Four phases of deformation are recorded by minor structures in the New Harbour Group (NHG) of southern Holy Island. The regional schistosity in these rocks is a dierentiated crenulation cleavage of D 2 age. An earlier preferred orientation (S 1 ) is commonly preserved as crenulations within the Q-do
A resistivity section of Holy Island (Anglesey)
โ Scribed by G. M. Habberjam; A. A. Jackson
- Book ID
- 102225808
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 403 KB
- Volume
- 9
- Category
- Article
- ISSN
- 0072-1050
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โฆ Synopsis
Abstract
An account is given of the use of square array resistivity techniques to derive an apparent resistivity section down the length of Holy Island (Anglesey). Possible interpretations of this section in terms of the distribution of true resistivity with depth are given and discussed briefly in relation to proposed geological structure.
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