@article{10272/10191,
year = {1998},
url = {http://hdl.handle.net/10272/10191},
abstract = {Clay minerals from the volcaniclastic deposits of the three different sedimentary settings (paleosols, continental lacustrine and transitional, fan delta) have been studied by X-ray, MEB y TEM. The clay fraction of this sediments consist largely of smectite (saponite) with minor irregular chlorite-smectite mixed layers and illite; they occur as replacement of ferromagnesian minerals, plagioclase microlites and glass matrix of the volcarenite and they are inferred to be direct diagenetic alteration products of volcanic components},
publisher = {Sociedad Geológica de España},
title = {Procesos de transformación y neoformación de esmectitas en los materiales volcanoclásticos de la isla de La Palma (Canarias)},
title = {Processes of transformation and heoformation of smectites in the volcaniclastic deposits from the La Palma (Canary Islands)},
author = {Vegas Salamanca, J. and García Romero, E. and Marfil Pérez, Rafaela},
}