T13 Volcanic and Landscape Evolution of the Jemez Mountains Volcanic Field

Sunday, 31 October 2010
8:00 AM - 12:00 PM
Mile High Ballroom 4AB

FUMAROLIC PIPES IN THE TSHIREGE MEMBER OF THE BANDELIER TUFF, JEMEZ MOUNTAINS VOLCANIC FIELD

Paper number: T13-9
Program: Technical Sessions
Time: 10:00 AM – 10:15 AM

Authors

Abstract

The geology exposed on the walls (3000 m2) of a large excavated pit in the Tshirege Member of Bandelier Tuff gives unparalled 3-D exposures of many structures that develop in thick deposits of pyroclastic flows. The subunits exhibit distinct rubble-filled fissures, or pipes, that range in width from centimeters to meters. The fissures exhibit zones of fines depletion, indurated wall structures, upward flaring geometry to the top of the host unit, and fissure-filling blocks of the host unit as well as rubble derived from overlying pyroclastic units. Furthermore, the overlying unit is heavily fractured immediately above the fumarolic pipes. The pipes are regularly spaced at about 4.5 or 7.5 meters apart. All these field characteristics are indicative of fumarolic activity.

Petrographic, XRD, and XRF studies of distinct pipes were done to investigate the chemical changes imparted to the tuff by the fumarolic activity. Petrography indicates that the pipe wall and pipe centers are enriched in tridymite and potassium feldspar. These minerals fill the void spaces in pumice and groundmass void spaces of the pipe wall rocks, imparting the indurated nature. Other mineralogic indicators of late stage fumarolic gas phase deposition are optically continuous, feathery overgrowths on sanidine phenocrysts and scapolite in pipe centers. Clinopyroxenes in the overlying rubble zones have oxidized rims indicative of highly oxidizing gases emanating from the fumarolic pipes below. Also, secondary clay alteration in the rubble zone point to these gases being acidic in nature.

XRD analyses of rubble zones above the pipes show a decrease of cristobalite (4 wt. %) and feldspar (9 wt. %), and subsequent increase of clay contents (12 wt. %). This change from feldspar and cristobalite to clay suggests an acidic nature of fumarolic gases. The data indicate that there have been systematic changes in the geochemistry of the fissures readily attributable to the action of fumarolic gases. XRF data also provide evidence of systematic major and trace element enrichment / depletion trends.

Field relations, petrography, XRD, and XRF element analyses all indicate that the filled fissures are fossil fumarolic pipes. Fumarolic activity, established after deposition, must have continued after emplacement and induration of overlying units.