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Superposition of Ductile Structures in the Montpelier Quadrangle: Central Vermont

By Jonathan Kim and Marjorie Gale
Poster presented at NE Geological Society of America Annual Meeting

Click on images below to enlarge them

Metasedimentary and metaigneous rocks of Ordovician through Devonian age rocks are mapped in the Montpelier Quadrangle. A major unconformity (RMC) that is locally faulted separates Ordovician rocks (Cram Hill + Moretown fms.) to the NW from Silurian-Devonian rocks (Shaw Mt., Northfield, + Waits River) to the SE. Within the Ordovician section, truncation of lithologies and truncation of the F1/F2 composite fold structure mapped in the northwest portion of the quadrangle suggest a fault contact (Shady Rill fault) between western and eastern sections of the Moretown Fm. The Montpelier quadrangle can be divided into three discontinuity-bounded structural domains (NW, central, and SE) which reflect the dominance of Taconian structures, an overlap domain, and Acadian structures, respectively.

In the NW domain (Domain 1), bedding is folded by two generations of steeply-plunging asymmetric tight folds (F1 and F2). Within the phyllitic units, well-developed closely spaced foliation and a “pinstripe” (S1) is parallel to the axial plane of the F1 folds and bedding is transposed. Bedding is preserved in the massive quartzites. Quartz rods (L1) are colinear with F1 fold axes. In the NW domain, S0 commonly trends nearly east-west whereas S1 trends NNE.

Moretown and Cram Hill Fm rocks of the central domain (Domain 2) are bounded by the Shady Rill fault (west) and the RMC (east). The dominant foliation in the Central domain is an S1/S2 composite foliation that has been re-oriented by F3 folds; S3 intensifies close to the RMC. F3 folds are isoclinal with severely attenuated limbs and preferentially develop in certain zones. Steeply-plunging lineations (L2) on the S3 cleavage planes are, in most cases, the F2 fold axes; however, steeply-plunging stretching lineations (L1) are also present. The F3 overprint obscures F1 and F2 structures. Bedding is only locally preserved in isolated fold hinges.

The structures in the Silurian and Devonian lithologies of the eastern domain (Domain 3) are related to the Acadian Orogeny; they consist of tight to isoclinal, moderately north-plunging folds (F3) with a steeply west-dipping axial planar spaced cleavage (S3). S3 is locally deformed by asymmetric, tight folds (F4) with sub-horizontal axes and a moderately west-dipping crenulation cleavage (S4). F3 folds and the northwest striking more open F4 folds occur both east and west of the RMC. F1 and F2 are absent east of the RMC.

FIGURE 1. Lithofacies Map FIGURE 2. FIGURE 3. Bedrock Map FIGURE 4. Cross-section FIGURE 5a. Domain 1 FIGURE 5b. FIGURE 5c. FIGURE 5d. FIGURE 5e. FIGURE 5f.

Bedrock geologic map (2003)
Bedrock photographs
Photolineament analysis (2004) Pascale et. al., 2004
Rockfall on Elm St. (2005)
Surficial Geologic map (Larsen, 1999)


Generalized Geologic 
	Map of Vermont - 1970 - click for larger map image

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