Serendipity struck a group of Ohio State University geologists last December as they picked away at the stratified sediment in an ancient stream bed high in the frigid Transantarctic Mountains.
New rock and paleomagnetic research give evidence for prolonged heating during the Cambrian-Ordovician tectonic consolidation of West Gondwanaland.
Some results have been hidden because they may be inaccessible to you
Show inaccessible results
Feedback