The relations among electrical conductivity and graphite
content, metamorphic grade, and fluid:rock interaction are
investigated for a suite of regionally metamorphosed
graphitic carbonate rocks from the Waits River Formation,
NE Vermont. Graphitization was complete by the lowest
grade of metamorphism attained in the area (450 degrees C
and 450 MPa). In low-grade rocks, graphite occurs as
inclusions within calcite and along grain boundaries, and
in medium-grade rocks, it concentrates near porphyroblasts.
In neither suite does graphite form interconnected networks.
Average reduced carbon abundances are 4400 and 2800 ppm for
the low- and medium-grade rocks, respectively. High-grade
rocks are almost void of graphite, except for one specimen.
The 13C values were determined for graphite and
carbonates and
18O values were determined for the
carbonates and silicate residues. There is no change in
isotopic values between low- and medium-grade rocks. In
contrast, high-grade rocks show marked decreases in
13C and
18O values of about 4 per mil compared to
low and medium-grade rocks. Both isotopic analyses and
graphite depletion in high-grade rocks was caused by influx
of large quantities of magmatic water during peak
metamorphism. Electrical conductivity was measured in the
laboratory on representative specimens. Rocks with high
carbon content (>7000 ppm) from both the low- and high-grade
zones display almost an order of magnitude higher electrical
conductivity than expected from their fluid content alone.
Graphite does not form an interconnected network in these
rocks, yet it combines with the saline fluids to
significantly increase electrical conductivities.
AGU Index Terms: 5109 Magnetic and electrical properties; 3660 Metamorphic petrology; 3645
Keywords/Free Terms: Electrical properties, metamorphic petrology, isotope composition.
JGR-Solid Earth 96JB01757