Scientific core hole Valles caldera No. 2b (VC-2b), New Mexico
Conference
·
OSTI ID:5621984
- Los Alamos National Lab., NM (USA)
Research core hole was continuously cored to 1.762 km on the western flank of the caldera's resurgent dome in 1988. Bottom hole temperature is about 295{degree}C within Precambrian (1.5 Ga) quartz monzonite, deep within the liquid-dominated portions of the Sulphur Springs hydrothermal system. VC-2b may be the deepest, hottest, continuously cored hole in North America. Core recovery was 99.2%. The only major drilling problems encountered were when temperatures at the bit exceeded 225{degree}C below depths of about 1000 m. The result of these conditions was loss of viscosity and/or lubricity in the mud, apparently caused by breakdown of the high temperature polymers. Lithologies in caldera-fill indicate the drill site may be proximal to ignimbrite vents and that an intracaldera lake with temperatures approaching boiling formed soon after the caldera itself. Structural correlations between VC-2b and the 528-m-deep companion hole VC-2a indicate the earlier Toledo caldera (1.45 Ma; Otowi Member tuffs) and even older Lower Tuffs caldera experienced no structural resurgence similar to the 1.12 million year old Valles caldera. The hydrothermal system penetrated by these bores, consists of a shallow vapor-rich cap, which has evolved from an earlier 200{degree}C liquid-dominated system, overlying stacked, liquid-dominated zones up to about 300{degree}C. Geochemistry of mud returns collected during drilling suggests chloride-rich geothermal fluids were entering the bore and mixing with the drilling fluids in the fractured lower Paleozoic and Precambrian sections. 23 refs., 5 figs., 1 tab.
- Research Organization:
- Los Alamos National Lab., NM (USA)
- Sponsoring Organization:
- DOE/ER
- DOE Contract Number:
- W-7405-ENG-36
- OSTI ID:
- 5621984
- Report Number(s):
- LA-UR-89-2025; CONF-891031--2; ON: DE89014316
- Country of Publication:
- United States
- Language:
- English
Similar Records
Isotopic and trace element characteristics of rhyolites from the Valles Caldera, New Mexico. Final technical report
Environmental sampling and mud sampling program of CSDP (Continental Scientific Drilling Program) core hole VC-2B, Valles Caldera, New Mexico
Caldera processes and magma-hydrothermal systems continental scientific drilling program: thermal regimes, Valles caldera research, scientific and management plan
Technical Report
·
Sun Sep 01 00:00:00 EDT 1991
·
OSTI ID:10189843
Environmental sampling and mud sampling program of CSDP (Continental Scientific Drilling Program) core hole VC-2B, Valles Caldera, New Mexico
Technical Report
·
Wed Feb 28 23:00:00 EST 1990
·
OSTI ID:7012834
Caldera processes and magma-hydrothermal systems continental scientific drilling program: thermal regimes, Valles caldera research, scientific and management plan
Technical Report
·
Thu May 01 00:00:00 EDT 1986
·
OSTI ID:5467724
Related Subjects
15 GEOTHERMAL ENERGY
BOREHOLES
CALDERAS
CAVITIES
DRILL CORES
ENERGY SYSTEMS
EVALUATION
FEDERAL REGION VI
FLUIDS
GEOLOGY
GEOPHYSICAL SURVEYS
GEOTHERMAL FLUIDS
GEOTHERMAL SYSTEMS
Geothermal Legacy
HYDROTHERMAL SYSTEMS
NEW MEXICO
NORTH AMERICA
RESERVOIR TEMPERATURE
SURVEYS
TEMPERATURE MEASUREMENT
TEMPERATURE SURVEYS
USA
WELL TEMPERATURE
BOREHOLES
CALDERAS
CAVITIES
DRILL CORES
ENERGY SYSTEMS
EVALUATION
FEDERAL REGION VI
FLUIDS
GEOLOGY
GEOPHYSICAL SURVEYS
GEOTHERMAL FLUIDS
GEOTHERMAL SYSTEMS
Geothermal Legacy
HYDROTHERMAL SYSTEMS
NEW MEXICO
NORTH AMERICA
RESERVOIR TEMPERATURE
SURVEYS
TEMPERATURE MEASUREMENT
TEMPERATURE SURVEYS
USA
WELL TEMPERATURE