Please use this identifier to cite or link to this item:
Export to Endnote
https://geoscience.nt.gov.au/gemis/ntgsjspui/handle/1/88971
Export to Endnote
Title: | Reconnaissance geology, Gulf of Carpentaria: A Process Report |
Title Holder / Company: | Frome-Broken Hill Company |
Report id: | PR1956-0001 |
Tenure: | OP4 |
Year: | 1956 |
Abstract: | Palaeozoic sediments are known to occur on the margins of the Carpentaria Basin. They folded and intruded by igneous rocks along the tectonic belts and are essentially undisturbed elsewhere. A thick sequence of sediments belonging to Calvert Hills Group on the southwest and west margin of the basin may include petroleum source beds. In places they are folded and faulted, but appear to be nearly flat lying in less disturbed areas. |
Date Added: | 25-Jun-2019 |
Appears in Collections: | Petroleum and Geothermal Tenure Reports (PEX Tenure) |
Files in this Report:
File | Size | Format | Add to Download |
---|---|---|---|
PR19560001.pdf | 5.34 MB | Add | |
PR1956-0001_Plans.zip | 57.79 MB | ZIP | Add |
Items in GEMIS are protected by copyright unless otherwise indicated.