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Internal [sup 238]U-series systematics of pumice from the November 13, 1985, eruption of Nevado de Ruiz, Colombia

Conference · · Geochimica et Cosmochimica Acta; (United States)
OSTI ID:6341784
;  [1];  [2];  [3]
  1. Arizona State Univ., Tempe (United States)
  2. Argonne National Lab., IL (United States)
  3. Los Almos National Lab., NM (United States)
High-precision mass spectrometer and alpha scintillation measurements of [sup 238]U-series nuclides were obtained for whole-rock pumice and constituent mineral and glass separates to help interpret the timing and nature of magmatic processes that led up to the 1985 eruption of Nevado de Ruiz volcano. Internal isochron diagrams for [sup 226]Ra/Ba vs. [sup 230]Th/Ba and [sup 230]Th/[sup 232]Th vs. [sup 238]U/[sup 232]Th show that data define linear arrays, indicating an average crystallization age of 6.1 [+-] 0.5 ka (Ra-Th isochron) and 7 [+-] 6 ka (Th-U isochron). Stratigraphic, petrographic geochemical, repose time, and eruption volume data for the Holocene eruptive sequence of Nevado del Ruiz indicate that significant changes occurred in the subvolcanic magma chamber between eruptions R9 ([approx]8.6 ka) and R8 ([approx]3.0 ka). This coincides with the average crystallization age derived from the U-series data and may represent the injection of a new batch (or batches) of mantle-derived magma into the subvolcanic magma chamber. 26 refs., 4 figs., 2 tabs.
OSTI ID:
6341784
Report Number(s):
CONF-911017--; CNN: EAR-8608977; EAR-8721206
Conference Information:
Journal Name: Geochimica et Cosmochimica Acta; (United States) Journal Volume: 57:6
Country of Publication:
United States
Language:
English