The Structure and Stratigraphy of Small Point, Maine: D3 Inverted Transtensional Map-Scale Folds of Neoacadian Provenance

The Cape Small Synform lies in an area of the Northern Appalachians that has undergone successive deformation from at least two major orogenic events, the Salinic Orogeny (440-423 Ma) and the Acadian Orogeny (421 – 400 Ma) (van Staal et al. 2009) and contains evidence for Norumbega shearing deformat...

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Bibliographic Details
Main Author: Sive, Haley Russell
Format: Text
Language:unknown
Published: SCARAB 2012
Subjects:
geology
deformation
transtension
metamorphism
shear
orogeny
Hermit Island
Hussey
Spring Point
Seal Island
Online Access:https://scarab.bates.edu/honorstheses/45
https://scarab.bates.edu/context/honorstheses/article/1051/type/native/viewcontent

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