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Title: Textural aspects of high T-low P polymetamorphism in the Rangeley area, western Maine: General implications for studies of Acadian metamorphic rocks in New England

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5934649
 [1]
  1. Univ. of Maine, Orono, ME (United States). Dept. of Geology

High T-Low P polymetamorphism in W. Maine results from overlapping, regionally extensive thermal aureoles around sheet-like granitic plutons. At least five metamorphic events have been recognized. The Rangeley-Oquossoc (R-O) area was affected by two high T, static events (M[sub 2] and M[sub 3]). M[sub 2], (400 Ma) developed and + St + Bt regionally. M[sub 3] (370 Ma), due to heating by the sheet-like Mooselookmeguntic Pluton (MP), is superimposed on M[sub 2] such that near the MP, M[sub 2] rocks were prograded to upper sillimanite zone, migmatitic gneisses. To the E., M[sub 2] rocks have been downgraded to garnet zone. Mineral chemistry and assemblage data strongly suggest that M[sub 3] parageneses closely approximated a new equilibrium. These temporally separate superimposed events produced pseudomorphic replacement textures; in the E. by downgrade reactions; in the W. by prograde reactions. The nature of the downgrade or prograde pseudomorphs reflects where they occur in the M[sub 3] range of metamorphic grades. Some authors have interpreted these textures as due to continuous PTt paths or K-metasomatism. Even worse, in some studies the textures are simply ignored and mineral assemblages merely assumed to be the result of a single, equilibrium metamorphic event. The three Al-silicate rocks in the Littleton-Mooselauke area of New Hampshire probably fall in this latter category. It is suggested that in most cases such textures are best interpreted as the R-O area. Metamorphic textures probably are unique in some aspects related to the details of the metamorphism(s) of the given area. However, in New England the commonness in Acadian metamorphic rocks of textures similar to those found in the fortuitously well displayed example of temporally separated polymetamorphism in the R-O area suggests a basis to recognize similar histories elsewhere.

OSTI ID:
5934649
Report Number(s):
CONF-9303211-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 25:2; Conference: 28. annual Geological Society of America (GSA) Northeastern Section meeting, Burlington, VT (United States), 22-24 Mar 1993; ISSN 0016-7592
Country of Publication:
United States
Language:
English

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