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- Gloucester subregion
- 1.1 Context statement for the Gloucester subregion
- 1.1.3 Geology
- 1.1.3.5 Potential basin connectivities
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The Gloucester Basin contains Permian sedimentary and volcanic rock units that rest unconformably on Carboniferous strata of the Late Paleozoic New England Fold Belt. No other basin lies on the top of the Gloucester Basin and therefore no connectivity is expected.
Last updated:
5 January 2018
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