Comparative thermometry on pelitic rocks and marbles of the Llano uplift, Texas
- Texas A and M Univ., College Station, TX (United States). Dept. of Geology
The Llano Uplift in central Texas is a Grenville-aged metamorphic complex consisting of amphibolite facies assemblages whose development has been attributed to the emplacement of granite plutons between 1.0--1.1 Ga. Temperatures have been obtained from garnet-biotite, garnet-ilmenite, and calcite-dolomite pairs as well as from various silicate equilibria. Application of these geothermometers yield consistent results and are thus indicative of peak conditions attending the amphibolite facies metamorphism. Temperature determined using garnet-biotite and garnet-ilmenite thermometry compare favorably with calcite-dolomite temperatures obtained from marbles in contact with granite plutons in the southeastern part of the uplift. The highest calcite-dolomite temperatures of [approximately]600 C are obtained from marbles containing an isobarically invariant assemblage consisting of calcite + dolomite + diopside + tremolite + forsterite. At pressures of 2--3 kbar, this isobarically invariant assemblage will be stable at a temperature range of [approximately]600--650 C. Also in close proximity to granites in the southeast uplift is the assemblage muscovite + quartz + k-feldspar + sillimanite [approximately] andalusite which indicate T 650 C and P 2.5 kbar. Assemblages consisting of garnet + sillimanite + quartz + plagioclase (GASP) and garnet + rutile + ilmenite + plagioclase + quartz (GRIPS) are currently being studied to provide additional constraints on pressures of amphibolite facies metamorphism.
- OSTI ID:
- 5690624
- Report Number(s):
- CONF-921058-; CODEN: GAAPBC
- Journal Information:
- Geological Society of America, Abstracts with Programs; (United States), Vol. 24:7; Conference: 1992 annual meeting of the Geological Society of America (GSA), Cincinnati, OH (United States), 26-29 Oct 1992; ISSN 0016-7592
- Country of Publication:
- United States
- Language:
- English
Similar Records
Quantitative estimates of metamorphic equilibria: Tallassee synform, Dadeville belt, Alabama's Inner Piedmont
Cordierite reaction textures in semipelitic rocks from metamorphic zone IV in central Massachusetts: Their interpretation and possible p-t significance
Related Subjects
GEOLOGIC FORMATIONS
GEOTHERMOMETRY
TEXAS
BIOTITE
CALCITE
COMPARATIVE EVALUATIONS
DOLOMITE
GARNETS
GEOLOGIC HISTORY
GEOTHERMOMETERS
ILMENITE
METAMORPHISM
MINERALOGY
RESERVOIR TEMPERATURE
CARBONATE MINERALS
DEVELOPED COUNTRIES
EVALUATION
MEASURING INSTRUMENTS
MICA
MINERALS
NORTH AMERICA
OXIDE MINERALS
OXYGEN COMPOUNDS
SILICATE MINERALS
SILICATES
SILICON COMPOUNDS
THERMOMETERS
USA
580000* - Geosciences