usually interpreted as a result of imbrication along subduction zone megathrusts. Using the Neoproterozoic/early Cambrian Blovice accretionary complex (BAC), Bohemian Massif, as a case example, we present a new model for the origin of alternating belts through the repetition of several cycles of (1) off-scraping and deformation of trench-fill sediments to form the coherent units, interrupted by (2) arrival and subduction of linear, trench-parallel volcanic elevations. The latter process leads to an increase in the wedge taper, triggering mass-wasting and formation of olistostromes. At the same time, ophiolitic melanges form by disruption of an upper part of the volcanic ridge and incorporation of the disrupted oceanfloor succession into the olistostromes. Specifically, the BAC represents a complete section across an accretionary wedge and records three such major pulses of ophiolitic melange formation through subduction of an outboard back-arc basin. Fault-bounded coherent belts alternating with belts of melanges are common in accretionary wedges and are usually interpreted as a result of imbrication along subduction zone megathrusts. Using the Neoproterozoic/early Cambrian Blovice accretionary complex (BAC), Bohemian Massif, as a case example, we present a new model for the origin of alternating belts through the repetition of several cycles of (1) off-scraping and deformation of trench-fill sediments to form the coherent units, interrupted by (2) arrival and subduction of linear, trench-parallel volcanic elevations. The latter process leads to an increase in the wedge taper, triggering mass-wasting and formation of olistostromes. At the same time, ophiolitic melanges form by disruption of an upper part of the volcanic ridge and incorporation of the disrupted oceanfloor succession into the olistostromes. Specifically, the BAC represents a complete section across an accretionary wedge and records three such major pulses of ophiolitic melange formation through subduction of an outboard back-arc basin.
dcterms:title
Growth of accretionary wedges and pulsed ophiolitic melange formation by successive subduction of trench-parallel volcanic elevations Growth of accretionary wedges and pulsed ophiolitic melange formation by successive subduction of trench-parallel volcanic elevations
skos:prefLabel
Growth of accretionary wedges and pulsed ophiolitic melange formation by successive subduction of trench-parallel volcanic elevations Growth of accretionary wedges and pulsed ophiolitic melange formation by successive subduction of trench-parallel volcanic elevations
skos:notation
RIV/00216208:11310/14:10282973!RIV15-MSM-11310___
n3:aktivita
n14:I
n3:aktivity
I
n3:cisloPeriodika
4
n3:dodaniDat
n8:2015
n3:domaciTvurceVysledku
n4:4043790 n4:7631219 n4:8387699
n3:druhVysledku
n13:J
n3:duvernostUdaju
n10:S
n3:entitaPredkladatele
n16:predkladatel
n3:idSjednocenehoVysledku
18651
n3:idVysledku
RIV/00216208:11310/14:10282973
n3:jazykVysledku
n17:eng
n3:klicovaSlova
Bohemian Massif; early Cambrian; Neoproterozoic; trench-parallel volcanic elevations; ophiolitic mélange; accretionary wedges
n3:klicoveSlovo
n11:Bohemian%20Massif n11:early%20Cambrian n11:ophiolitic%20m%C3%A9lange n11:Neoproterozoic n11:accretionary%20wedges n11:trench-parallel%20volcanic%20elevations
n3:kodStatuVydavatele
GB - Spojené království Velké Británie a Severního Irska
n3:kontrolniKodProRIV
[5F17A8CCC9D2]
n3:nazevZdroje
Terra Nova
n3:obor
n15:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n8:2014
n3:svazekPeriodika
26
n3:tvurceVysledku
Hajná, Jaroslava Kachlík, Václav Žák, Jiří
n3:wos
000339259400009
s:issn
0954-4879
s:numberOfPages
8
n18:doi
10.1111/ter.12103
n5:organizacniJednotka
11310