11 D3. Southern Appalachian and Analogous Terranes I
Friday, 2 April 2021
8:00 AM - 12:00 PM
FMR, Inc. Room
A POSSIBLE NEOACADIAN METAMORPHIC BELT IN THE BLUE RIDGE OF ALABAMA AND GEORGIA: METAMORPHISM OF THE PUMPKINVINE CREEK FORMATION AND THE MAD INDIAN GROUP
Paper number: 11-8
Program: Technical Sessions
Time: 10:20 AM – 10:40 AM
Authors
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Hannah DicksonUniversity of Alabama, Tuscaloosa, AL
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Harold H. StowellUniversity of Alabama, Tuscaloosa, AL
Abstract
Sample 17Ash01 was collected from the Mad Indian Group near Micaville , Alabama and is a garnet-kyanite-biotite-muscovite schist with minor sillimanite and staurolite. The MAD for this sample indicates metamorphism occurred during loading from 6.5 kbar 550°C to 9 kbar 650°C. Garnet growth occurred at 357±3 Ma during the Neoacadian orogeny based on Sm-Nd geochronology. Sample 17PumCan01 was collected from the Pumpkinvine Creek formation near Canton, Georgia, c. 125 km northeast of Micaville. The sample is a coarse-grained garnet-hornblende-kyanite gneiss with minor staurolite. A preliminary MAD indicates c. 150°C of heating and 5 kbar of loading to peak conditions of 610-715°C and 8.5-11 kbar, overlapping with the P-T-t results for the Mad Indian Group.
Recent studies highlight the geochemical and structural similarities between the two units, suggesting both units as part of a c. 460 Ma Laurentian margin and back arc system. No published metamorphic age data exists for the Pumpkinvine Creek formation; however, an unpublished 313 Ma Ar-Ar hornblende cooling age is suggestive of peak metamorphism during the Neoacadian. Additional P-T-t data is needed to confirm the possible extent of Neoacadian metamorphism.
Geological Society of America Abstracts with Programs. Vol. 53, No. 2
doi: 10.1130/abs/2021SE-362349
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