Vol. 297, Issue 7, 1997

Science Paper
Grain-scale Stable Isotope Disequilibrium During Fluid-Rock Interaction; 1, Series Approximations for Advective-Dispersive Transport and First-Order Kinetic Mineral-Fluid Exchange
R. AbartR. Sperb
Stable isotope fronts provide lasting evidence of fluid-rock interaction. The processes involved in material transport and mineral-fluid exchange may be identified from an analysis of front geometries based on transport...
Science Paper
Grain-scale Stable Isotope Disequilibrium During Fluid-Rock Interaction; 2, an Example From the Penninic-Austroalpine Tectonic Contact in Eastern Switzerland
H. EppelR. Abart
At the tectonic contact between the Penninic Platta Nappe and the Lower-Austroalpine Err Unit in eastern Switzerland carbon and oxygen isotope fronts are preserved at the interface of serpentinites and...
Science Paper
A Geologic History of the North-Central Appalachians; Part 2, the Appalachian Basin From the Silurian Through the Carboniferous
Rodger T. Faill
The north-central Appalachians occupy a critical position within the 3000+ km-long Appalachian orogen, lying southwest of the boundary between the central and northern Appalachians (CNAB). The one-billion-year-long history of tectonic...
Miscellaneous
A Note on the Terrane Concept, Based on an Introduction to the Terrane '97 Conference, Christchurch, New Zealand, February, 1997
D. S. Coombs
A widely accepted definition of tectonostratigraphic terrane is that of Howell, Jones, and Schermer (1985): a fault-bounded package of rocks of regional extent characterized by a geologic history that differs...

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