The emergence of volcanic oceanic islands on a slow-moving plate: The example of Madeira Island, NE Atlantic (Q155777): Difference between revisions
From geokb
(Created a new Item: Added new publication item from USGS Pubs Warehouse) |
(Changed an Item: added addresses place and/or addresses subject claims from Pubs Warehouse and OpenAlex sources) |
||
| Property / addresses subject | |||
| Property / addresses subject: Climate Change and Paleoclimatology / rank | |||
Normal rank | |||
| Property / addresses subject: Climate Change and Paleoclimatology / reference | |||
| Property / addresses subject | |||
| Property / addresses subject: Paleoredox and Paleoproductivity Proxies / rank | |||
Normal rank | |||
| Property / addresses subject: Paleoredox and Paleoproductivity Proxies / reference | |||
| Property / addresses subject | |||
| Property / addresses subject: Tectonic and Geochronological Evolution of Orogens / rank | |||
Normal rank | |||
| Property / addresses subject: Tectonic and Geochronological Evolution of Orogens / reference | |||
Revision as of 11:07, 19 August 2024
a Article (Journal Article) published by American Geophysical Union as part of series - Geochemistry, Geophysics, Geosystems
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | The emergence of volcanic oceanic islands on a slow-moving plate: The example of Madeira Island, NE Atlantic |
a Article (Journal Article) published by American Geophysical Union as part of series - Geochemistry, Geophysics, Geosystems |
