2024-03-19T09:42:10Zhttp://digital.csic.es/dspace-oai/requestoai:digital.csic.es:10261/1513092018-07-19T07:45:14Zcom_10261_82com_10261_8col_10261_335
2017-06-13T08:00:07Z
urn:hdl:10261/151309
Remarkable variability in dyke features at the Vicuña Pampa Volcanic Complex, Southern Central Andes
Guzmán, Silvina
Neri, M.
Carniel, R.
Martí Molist, Joan
Grosse, P.
Montero-López, Carolina
Geyer, Adelina
Ministerio de Economía y Competitividad (España)
Agencia Nacional de Promoción Científica y Tecnológica (Argentina)
Consejo Nacional de Investigaciones Científicas y Técnicas (Argentina)
Dykes at the Vicuña Pampa Volcanic Complex, which are mostly basaltic (trachy)-andesite and (trachy)-andesite, are exposed at the base and along the walls of a large depression resulting from intense degradation. Dykes intruding stiff layers (lavas, plugs and necks) are thin, mostly dip >60° and have coherent textures, whereas dykes intruding more compliant materials (breccias and conglomerates) tend to be thicker, have lower dips and have coherent, brecciated or mixed textures (coherent and brecciated textural domains in a single or compound dyke). Single dykes with brecciated and mixed textures are only found intruding near-surface units. Dykes with mixed textures always have sharp contacts between domains. Dykes with sinuous domain contacts and enclaves of one domain inside the other are interpreted as resulting from dyke arrest, partial cooling and reinjection of new magma. Dykes with straight domain contacts are considered to be compound dykes, with a new dyke intruding along the margins of an older, solidified one.
2017-06-13T08:00:07Z
2017-06-13T08:00:07Z
2017-05
artículo
Terra nova, 29(4): 224–232 (2017)
0954-4879
http://hdl.handle.net/10261/151309
10.1111/ter.12268
1365-3121
http://dx.doi.org/10.13039/501100003329
http://dx.doi.org/10.13039/501100003074
http://dx.doi.org/10.13039/501100002923
eng
http://dx.doi.org/10.1111/ter.12268
Sí
openAccess
John Wiley & Sons