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Details van artikel 6 van 14 gevonden artikelen
| Titel: |
Geological interpretation of the Cootamundra gravity high, New South Wales |
| Auteur: |
Watts, M. D. |
| Verschenen in: |
Australian journal of earth sciences |
| Paginering: | Jaargang 18 (1971) nr. 3 pagina's 229-234 |
| Jaar: |
1971-11 |
| Inhoud: |
An intense Bouguer anomaly 'high' of about 30 milligals amplitude has been delineated to the east of Cootamundra, New South Wales. It is correlated with a north-trending belt of basic metamorphic rocks of probable Upper Silurian age. The subsurface shape of the belt is deduced by qualitative and quantitative analytical techniques applied to the gravity data; it is inferred that the boundary on the western side is near-vertical, while that on the eastern side is believed to have been overthrust by the Middle Devonian Young Granite. It appears also that there are no horizontal density variations below a depth of 6-7 km, implying that the base of the Young Granite lies at about this depth. |
| Uitgever: |
Taylor & Francis |
| Bronbestand: |
Elektronische Wetenschappelijke Tijdschriften |
Details van artikel 6 van 14 gevonden artikelen
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