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Investigations of the Dunes geothermal anomaly, Imperial Valley, California. Part III. Further petrological studies. Hydrothermal alteration and mass transfer in the discarge portion of the Dunes geothermal system, Imperial Valley of California, USA

Technical Report ·
OSTI ID:7228211
This study concerns self-sealing in stratigraphically-controlled sedimentary aquifers in the discharge portion of a hydrothermal system, located at the Southeast margin of the Salton Trough. Intense low-temperature hydrothermal alteration of deltaic sediments of the Colorado River occurs in this discharge portion. The aquifers are stratigraphically controlled with seven zones of intensively silicified quartzites developed in the upper 318 m. Shale beds of low permeability separate these silicified horizons from poorly indurated sandstones which are cemented by varying amounts of hematite, calcite, gypsum and montmorillonoid clays. The silicified zones were formed in what were originally much more permeable sandstones and conglomerates. Hydrothermally altered sands have a net chemical gain of SiO/sup 2/ and K/sup 2/O, and loss of CaO, Na/sup 2/O, FeO, and MgO, relative to unaltered surface sands, due to reaction with silica-saturated hydrothermal solutions having a high K+/H+ activity ratio. Hot brines migrated laterally rather than vertically through the formation. Hydrothermal metasomatism reduced the permeability of the aquifers forming a dense cap-rock which modified the hydrology and provided a geophysical exploration target.
Research Organization:
California Univ., Riverside (USA). Inst. of Geophysics and Planetary Physics
OSTI ID:
7228211
Report Number(s):
PB-259818; IGPP-UCR-75-14
Country of Publication:
United States
Language:
English