The Holocene Pucón eruption of Volcán Villarrica, Chile : Deposit architecture and eruption chronologyTipo de material: TextoIdioma: Inglés Detalles de publicación: 2010Descripción: pp. 677-692Tema(s): Otra clasificación:
|Tipo de ítem||Biblioteca actual||Colección||Solicitar como||Copia número||Estado||Fecha de vencimiento||Código de barras|
|Artículos de Revistas||SERVICIO NACIONAL DE GEOLOGÍA Y MINERÍA (SERNAGEOMIN)||Colección BSNGM||14411 (Navegar estantería(Abre debajo))||C.1||Disponible||38510|
The Pucón eruption was the largest Holocene explosive outburst of Volcán Villarrica, Chile. It discharged >1.0 km3 of basaltic-andesite magma and >0.8 km3 of pre-existing rock, forming a thin scoria-fall deposit overlain by voluminous ignimbrite intercalated with pyroclastic surge beds. The deposits are up to 70 m thick and are preserved up to 21 km from the present-day summit, post-eruptive lahar deposits extending farther. Two ignimbrite units are distinguished: a lower one (P1) in which all accidental lithic clasts are of volcanic origin and an upper unit (P2) in which basement granitoids also occur, both as free clasts and as xenoliths in scoria. P2 accounts for ~80% of the erupted products. Following the initial scoria fallout phase, P1 pyroclastic flows swept down the northern and western flanks of the volcano, magma fragmentation during this phase being confined to within the volcanic edifice. Following a pause of at least a couple of days sufficient for wood devolatilization, eruption recommenced, the fragmentation level dropped to within the granitoid basement, and the pyroclastic flows of P2 were erupted. The first P2 flow had a highly turbulent front, laid down ignimbrite with large-scale cross-stratification and regressive bedforms, and sheared the ground; flow then waned and became confined to the southeastern flank. Following emplacement of pyroclastic surge deposits all across the volcano, the eruption terminated with pyroclastic flows down the northern flank. Multiple lahars were generated prior to the onset of a new eruptive cycle. Charcoal samples yield a probable eruption age of 3,510?±?60 14C years BP.