{"help": "https://data.gov.au/data/en/api/3/action/help_show?name=package_show", "success": true, "result": {"archived": false, "author_email": null, "contact_point": "clientservices@ga.gov.au", "creator_user_id": "c2fbbe4a-4ba0-4945-808b-67454605a4cf", "duplicate_score": 1, "geospatial_topic": [], "id": "88aa6039-1a21-4519-97cf-3bbf9405ac5d", "isopen": false, "language": "eng", "license_id": "notspecified", "license_title": "notspecified", "maintainer": null, "maintainer_email": null, "metadata_created": "2026-03-05T10:22:33.063761", "metadata_modified": "2026-03-05T10:22:33.063769", "name": "global-sea-level-change-as-a-method-of-correlating-the-late-permian-coal-measures-in-the-sydney8", "notes": "Eustatic changes in sea level can be used to correlate sequences in widely separated areas.  Thick terrestrial sequences with marine intercalations are especially suitable, provided the marine beds are not the result of tectonic subsidence. The method has been used to correlate Late Permian coal measures in the Sydney, Gunnedah, and Bowen Basins.  The Dempsey Formation and its equivalents in the Sydney Basin, an unnamed correlative in the Gunnedah Basin, and the Black Alley Shale and MacMillan Formation in the Bowen Basin have been identified as being deposited during the same eustatic highstand, a result consistent with palynological conclusions. The Kulnura Marine Tongue (Sydney Basin) and the lower Burngrove Formation (Bowen Basin), on the other hand, owe their origin to tectonism. 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